REYKJAVIK 010001 64 09 N 21 56 W55241973229 54 4 0 0 1951 2199 2063 1907 1915 1933 1988 2033 2078 2079 2181 2197 2299 2073 99999 1956 31293130 - 99999999999999999999 2120 1980 2030 1970 1970 2120 2180 228099999 4860 1957 2290 2190 2150 2080 2120 2080 2090 2020 2030 2240 2140 2200 2135 4860 1958 2160 1980 1980 2000 1930 2000 2040 2120 2170 2200 2250 2220 2088 4860 1959 2050 2170 2230 2080 2030 2110 2170 2090 2150 2280 2240 2320 2160 4860 1960 2140 2060 1890 2070 2060 2140 2150 2070 2200 2160 2330 2290 2130 4860 1961 2200 2250 2190 2120 2080 2210 2090 2160 2280 2070 2030 2150 2150 4860 1962 2280 2110 1940 1960 1990 2090 2070 2170 2190 2220 2160 2110 2107 4860 1963 1940 2090 2250 2070 1900 1750 2130 2140 2190 2300 2270 2200 2104 4860 1964 2270 2210 2220 2130 2200 2210 2250 2150 2270 2270 2290 2240 2226 4860 1965 2240 1970 2080 2140 2140 2300 2160 2220 2250 2300 2180 2300 2191 4860 1966 2170 2190 2050 2060 2070 2140 2070 1900 2280 2190 2170 2220 2125 4860 1967 2130 2250 2150 2040 2070 2150 2120 2180 2220 2320 2230 2120 2165 4860 1968 2150 2010 2100 2000 1980 2150 2030 2110 2170 2240 2270 2230 2120 4860 1969 2110 1930 2030 2020 2030 2180 2190 2200 2190 2270 2150 2170 2124 4860 1970 2210 2150 1970 2030 2080 2100 2080 2110 2170 2140 2310 2120 2123 4860 1971 2200 2120 2040 2060 2150 2060 2120 2200 2200 2240 2150 2220 2148 4860 1972 2320 2260 2230 2150 2200 2250 2170 2140 2150 2230 2180 2390 2221 4860 1973 2280 2150 2120 1980 2060 2170 2160 2190 2250 2190 2170 2150 2156 4860 1974 2410 2190 2140 2080 2130 2160 2200 2200 2220 2100 2230 2270 2196 4860 1975 2290 2170 2080 1990 1950 2060 2130 2180 2210 2220 2230 2140 2139 4860 1976 1031 6 6XX 2200 2260 2280 2040 2160 219099999 2240 2130 2340 2310 2190 2213 4860 1977 6 5 2142 2182 2141 2076 2038 2081 2159 2175 2245 2328 2252 2264 2170 4860 1978 303130 - 2233 2109 2278999999999999999 2139 2183 2222 2221 2357 238099999 4860 1979 02 2201 2226 2185 2019 2078 2178 2237 2269 2250 2301 2305 2326 2214 4860 1980 2150 2244 2103 2094 2060 2095 2128 2171 2260 2206 2143 2189 2153 4860 1981 2 2045 2085 2118 2005 2127 2148 2188 2204 2262 2197 2242 2217 2154 4860 1982 2 2177 2449 2234 2163 2143 2167 2326 2231 2339 2296 2361 2357 2269 4860 1983 2312 2115 2247 2112 2171 2219 2219 2168 2321 2472 2346 2448 2264 4860 1984 31293130 43031 330 - 99999999999999999999 21069999999999 221399999 2327 2331 234499999 4860 1985 430 2 4 2XX 2206 2225 2165 2136 209099999 2176 2183 2220 2266 2226 2278 2198 4860 1986 215 2 5 8 9 3XX 2283 2093 2311 2124 2220 2300 2219 2165 2167 2468 2345 2417 2257 4860 1987 5 9 7 2198 2293 2256 2244 2138 2152 2276 2260 2363 2352 2328 2339 2266 4860 1988 331 7 21512 3XX 2351 219699999 2050 2168 2181 2234 2281 2233 2282 2288 2376 2240 4860 1989 8 7 2 2347 2354 2275 2081 2203 2250 2189 2306 2278 2346 2288 2351 2274 4860 1990 3111 XX 2424 2411 2243 216499999 2226 2298 2312 2271 2355 2266 2362 2305 4860 1991 2 3 4 731XX 2379 2247 2194 2211 2075 2196 2235 2341 2279 2217 226499999 2240 4860 1992 10 4 1 2117 2268 2147 2119 2051 2108 2175 2238 2185 2111 2305 2231 2172 4860 1993 4 9 6 2318 2047 2114 2091 2004 2140 2100 2135 2205 2119 2426 2335 2170 4860 1994 3 1 2 2 1 1 2253 2123 2281 2083 2098 2176 2207 2151 2175 2192 2302 2315 2198 4860 1995 2213 2256 2117 1951 2039 2020 2151 2160 2173 2290 2149 2164 2140 4860 1996 2261 2150 2081 2130 2108 2184 2203 2196 2207 2296 2238 2186 2187 4860 1997 2205 2353 2207 2093 2112 2131 2197 2248 2246 2221 2341 2360 2225 4860 1998 2 2255 2269 2120 2127 2065 2112 2191 2249 2240 2278 2318 2360 2215 4860 1999 2298 2199 2097 2077 2140 2187 2194 2165 2298 2267 2265 2318 2209 4860 2000 2 2169 2305 2091 2057 2134 2157 2140 2168 2280 2367 2261 2296 2202 4860 2001 1 2 2267 2155 2144 2109 2100 2118 2196 2254 2250 2392 2267 2182 2204 4860 2002 2403 2304 2190 2183 2156 2207 2185 2210 2195 2258 2396 2295 2249 4860 2003 2294 2314 2278 2214 2219 2301 2284 2249 2306 2244 2389 2270 2280 4860 2004 112 915 4 5 5 3 1 XX 2305 2147 2267 2212 2144 2232 2252 2270 2351 2287 2272 2353 2266 4860 2005 2240 2033 2081 2166 2058 2171 2214 2289 2272 2271 2281 2235 2193 4860 2006 4 2289 2179 2133 2150 2147 2211 2242 2204 2364 2358 2439 2365 2257 4860 2007 4 2301 2290 2242 2169 2225 2178 2232 2237 2270 2381 2234 2410 2264 4860 2008 2368 2289 2222 2110 2139 2183 2233 2296 2302 2343 2246 2283 2251 4860 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Reykjavik 010/001 RLR(1973) is 17.4m below BM No.77 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-MAR-96 : March 1994:new tide gauge, pressure type GRINDAVIK 010011 63 50 N 22 26 W01241964 9 4 0 0 1957 312831303130313130 - 999999999999999999999999999999999999999999999 2048 1823 189399999 5092 1958 1823 1695 1707 1713 1652 1673 1737 1820 1871 1914 1981 1960 1796 5092 1959 28 XX 175699999 1948 1768 1664 1783 1835 1777 1829 1811 1914 1972 1825 5092 1960 1847 1783 1896 1878 1875 1896 1932 1826 1935 1844 2021 1984 1893 5092 1961 1 1 4 2 1999 1951 1804 1795 1753 1847 1743 1853 1957 1957 1868 1804 1861 5092 1962 2033 1756 1597 1707 1646 1807 1713 1820 1871 1875 1829 1853 1792 5092 1963 1 1 3 1 1 1643 1841 1978 1777 1811 1774 1801 1841 1850 1981 1942 1911 1846 5092 1964 1 4 3 3 1 230 XX 1978 1878 1902 1786 1859 1878 1881 1820 1932 189099999 1932 1887 5092 1965 3 2 1996 1664 1795 1811 1826 1954 1963 1722 1966 2021 1951 2060 1894 5092 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Grindavik 010/011 RLR(1964) is 10.6m below BM No2 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Grindavik 010/011 RLR(1964) is 10.6m below BM No2 JAN MAYEN 012001 70 55 N 08 43 W04249999230 7 3 0 0 1974 312831303130 5 - 999999999999999999999999999999 1076 1012 1093 982 1063 112399999 99999 1975 6 4 2 3 3 51430313031 - 1083 999 951 836 824 937 1060 9709999999999999999999999999 99999 1978 3128 30 - 9999999999 968 819 910 997 940 982 1026 105699999 98199999 99999 1979 14 7 992 1036 923 761 905 998 1021 1050 1104 1016 1034 1066 995 99999 1980 303130313130313031 - 930 888 87099999999999999999999999999999999999999999999999999 99999 1982 3 931 1016 955 858 779 909 1038 1034 1079 1060 1069 1061 982 99999 1983 1 9 1069 866 985 784 764 955 1035 980 965 1023 1017 1070 965 99999 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 10-OCT-94 : DATA DISCONTINUED BECAUSE OBSERVATIONS ARE THOUGHT TO BE DISTORTED AND THE SITE OF THE GAUGE DOES NOT GIVE TRUE SEA LEVEL OBSERVATIONS TORSHAVN 015011 62 01 N 06 46 W61961966237 48 8 0 0 1957 31 2 1 1 1 XX 99999 38 -34 -139 -127 -85 -19 -26 -8 99 -25 68 -23 6970 1958 1 25 -27 -146 -141 -113 -105 -69 -10 -7 53 -7 113 -36 6970 1959 2 7 1 5 1 1 1 1 3 -56 -71 5 -23 -147 -40 28 -8 6 73 102 146 2 6970 1960 10 9 2 5 2 1 -124 -21 -138 -109 -117 -27 63 41 43 43 143 91 -9 6970 1961 1 2 1 3 1 1 6 -28 -30 -45 52 -16 66 117 138 74 2 28 6970 1962 1 1 1 4 91 -152 -156 -171 -100 -51 -95 23 32 49 -20 6 -45 6970 1963 131 1 7 9 XX -140 -4399999 -56 -33 -45 5 43 50 112 161 44 10 6970 1964 2 31303130313130313031 - -5 49999999999999999999999999999999999999999999999999999999 6970 1965 31283130313031 2 - 99999999999999999999999999999999999 24 66 59 58 10199999 6970 1966 36 66 -8 -91 -21 5 43 19 91 74 15 98 27 6970 1967 1 1 -49 61 66 -103 -22 -31 27 -1 54 162 19 31 18 6970 1968 2 1 3 30313031 - 3 -112 4 -107 -117 9 -80 -389999999999999999999999999 6970 1969 31283130 2 3 53031 - 99999999999999999999 -65 23 35 31 50 83999999999999999 6970 1972 31 1 6 XX 99999 19 -6 -11 -18 92 31 10 24 88 173 170 52 6970 1973 1 1030 XX 51 32 -61 -100 -72 -9 12 29 46 199999 27 -4 6970 1974 9 4 176 -4 -110 -153 -33 -16 81 70 172 -3 104 140 36 6970 1975 1 162 -60 -51 -115 -171 -68 34 -13 93 17 55 -1 -9 6970 1976 1 25 -9 -1 -126 -54 -36 6 -40 6 176 154 61 14 6970 1977 5 8 1 8XX 66 47 -2 -30 -121 -57 -43 -14 38 129 126 46 15 6970 1978 7 2 1 74 -37 62 -141 -111 7 8 -24 75 33 133 90 14 6970 1979 -23 -36 1 -128 -99 -25 11 56 85 69 72 104 8 6970 1980 10 7 9 -81 -26 -69 -138 -108 23 5 18 94 80 37 31 -11 6970 1981 31 5 330 - 99999 -81 0 -198 -49 -74 -27 -26 93 8899999 6199999 6970 1982 3313031 2 9 2 - -10 78 -20 -78999999999999999 64 103 117 188 13499999 6970 1983 31 4 831 - 80 -135 0 -92 -40 -4499999 -16 8999999 47 11799999 6970 1984 13130 3 3 2 1 5 5 - 87 -88 -152 -1129999999999 42 -16 73 119 118 6999999 6970 1985 1 1 5 23031 5 1 2 2 4 - -66 -71 -57 -26 -949999999999 115 61 14 54 9599999 6970 1986 4 31 131 4 1 - 71 -17399999 -9999999 -22 114 12 10 174 158 14199999 6970 1987 31 XX -75 9 -37 -6399999 9 74 60 154 154 98 102 44 6970 1988 313031 - 198 49 -21 -114999999999999999 147 100 81 74 9999999 6970 1989 140 180 89 -34 -26 22 7 157 75 139 95 159 83 6970 1990 31 XX 231 233 62 -1 -102 2799999 86 55 127 50 106 79 6970 1991 3 14 64 -39 -39 -39 -123 62 16 47 92 58 141 -41 19 6970 1992 2 -18 91 31 3 -63 -10 53 127 62 33 177 97 49 6970 1993 31 1XX 179 -91 -50 -35 -87 199999 26 57 6 80 153 22 6970 1994 1 10 2 6 98 -5 94 -42 -54 75 34 72 61 91 125 131 59 6970 1995 31 1 30 130 - 99999 144 -16 -133 -63 -106 1 -5199999 17599999 -1299999 6970 1996 7 95 29 -99 -27 -24 5 42 37 36 154 122 13 32 6970 1997 2 35 195 11 -86 -14 12 16 37 72 76 166 118 52 6970 1998 31 4 303130 1 2 - 99999 94 -33999999999999999 93 89 91 153 110 14099999 6970 1999 30 131303130 - 163 60 -599999 -30 9 4799999999999999999999 16499999 6970 2000 2 19 115 -69 -62 -49 -5 -12 25 102 185 182 169 50 6970 2001 89 -12 21 -49 -67 -5 26 76 88 240 104 12 44 6970 2002 3130 - 173 168 13 -209999999999 60 92 81 114 175 7399999 6970 2003 731XX 144 31 52 32 101 135 126 83 139 126 23199999 107 6970 2004 312931303130313130 - 999999999999999999999999999999999999999999999 212 97 13599999 6970 2005 30 7 XX 114 -53 -45 17 -3999999 68 123 131 133 130 50 56 6970 2006 2 51 32 6 54 45 41 92 105 180 221 252 181 105 6970 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Torshavn 015/011 RLR(1966) is 9.3m below BMK-87-9030 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 08-APR-92 : SOME BM UNCERTAINTY BEFORE 1963 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 07-JUL-92 : PRIOR TO 1991 FCODE=24 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Torshavn 015/011 RLR(1966) is 9.3m below BMK-87-9030 BARENTSBURG 025001 78 04 N 14 15 E02241972231 61 15 0 0 1948 3129313031XX - 9999999999999999999999999 1090 1080 1160 1180 1230 1260 128099999 5911 1949 1200 1280 1090 1090 970 1020 1120 1180 1220 1250 1160 1210 1149 5911 1950 1180 1180 1170 1060 1060 1130 1100 1140 1200 1280 1290 1190 1165 5911 1951 1250 1200 1100 1090 1100 1190 1220 1210 1240 1310 1240 1360 1209 5911 1952 1220 1110 1060 1100 1100 1200 1260 1250 1220 1220 1260 1190 1183 5911 1953 1250 1170 1150 1060 1120 1100 1160 1220 1240 1260 1310 1410 1204 5911 1954 1190 1150 1160 1080 1020 1180 1190 1190 1220 1280 1240 1220 1177 5911 1955 1190 1040 1040 1040 1080 1110 1220 1200 1180 1240 1160 1190 1141 5911 1956 1110 1020 1120 970 1100 1100 1080 1100 1120 1220 1190 1220 1113 5911 1957 1250 1060 1080 1080 1040 1080 1080 1140 1130 1310 1180 1230 1138 5911 1958 1120 1090 950 970 1000 1050 1130 1100 1200 1210 1230 1170 1102 5911 1959 1070 1310 1200 1020 1050 1160 1180 1160 1200 1220 1210 1240 1168 5911 1960 1060 1080 1040 1060 1020 1070 1010 1190 1190 1180 1190 1220 1109 5911 1961 1160 1210 1230 1080 1080 1200 1160 1190 1260 1220 1240 1210 1187 5911 1962 1240 1120 940 1000 970 1110 1120 1140 1170 1270 1200 1190 1122 5911 1963 XX 1100 1070 1060 980 1030 1060 1110 1080 1150 1240 1200 1230 1109 5911 1964 1310 1160 1180 1060 1140 1150 1170 1080 1190 1190 1250 1190 1172 5911 1965 1100 1070 1020 970 970 1070 1090 1080 1200 1200 1170 1140 1090 5911 1966 1090 1040 980 900 1000 1070 1110 1090 1170 1120 1200 1090 1072 5911 1967 1060 1160 1160 1140 1040 1210 1220 1180 1250 1320 1310 1210 1188 5911 1968 1170 1170 1220 1090 1100 1170 1120 1110 1050 1130 1240 1260 1153 5911 1969 1080 1050 1060 1010 1030 1130 1200 1160 1300 1290 1250 1200 1147 5911 1970 1110 1030 910 910 1000 1110 1180 1200 1190 1190 1170 1230 1103 5911 1971 1170 1050 980 980 1060 1070 1200 1250 1240 1220 1230 1220 1139 5911 1972 1130 1140 1030 1030 1040 1090 1160 1190 1180 1200 1210 1320 1143 5911 1973 1210 1140 1080 950 1020 1130 1160 1150 1170 1150 1170 1180 1126 5911 1974 1240 1130 1080 1010 970 1100 1200 1180 1190 1090 1140 1260 1133 5911 1975 1240 1130 1080 1050 1020 1110 1240 1160 1250 1170 1220 1240 1159 5911 1976 1220 1260 1150 1070 1000 1110 1180 1240 1130 1090 1220 1140 1150 5911 1977 1020 1000 1030 1020 1020 1050 1100 1090 1200 1210 1250 1200 1100 5911 1978 313130313031 - 1150 900 1020 900 940 104099999999999999999999999999999999999 5911 1979 980 990 1100 920 870 1060 1090 1120 1220 1160 1210 1290 1085 5911 1980 1100 1130 970 1050 1010 1090 1090 1130 1150 1130 1170 1180 1100 5911 1981 1150 1130 1030 1050 1030 1080 1080 1110 1120 1070 1230 1150 1102 5911 1982 1120 1150 1060 1140 1000 1040 1140 1110 1180 1110 1260 1210 1131 5911 1983 1230 1100 1080 940 1010 1130 1150 1170 1140 1210 1260 1210 1136 5911 1984 31303131 - 1150 1080 930 104099999999999999999999 1150 1160 1160 123099999 5911 1985 1060 1040 1040 970 910 990 1030 1070 1090 1110 1140 1130 1048 5911 1986 1090 930 1070 880 980 1030 1080 1080 1090 1090 1170 1170 1056 5911 1987 3128 - 9999999999 770 950 960 930 1060 1030 1070 1120 1120 116099999 5911 1988 1150 930 930 910 850 1080 1060 1080 1130 1160 1220 1190 1058 5911 1989 1260 1220 1100 940 1040 1070 1110 1120 1180 1140 1180 1200 1130 5911 1990 1210 1230 1140 1150 1080 1040 1110 1110 1060 1140 1070 1220 1130 5911 1991 1290 1170 1060 1070 880 900 960 1130 1170 1160 1160 1270 1101 5911 1992 3129 - 9999999999 1050 940 1080 1120 1170 1200 1200 1230 1130 127099999 5911 1993 3031 - 1390 1200 1060 970 890 930 1010 1090 1100 1030999999999999999 5911 1994 313130313031 - 1140 1070 1120 1020 1040 117099999999999999999999999999999999999 5911 1995 1130 1160 980 930 850 900 1010 1040 990 1020 1030 1000 1003 5911 1996 31XX 1040 840 780 650 650 790 1040 1000 960 1110 110099999 905 5911 1997 31XX 1190 1100 1050 890 740 800 790 900 940 930 93099999 932 5911 1998 31 3031 - 99999 1150 1060 880 940 740 1040 1100 1020 1050999999999999999 5911 1999 312831303130 - 999999999999999999999999999999 870 860 950 850 1090 114099999 5911 2000 1060 1030 850 770 810 850 850 860 930 950 900 890 895 5911 2001 312831303130313130 31 - 999999999999999999999999999999999999999999999 1100 10809999999999 5911 2002 1130 1130 990 970 860 1010 1070 1070 1090 1040 1090 1090 1044 5911 2003 1130 980 1000 990 940 1060 1030 1060 1120 1080 1130 1140 1060 5911 2004 31XX 1070 1030 1050 950 960 1060 1100 1070 1090 1100 112099999 1055 5911 2005 3128 - 9999999999 900 930 930 970 1030 1040 1140 1140 1140 104099999 5911 2006 1150 970 820 950 930 1050 1050 990 1130 1070 1180 1200 1041 5911 2007 1140 950 980 960 910 950 990 1050 1050 1160 1090 1180 1034 5911 2008 1130 1060 950 830 850 900 960 1020 1080 1130 1110 1050 1006 5911 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Barentsburg 025/001 RLR(1972) is 12.9m below BM =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 17-JUN-93 : July-December 1979 for Barentsburg are anomalously high. =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Barentsburg 025/001 RLR(1972) is 12.9m below BM =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 13-OCT-97 : 1979 data revised =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 1999Aug19 : confirmation received that the gauge has been completely destroyed and is impossible to repair =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2002May21 : Barentzburg - gauge apparently functioning again. Gap Nov.1998-June 1999 only. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Nov-2006 : Post 1995 data looks suspect BARENTSBURG II (SPITSBERGEN) 025002 78 04 N 14 15 EK7042002231 46 2 0 39 1948 3129313031 - 9999999999999999999999999 -40 -50 30 50 100 130 15099999 7000 1949 70 150 -40 -40 -160 -110 -10 50 90 120 30 80 18 7000 1950 50 50 40 -70 -70 0 -30 10 70 150 160 60 35 7000 1951 120 70 -30 -40 -30 60 90 80 110 180 110 230 79 7000 1952 90 -20 -70 -30 -30 70 130 120 90 90 130 60 53 7000 1953 120 40 20 -70 -10 -30 30 90 110 130 180 280 75 7000 1954 60 20 30 -50 -110 50 60 60 90 150 110 90 47 7000 1955 60 -90 -90 -90 -50 -20 90 70 50 110 30 60 12 7000 1956 -20 -110 -10 -160 -30 -30 -50 -30 -10 90 60 90 -17 7000 1957 120 -70 -50 -50 -90 -50 -50 10 0 180 50 100 9 7000 1958 -10 -40 -180 -160 -130 -80 0 -30 70 80 100 40 -28 7000 1959 -60 180 70 -110 -80 30 50 30 70 90 80 110 37 7000 1960 -70 -50 -90 -70 -110 -60 -120 60 60 50 60 90 -21 7000 1961 30 80 100 -50 -50 70 30 60 130 90 110 80 56 7000 1962 110 -10 -190 -130 -160 -20 -10 10 40 140 70 60 -7 7000 1963 -30 -60 -70 -150 -100 -70 -20 -50 20 110 70 100 -20 7000 1964 180 30 50 -70 10 20 40 -50 60 60 120 60 43 7000 1965 -30 -60 -110 -160 -160 -60 -40 -50 70 70 40 10 -40 7000 1966 -40 -90 -150 -230 -130 -60 -20 -40 40 -10 70 -40 -58 7000 1967 -70 30 30 10 -90 80 90 50 120 190 180 80 58 7000 1968 40 40 90 -40 -30 40 -10 -20 -80 0 110 130 23 7000 1969 -50 -80 -70 -120 -100 0 70 30 170 160 120 70 17 7000 1970 -20 -100 -220 -220 -130 -20 50 70 60 60 40 100 -27 7000 1971 40 -80 -150 -150 -70 -60 70 120 110 90 100 90 10 7000 1972 0 10 -100 -100 -90 -40 30 60 50 70 80 190 14 7000 1973 80 10 -50 -180 -110 0 30 20 40 20 40 50 -4 7000 1974 110 0 -50 -120 -160 -30 70 50 60 -40 10 130 3 7000 1975 110 0 -50 -80 -110 -20 110 30 120 40 90 110 29 7000 1976 90 130 20 -60 -130 -20 50 110 0 -40 90 10 20 7000 1977 -110 -130 -100 -110 -110 -80 -30 -40 70 80 120 70 -30 7000 1978 313031 - f 10 -230 -100 -230 -190 -70 10999999999999999 210 28099999 7000 1979 f 90 100 -30 -210 -260 -70 200 230 330 270 320 400 115 7000 1980 -30 0 -160 -80 -120 -40 -40 0 20 0 40 50 -30 7000 1981 20 0 -100 -80 -100 -50 -50 -20 -10 -60 100 20 -28 7000 1982 -10 20 -70 10 -130 -90 10 -20 50 -20 130 80 -4 7000 1983 100 -30 -50 -190 -120 0 20 40 10 80 130 80 6 7000 1984 313031 - 30 -50 -200 -60999999999999999 0 20 30 30 10099999 7000 1985 -70 -90 -90 -160 -220 -140 -100 -60 -40 -20 10 0 -82 7000 1986 -40 -200 -60 -250 -150 -100 -50 -50 -40 -40 40 40 -74 7000 1987 28 XX 3099999 -380 -180 -170 -200 -80 -100 -60 -10 -10 30 -103 7000 1988 20 -200 -200 -220 -270 -50 -70 -50 0 30 90 70 -70 7000 1989 120 90 -30 -190 -90 -60 -20 0 50 10 50 70 0 7000 1990 80 100 10 20 -50 -90 -20 -20 -70 10 -60 90 0 7000 1991 160 40 -70 -60 -260 -220 -170 0 30 30 30 150 -29 7000 1992 190 110 -70 -180 -50 -10 40 70 70 90 0 150 34 7000 1993 270 60 -70 -160 -240 -180 -120 -40 -30 -100 130 80 -34 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Possible tide gauge replacement in 1978. Years 1978 and 1979 flagged. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. NY-ALESUND 025021 78 56 N 11 56 E04241994 33 2 0 0 1976 3129313031303131 - 9999999999999999999999999999999999999999 1890 1881 2001 193199999 5100 1977 6 8 1815 1802 1810 1779 1779 1812 1875 1864 1967 1966 2008 1953 1870 5100 1978 1 4 1919 1692 1844 1731 1758 1826 1809 1898 1936 2001 2143 1951 1874 5100 1979 9 5 1841 1885 1798 1659 1744 1852 1892 1884 1990 1955 1955 2055 1877 5100 1980 1 1869 1912 1744 1822 1775 1855 1842 1882 1916 1885 1918 1931 1862 5100 1981 1 1886 1900 1759 1814 1792 1854 1897 1898 1913 1825 1982 1887 1867 5100 1982 2 1883 1935 1851 1912 1779 1812 1911 1863 1927 1886 2035 2004 1899 5100 1983 9 1 2047 1881 1887 1701 1785 1886 1934 1959 1924 1989 2041 1998 1923 5100 1984 2 1968 1912 1769 1826 1827 1834 1880 1967 1896 1931 1947 2011 1898 5100 1985 2 8313014 1 - 1842 1807 1798 17499999999999 1877 1905 1931 1965 1890 185199999 5100 1986 313031 - 1872 1763 1896 1666999999999999999 1831 1836 1965 1879 189699999 5100 1987 2 1231303131 - 1900 1762 1672 168899999999999999999999 1816 1842 1838 188699999 5100 1988 3130313031 - 1865 1678 1669 1650 1605 1788 1751999999999999999999999999999999 99999 1989 3128313031303131 - 9999999999999999999999999999999999999999 1997 1973 2025 204299999 99999 1990 2064 2078 2052 1945 1853 1823 1865 1872 1935 1979 1866 1958 1940 99999 1991 2 2000 1852 1726 1757 1753 1795 1827 1915 1873 1879 1863 2004 1854 99999 1992 2 2019 1901 1838 1706 1830 1856 1882 1882 1832 1805 1892 2039 1874 5100 1993 6 1 2152 1939 1828 1757 1699 1770 1791 1878 1877 1858 1997 1914 1869 5100 1994 1848 1842 1884 1787 1808 1931 1915 1908 1827 1883 1964 2021 1885 5100 1995 3 3 3 1881 1900 1783 1733 1732 1791 1875 1894 1893 1903 1926 1915 1851 5100 1996 8 1970 1801 1816 1713 1714 1809 1866 1837 1810 1909 1905 1807 1831 5100 1997 5 1959 1892 1837 1782 1693 1751 1762 1857 1888 1859 1865 1931 1839 5100 1998 3 1830 1882 1823 1661 1734 1679 1768 1846 1779 1849 1850 1952 1805 5100 1999 1885 1811 1657 1696 1713 1826 1837 1802 1913 1831 1983 1897 1821 5100 2000 1881 1856 1768 1676 1717 1757 1746 1766 1855 1847 1792 1847 1792 5100 2001 1854 1778 1664 1661 1692 1729 1772 1782 1834 1891 1891 1814 1780 5100 2002 1917 1849 1729 1697 1647 1777 1766 1783 1847 1763 1830 1865 1789 5100 2003 1887 1841 1861 1725 1748 1800 1798 1808 1874 1843 1877 1902 1830 5100 2004 1840 1822 1807 1734 1734 1815 1857 1860 1877 1892 1898 1938 1840 5100 2005 1927 1767 1678 1714 1713 1758 1833 1847 1892 1859 1913 1820 1810 5100 2006 1924 1757 1592 1671 1719 1815 1852 1799 1844 1787 1917 1962 1803 5100 2007 1922 1685 1711 1713 1678 1728 1731 1792 1799 1896 1839 1892 1783 5100 2008 1845 1822 1661 1531 1593 1647 1688 1716 1800 1860 1854 1834 1738 5100 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1992 RUSSKAYA GAVAN 030001 76 12 N 62 35 E02241972 99 39 16 0 0 1953 970 1050 1120 980 1010 970 970 1030 1180 1160 1210 1410 1088 6022 1954 1130 1090 1020 860 770 980 1020 1020 1040 1150 1150 1120 1029 6022 1955 1190 880 840 930 900 980 1080 1120 1000 1120 1100 1040 1015 6022 1956 820 880 1050 820 970 980 890 940 1070 1110 1090 1170 983 6022 1957 1200 960 950 940 900 960 900 990 970 1100 1110 1190 1014 6022 1958 1100 910 810 850 790 900 980 1020 1070 1070 1110 900 959 6022 1959 790 1160 1090 840 860 1040 1020 1020 1020 990 1060 970 988 6022 1960 960 910 910 880 850 970 890 920 980 1110 1170 1150 975 6022 1961 960 1040 1060 870 810 930 900 1000 1230 1130 1100 1130 1013 6022 1962 1100 1010 770 770 740 910 910 970 1080 1180 1130 1120 974 6022 1963 990 910 850 890 890 910 1070 880 1060 1250 1120 1120 995 6022 1964 31 XX 1170 1060 970 790 920 97099999 950 970 1120 1060 1000 998 6022 1965 930 900 920 820 820 970 950 930 1010 1190 1090 970 958 6022 1966 930 750 720 620 880 900 970 1030 1090 890 980 960 893 6022 1967 910 960 970 910 810 980 980 960 1110 1150 1010 1000 979 6022 1968 910 940 1010 850 760 990 960 1020 950 1010 970 1120 958 6022 1969 920 970 840 680 690 870 970 950 940 1080 1120 1110 928 6022 1970 960 840 710 730 820 1040 950 990 950 1010 1010 1100 926 6022 1971 1000 870 790 820 960 980 1020 1050 1100 1160 1070 1060 990 6022 1972 1020 970 840 770 740 820 990 1030 970 1070 940 1190 946 6022 1973 1200 1110 1000 800 850 930 980 970 960 1030 1040 990 988 6022 1974 1090 850 940 880 760 900 990 950 950 900 990 1130 944 6022 1975 1110 1090 950 810 810 930 970 950 1080 1040 1070 1220 1002 6022 1976 1030 1090 880 870 700 900 960 1050 1010 940 1160 960 960 6022 1977 800 830 880 760 940 950 950 840 1010 990 990 1130 923 6022 1978 920 780 910 710 820 970 910 880 990 1070 1310 1000 940 6022 1979 950 850 690 600 710 920 880 810 1010 1050 1070 1080 885 6022 1980 800 980 790 840 850 950 910 900 990 1070 990 970 919 6022 1981 1000 970 770 890 830 890 920 990 960 890 1160 970 937 6022 1982 970 1090 910 940 820 870 1000 940 1080 970 1080 1110 982 6022 1983 1140 990 910 770 810 860 1010 1100 980 1070 1200 1200 1004 6022 1984 1080 1090 910 820 830 900 900 980 980 960 1000 1110 963 6022 1985 980 950 900 830 800 880 840 920 990 1160 1010 870 927 6022 1986 920 930 1110 810 850 990 950 900 1090 1090 1270 1130 1004 6022 1987 1080 920 850 850 880 830 1040 930 960 1140 1100 1090 973 6022 1988 1070 820 870 830 750 950 910 870 1010 1110 1170 1210 965 6022 1989 1250 1170 950 770 910 980 1090 1030 1010 990 1050 1270 1039 6022 1990 31 31 - 1060 1170 1150 980 1040 890 93099999 930 1140 11509999999999 6022 1991 3128 313130313031 - 9999999999 850 960 880 92099999999999999999999999999999999999 6022 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Russkaya Gavan 030/001 RLR(1972) is 11.5m below BM SG2F =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Russkaya Gavan 030/001 RLR(1972) is 11.5m below BM SG2F =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 19-JUL-95 : No observations made 1992-93 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 25-JAN-96 : no data for 1994 - gauge malfunction =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-FEB-96 : no data for 1995 - gauge malfunction =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 1999Aug19 : No data after 1991 because site closed. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2002May21 : Russkaya Gavan confirmed as malfunctioned, probably in 1991; =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003May29 : No data in 2002 due to malfunctioning gauge. RUSSKAIA GAVAN II 030003 76 11 N 62 35 EK7042002099 41 0 0 39 1953 0 80 150 10 40 0 0 60 210 190 240 440 119 7000 1954 160 120 50 -110 -200 10 50 50 70 180 180 150 59 7000 1955 220 -90 -130 -40 -70 10 110 150 30 150 130 70 46 7000 1956 -150 -90 80 -150 0 10 -80 -30 100 140 120 200 13 7000 1957 230 -10 -20 -30 -70 -10 -70 20 0 130 140 220 45 7000 1958 130 -60 -160 -120 -180 -70 10 50 100 100 140 -70 -11 7000 1959 -180 190 120 -130 -110 70 50 50 50 20 90 0 17 7000 1960 -10 -60 -60 -90 -120 0 -80 -50 10 140 200 180 5 7000 1961 -10 70 90 -100 -160 -40 -70 30 260 160 130 160 43 7000 1962 130 40 -200 -200 -230 -60 -60 0 110 210 160 150 4 7000 1963 20 -60 -120 -80 -80 -60 100 -90 90 280 150 150 26 7000 1964 31 XX 200 90 0 -180 -50 099999 -20 0 150 90 30 28 7000 1965 -40 -70 -50 -150 -150 0 -20 -40 40 220 120 0 -11 7000 1966 -40 -220 -250 -350 -90 -70 0 60 120 -80 10 -10 -76 7000 1967 -60 -10 0 -60 -160 10 10 -10 140 180 40 30 9 7000 1968 -60 -30 40 -120 -210 20 -10 50 -20 40 0 150 -12 7000 1969 -50 0 -130 -290 -280 -100 0 -20 -30 110 150 140 -42 7000 1970 -10 -130 -260 -240 -150 70 -20 20 -20 40 40 130 -44 7000 1971 30 -100 -180 -150 -10 10 50 80 130 190 100 90 21 7000 1972 50 0 -130 -200 -230 -150 20 60 0 100 -30 220 -24 7000 1973 230 140 30 -170 -120 -40 10 0 -10 60 70 20 18 7000 1974 120 -120 -30 -90 -210 -70 20 -20 -20 -70 20 160 -25 7000 1975 140 120 -20 -160 -160 -40 0 -20 110 70 100 250 32 7000 1976 60 120 -90 -100 -270 -70 -10 80 40 -30 190 -10 -8 7000 1977 -170 -140 -90 -210 -30 -20 -20 -130 40 20 20 160 -47 7000 1978 -50 -190 -60 -260 -150 0 -60 -90 20 100 340 30 -30 7000 1979 -20 -120 -280 -370 -260 -50 -90 -160 40 80 100 110 -85 7000 1980 -170 10 -180 -130 -120 -20 -60 -70 20 100 20 0 -51 7000 1981 30 0 -200 -80 -140 -80 -50 20 -10 -80 190 0 -34 7000 1982 0 120 -60 -30 -150 -100 30 -30 110 0 110 140 11 7000 1983 170 20 -60 -200 -160 -110 40 130 10 100 230 230 34 7000 1984 110 120 -60 -150 -140 -70 -70 10 10 -10 30 140 -7 7000 1985 10 -20 -70 -140 -170 -90 -130 -50 20 190 40 -100 -43 7000 1986 -50 -40 140 -160 -120 20 -20 -70 120 120 300 160 34 7000 1987 110 -50 -120 -120 -90 -140 70 -40 -10 170 130 120 3 7000 1988 100 -150 -100 -140 -220 -20 -60 -100 40 140 200 240 -5 7000 1989 280 200 -20 -200 -60 10 120 60 40 20 80 300 69 7000 1990 31XX 90 200 180 10 70 -80 -40 60 -40 170 17099999 71 7000 1991 3128 3130313031 - 9999999999 -120 -10 -90 -50 20999999999999999999999999999999 7000 1992 312931 - 999999999999999 -300 -10 100 130 90 60 110 100 34099999 7000 1993 31 3130313031 - 460 12099999 -170 -210 -150 -170999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. BELYI NOS 030007 69 36 N 60 13 EK7042002 24 0 0 39 1957 303130 30 - -570 -750 -860999999999999999 -180 -130 -130 -10099999 9099999 7000 1958 3031 - -70 -370 -320 -240 -420 -40 -20 0 90 90999999999999999 7000 1959 3031 - -20 350 320 -210 -70 40 80 90 190 50999999999999999 7000 1960 -20 -120 -120 -170 -250 50 -130 -110 -120 350 150 80 -34 7000 1961 230 10 50 -140 -220 0 -110 -190 110 100 60 100 0 7000 1962 150 180 -90 -120 -150 40 -110 -50 -40 160 140 60 13 7000 1963 170 100 -90 -180 -210 -140 80 -150 50 330 130 110 17 7000 1964 200 -40 -80 -380 -200 150 50 -70 100 290 -30 80 7 7000 1965 40 -110 -40 -100 -180 0 40 -80 80 90 -130 -120 -42 7000 1966 190 -290 -290 -510 -100 10 70 160 200 -50 360 -40 -22 7000 1967 70 240 120 60 -110 70 30 -10 240 320 70 140 102 7000 1968 -40 60 120 -110 -110 20 30 150 50 240 -70 -70 23 7000 1969 -270 -350 -200 -340 -440 -160 60 170 140 220 230 220 -58 7000 1970 70 -130 -320 -330 20 210 -50 -110 -50 -10 140 150 -34 7000 1971 110 -290 -130 -110 0 -180 130 260 340 130 180 190 55 7000 1972 120 -20 -260 -40 -190 -100 110 180 190 440 20 280 62 7000 1973 270 130 70 -160 -90 110 -30 80 130 160 300 -100 72 7000 1974 90 -230 -40 -90 -190 -50 -80 -130 120 -90 -110 240 -45 7000 1975 250 120 80 -170 -180 -20 110 20 340 470 690 460 181 7000 1976 -80 90 -140 -90 -220 -90 -60 90 200 200 430 220 45 7000 1977 -20 -330 -140 -180 -90 0 0 -200 200 50 210 280 -17 7000 1978 20 70 -180 -370 -260 -130 -80 -110 40 230 340 60 -32 7000 1979 28 XX -5099999 -280 -360 -130 0 -40 -160 160 180 50 190 -40 7000 1980 30 31 - 140 360 -60 -80 1099999 -60 -70 4099999 110 13099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KRENKELIA (HEISA OSTROV) 030014 80 37 N 58 03 EK7042002 29 0 0 39 1962 290 240 220 210 200 190 160 150 170 190 130 120 189 7000 1963 110 120 20 -40 -10 40 140 -10 -10 110 130 -50 45 7000 1964 20 0 -10 -120 20 100 90 90 100 120 20 30 39 7000 1965 30 -30 10 -60 -20 90 60 50 80 160 90 70 45 7000 1966 80 -40 -100 -160 90 100 110 140 220 80 90 -40 48 7000 1967 80 130 60 70 10 80 70 60 160 220 110 90 95 7000 1968 10 10 100 -10 10 120 100 70 20 90 50 100 56 7000 1969 -110 -120 -30 -60 -20 50 40 70 60 70 120 60 12 7000 1970 10 -50 -220 -130 -20 120 40 60 30 30 40 30 -5 7000 1971 20 -200 -130 -150 -10 0 20 60 110 100 120 30 -1 7000 1972 70 30 -70 -60 -100 -70 40 30 10 100 -60 170 8 7000 1973 140 30 0 -190 -60 30 30 30 60 50 40 20 15 7000 1974 40 -100 -10 -20 -100 0 40 40 50 -20 -20 70 -2 7000 1975 120 70 -30 -130 -130 -30 30 40 80 70 50 160 25 7000 1976 0 100 -20 -50 -120 20 70 110 80 30 80 40 28 7000 1977 -140 -90 -10 -30 -20 -30 10 -80 80 40 40 120 -9 7000 1978 100 -30 -20 -130 -80 0 0 -10 60 100 190 20 17 7000 1979 -110 -100 -300 -310 -220 -40 -70 -130 -10 0 -70 70 -108 7000 1980 -150 -70 -280 -220 -200 -80 -90 -110 -70 -50 -100 -100 -127 7000 1981 -50 -140 -150 -60 -50 -40 20 -40 -40 -110 80 70 -42 7000 1982 60 80 -80 -20 -110 -30 80 -20 60 -60 -10 40 -2 7000 1983 130 100 -100 -220 -140 -20 0 70 -50 70 160 110 9 7000 1984 -30 -50 -140 -180 -100 -60 -60 0 -10 -50 -30 30 -57 7000 1985 -60 -100 -70 -130 -200 -70 -90 -40 10 120 20 -30 -53 7000 1986 -50 -50 10 -120 -160 -30 -100 -100 -20 10 30 30 -46 7000 1987 10 -70 -150 -160 -120 -110 0 -80 -80 -40 -70 -40 -76 7000 1989 170 120 -60 -190 -70 -10 -30 -40 -20 -40 -50 120 -9 7000 1990 -70 40 80 0 70 -70 -50 50 -40 90 20 40 14 7000 1991 3130313031 - 80 -20 -170 -50 -60 -30 10999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MALYE KARMAKULY 030016 72 22 N 52 42 EK7042002 37 0 0 39 1950 360 240 360 220 450 760 -50 -50 40 120 30 50 210 7000 1951 190 -60 -150 -80 -100 -40 -10 -70 30 150 30 -170 -23 7000 1952 -130 -50 -50 -40 -40 20 -10 -30 10 -10 -40 -90 -39 7000 1953 10 -160 0 -170 -110 -100 -10 -30 100 80 60 230 -7 7000 1954 40 -20 -40 -90 -230 -10 -70 0 0 130 30 0 -22 7000 1955 150 0 -110 -60 -30 30 0 10 0 130 90 -70 12 7000 1956 3131 - -130 -170 60 -140 -10 -109999999999 -40 0 -70 099999 7000 1957 240 50 60 -180 -180 -160 -190 -60 -110 40 10 40 -37 7000 1958 -160 -240 -290 -200 -120 -20 -130 -230 -140 -140 0 -180 -154 7000 1959 -370 60 0 -280 -250 -180 -70 -40 70 50 -10 -10 -87 7000 1960 -40 -70 170 160 420 620 -150 -80 30 110 -20 -90 88 7000 1961 313130313031 - -30 80 180 60 50 -7099999999999999999999999999999999999 7000 1962 3128 31 30 - 9999999999 390 -120 -130 0 5099999 220 27099999 19099999 7000 1963 50 330 -30 -90 -40 0 70 -50 60 220 200 160 72 7000 1964 250 80 40 -170 -60 60 -10 -60 110 190 160 120 59 7000 1965 40 0 30 -30 -10 70 -30 -20 20 100 -10 -60 8 7000 1966 -10 -270 -190 -310 -230 -180 -70 10 110 40 180 -70 -81 7000 1967 -20 100 130 0 -80 20 -10 -40 0 30 0 0 10 7000 1968 -260 -110 -10 -130 -140 -60 -60 -20 -100 0 0 50 -70 7000 1969 -200 -200 -100 -220 -250 -130 -80 -110 0 100 90 0 -91 7000 1970 -60 -180 -300 -230 -180 0 -90 -70 -50 20 50 70 -85 7000 1971 20 -190 -190 -200 -140 -140 -30 0 40 110 70 60 -48 7000 1972 -10 0 -110 -180 -240 -200 -80 -80 -50 40 -90 180 -68 7000 1973 60 0 -10 -250 -200 -80 -80 -10 30 90 90 -30 -33 7000 1974 20 -120 -20 40 -110 10 -10 40 10 -80 -50 70 -16 7000 1975 30 XX 90 110 20 -150 -130 -40 -10 -1099999 80 50 150 14 7000 1976 -20 60 -120 -50 -190 -120 0 100 0 -80 -40 -30 -41 7000 1977 28 31 - 4099999 60 -110 -80 -30 -80 -90 50 10 809999999999 7000 1978 31 31 - -190 -210 -60 -190 -180 -120 -100 -80 5099999 2709999999999 7000 1979 31 30 - 99999 -100 -120 -130 0 160 10 -40 140 10099999 2099999 7000 1980 30 XX -20 0 -100 -90 -5099999 40 -170 10 10 0 -10 -35 7000 1995 3128313031 3130 - 9999999999999999999999999 -50 70 0 1509999999999 16099999 7000 1996 30 30 - 50 -10 40 50 11099999 20 -70 170 -8099999 20099999 7000 1997 3031 31 - 140 160 20 50 1209999999999 70 9099999 400 39099999 7000 1998 30 31 - 220 530 410 20 5099999 380 140 15099999 250 12099999 7000 1999 31 313031 - 80 -80 190 210 270 28099999 110 15099999999999999999999 7000 2000 31 30 3031 - 99999 60 20 200 28099999 30 100 100 30999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MURMANSK 030018 68 58 N 33 03 E02241972274 57 6 0 0 1952 4580 4420 4350 4470 4440 4500 4550 4580 4620 4470 4470 4500 4496 2508 1953 4630 4430 4590 4390 4470 4400 4480 4450 4580 4580 4690 4710 4533 2508 1954 4580 4400 4500 4450 4360 4540 4500 4540 4600 4660 4520 4590 4520 2508 1955 4650 4380 4340 4360 4440 4560 4570 4520 4520 4630 4610 4500 4506 2508 1956 4460 4250 4430 4320 4490 4470 4410 4490 4550 4580 4490 4540 4457 2508 1957 4570 4480 4410 4360 4390 4520 4430 4440 4460 4640 4640 4690 4503 2508 1958 4470 4440 4310 4290 4350 4430 4520 4410 4550 4550 4570 4470 4447 2508 1959 4450 4690 4580 4340 4470 4500 4480 4520 4670 4560 4460 4360 4507 2508 1960 4410 4400 4320 4340 4350 4450 4360 4380 4370 4440 4380 4420 4385 2508 1961 4400 4470 4620 4390 4340 4520 4470 4450 4590 4550 4580 4630 4501 2508 1962 4610 4480 4350 4340 4380 4510 4440 4500 4500 4640 4490 4590 4486 2508 1963 4480 4410 4360 4280 4330 4430 4480 4520 4520 4650 4570 4610 4470 2508 1964 4700 4420 4330 4280 4260 4490 4500 4440 4580 4540 4620 4580 4478 2508 1965 4450 4430 4400 4540 4360 4470 4470 4450 4470 4640 4510 4430 4452 2508 1966 4390 4380 4330 4230 4360 4390 4490 4480 4620 4450 4490 4310 4410 2508 1967 4420 4480 4570 4420 4310 4500 4480 4440 4540 4670 4520 4580 4494 2508 1968 4460 4500 4560 4360 4310 4480 4410 4450 4350 4510 4480 4540 4451 2508 1969 4290 4260 4340 4280 4260 4380 4420 4410 4490 4640 4600 4450 4402 2508 1970 4460 4400 4270 4270 4300 4430 4420 4400 4470 4530 4520 4590 4422 2508 1971 4540 4380 4350 4350 4370 4410 4440 4500 4570 4630 4610 4620 4481 2508 1972 4440 4390 4430 4330 4290 4360 4440 4520 4560 4650 4620 4770 4483 2508 1973 4610 4590 4560 4400 4360 4440 4300 4400 4430 4480 4480 4440 4458 2508 1974 4470 4360 4290 4300 4250 4360 4350 4350 4430 4250 4230 4580 4352 2508 1975 4510 4500 4400 4310 4350 4460 4410 4410 4540 4490 4460 4590 4452 2508 1976 4570 4440 4390 4440 4260 4400 4470 4470 4490 4360 4480 4390 4430 2508 1977 4340 4460 4390 4340 4310 4410 4380 4370 4480 4410 4530 4540 4413 2508 1978 4490 4260 4350 4260 4250 4360 4330 4370 4430 4570 4660 4410 4396 2508 1979 4340 4390 4300 4190 4340 4460 4430 4400 4610 4510 4520 4640 4428 2508 1980 4420 4430 4270 4330 4340 4400 4350 4360 4430 4480 4540 4550 4408 2508 1981 4500 4410 4360 4370 4270 4440 4430 4460 4460 4430 4590 4540 4438 2508 1982 4530 4580 4390 4450 4390 4480 4480 4460 4590 4500 4740 4680 4522 2508 1983 4720 4550 4530 4280 4370 4300 4520 4620 4590 4780 4780 4680 4561 2508 1984 4540 4410 4290 4320 4330 4420 4370 4450 4390 4550 4540 4720 4445 2508 1985 4430 4330 4280 4400 4320 4400 4350 4400 4520 4700 4560 4460 4430 2508 1986 4380 4380 4520 4340 4470 4550 4430 4400 4610 4610 4670 4630 4500 2516 1987 4440 4480 4310 4340 4370 4360 4430 4240 4490 4480 4480 4630 4420 2516 1988 4480 4270 4270 4340 4300 4420 4340 4390 4490 4600 4720 4640 4439 2516 1989 4750 4700 4500 4280 4510 4480 4570 4530 4610 4610 4600 4740 4573 2516 1990 4570 4770 4680 4440 4500 4390 4420 4450 4430 4590 4570 4620 4535 2516 1991 4710 4480 4390 4450 4460 4500 4570 4570 4710 4600 4650 4790 4574 2516 1992 4850 4690 4560 4360 4510 4580 4600 4610 4530 4600 4580 4820 4608 2516 1993 4950 4730 4530 4370 4410 4550 4510 4480 4520 4600 4510 4600 4563 2516 1994 3130313130313031 - 4580 4510 4480 4370999999999999999999999999999999999999999999999 2516 1995 31 30 - 99999 4770 4530 4600 4470 4530 4590 464099999 4770 4680 467099999 2516 1996 4640 4460 4440 4480 4490 4620 4630 4500 4550 4750 4720 4630 4575 2516 1997 4810 4700 4680 4570 4450 4510 4500 4570 4730 4770 4610 4660 4630 2516 1998 28 30 - 467099999 4490 4380 4510 4490 4610 4560 4570 467099999 480099999 2516 1999 28 XX 463099999 4390 4520 4520 4590 4700 4670 4720 4780 4820 4830 4652 2516 2000 4850 4820 4770 4560 4620 4650 4560 4620 4640 4640 4550 4670 4662 2516 2001 4700 4570 4560 4540 4580 4530 4580 4660 4630 4830 4830 4690 4642 2516 2002 4860 4780 4670 4520 4590 4620 4590 4620 4720 4680 4640 4640 4660 2516 2003 31 XX 99999 4710 4760 4550 4590 4630 4550 4670 4730 4740 4700 4820 4680 2516 2004 4600 4660 4520 4480 4580 4630 4590 4590 4750 4720 4840 4880 4653 2516 2005 4780 4580 4540 4580 4570 4640 4660 4710 4850 4790 4860 4660 4690 2516 2006 4720 4660 4580 4540 4590 4710 4720 4590 4770 4720 4800 4920 4693 2516 2007 4880 4530 4630 4670 4610 4660 4650 4580 4670 4680 4650 4720 4661 2516 2008 4580 4650 4480 4340 4410 4470 4500 4510 4500 4680 4630 4590 4528 2516 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Murmansk 030/018 RLR(1972) is 21.8m below BM =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Murmansk 030/018 RLR(1972) is 21.8m below BM =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Consider data suspect October 1995 onwards. MURMANSK II 030019 68 58 N 33 03 EK7042002274 41 0 0 39 1952 110 -50 -120 0 -30 30 80 110 150 0 0 30 26 7000 1953 160 -40 120 -80 0 -70 10 -20 110 110 220 240 64 7000 1954 110 -70 30 -20 -110 70 30 70 130 190 50 120 51 7000 1955 180 -90 -130 -110 -30 90 100 50 50 160 140 30 38 7000 1956 -10 -220 -40 -150 20 0 -60 20 80 110 20 70 -12 7000 1957 100 10 -60 -110 -80 50 -40 -30 -10 170 170 220 33 7000 1958 0 -30 -160 -180 -120 -40 50 -60 80 80 100 0 -23 7000 1959 -20 220 110 -130 0 30 10 50 200 90 -10 -110 35 7000 1960 -60 -70 -150 -130 -120 -20 -110 -90 -100 -30 -90 -50 -85 7000 1961 -70 0 150 -80 -130 50 0 -20 120 80 110 160 31 7000 1962 140 10 -120 -130 -90 40 -30 30 30 170 20 120 16 7000 1963 10 -60 -110 -190 -140 -40 10 50 50 180 100 140 1 7000 1964 230 -50 -140 -190 -210 20 30 -30 110 70 150 110 8 7000 1965 -20 -40 -70 70 -110 0 0 -20 0 170 40 -40 -2 7000 1966 -80 -90 -140 -240 -110 -80 20 10 150 -20 20 -160 -60 7000 1967 -50 10 100 -50 -160 30 10 -30 70 200 50 110 24 7000 1968 -10 30 90 -110 -160 10 -60 -20 -120 40 10 70 -19 7000 1969 -180 -210 -130 -190 -210 -90 -50 -60 20 170 130 -20 -68 7000 1970 -10 -70 -200 -200 -170 -40 -50 -70 0 60 50 120 -48 7000 1971 70 -90 -120 -120 -100 -60 -30 30 100 160 140 150 12 7000 1972 -30 -80 -40 -140 -180 -110 -30 50 90 180 150 300 14 7000 1973 140 120 90 -70 -110 -30 -170 -70 -40 10 10 -30 -13 7000 1974 0 -110 -180 -170 -220 -110 -120 -120 -40 -220 -240 110 -118 7000 1975 40 30 -70 -160 -120 -10 -60 -60 70 20 -10 120 -18 7000 1976 100 -30 -80 -30 -210 -70 0 0 20 -110 10 -80 -40 7000 1977 -130 -10 -80 -130 -160 -60 -90 -100 10 -60 60 70 -57 7000 1978 20 -210 -120 -210 -220 -110 -140 -100 -40 100 190 -60 -74 7000 1979 -130 -80 -170 -280 -130 -10 -40 -70 140 40 50 170 -42 7000 1980 -50 -40 -200 -140 -130 -70 -120 -110 -40 10 70 80 -62 7000 1981 30 -60 -110 -100 -200 -30 -40 -10 -10 -40 120 70 -32 7000 1982 60 110 -80 -20 -80 10 10 -10 120 30 270 210 52 7000 1983 250 80 60 -190 -100 -170 50 150 120 310 310 210 91 7000 1984 70 -60 -180 -150 -140 -50 -100 -20 -80 80 70 250 -25 7000 1985 -40 -140 -190 -70 -150 -70 -120 -70 50 230 90 -10 -40 7000 1986 -90 -90 50 -130 0 80 -40 -70 140 140 200 160 30 7000 1987 -30 10 -160 -130 -100 -110 -40 -230 20 10 10 160 -50 7000 1988 10 -190 -200 -130 -170 -40 -130 -70 20 140 240 180 -28 7000 1989 270 240 40 -190 40 10 110 70 150 140 140 280 108 7000 1991 230 20 -80 -20 -10 30 100 110 250 130 190 320 106 7000 1992 390 230 110 -110 40 110 140 150 60 130 110 350 143 7000 1993 480 280 90 -60 -40 120 50 20 70 140 60 130 111 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. CAPE ZHELANIJA 030021 76 57 N 68 35 E02249999 3 0 0 0 1957 312831303130 - 999999999999999999999999999999 550 620 620 670 670 73099999 99999 1958 3130 - 680 570 540 6609999999999 520 700 670 660 830 71099999 99999 1959 590 890 780 490 590 670 670 600 640 620 620 660 652 99999 LINAKHAMARI 030025 69 39 N 31 22 E06061938 9 5 0 0 1931 1897 1887 1883 1767 1807 1926 1945 1950 2022 2173 1989 2160 1951 5040 1932 2216 2018 1910 1843 1790 1857 1939 2026 2135 2045 2113 2218 2009 5040 1933 2073 1942 1923 1930 1821 1877 2008 1999 1972 2065 2041 2066 1976 5040 1934 2207 2107 1803 1827 1944 1921 1836 1857 1903 2060 2077 1996 1962 5040 1935 2014 2073 1951 1758 1857 1907 1974 1922 1991 1950 1931 1897 1935 5040 1936 1877 1851 1812 1794 1769 1903 1910 1959 2058 2081 2106 2234 1946 5040 1937 2019 1958 1709 1753 1830 1907 1845 1875 1993 2042 2062 1871 1905 5040 1938 2017 2050 2101 1950 1831 1898 1861 1977 1992 2023 2162 1921 1982 5040 1939 31XX 1974 2086 1860 1900 1798 1929 1894 1916 1976 1968 200899999 1937 5040 FORMERLY IN FINLAND AND KNOWN AS LIINAHAMARI =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Linakhamari 030/025 RLR(1938) is 10.1m below BMF1 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Linakhamari 030/025 RLR(1938) is 10.1m below BMF1 CAPE CHELYUSKIN 030031 77 43 N104 17 E02249999 3 0 0 0 1957 312831303130 - 999999999999999999999999999999 680 710 690 580 620 72099999 99999 1958 31 XX 640 580 510 520 440 660 660 750 73099999 830 770 644 99999 1959 620 950 920 660 670 830 740 620 640 580 740 920 741 99999 CAPE SCHMIDT 030041 68 55 N179 28 E02249999 3 0 0 0 1957 312831303130 - 999999999999999999999999999999 1690 1800 1480 1440 1230 127099999 99999 1958 1260 1110 1120 1160 1160 1220 1320 1380 1670 1770 1460 1200 1319 99999 1959 1010 1370 1190 1070 1210 1470 1620 1200 1120 1540 1320 1560 1307 99999 BOLVANSKII NOS (FEDOROVA) 030305 70 27 N 59 05 EK7042002 43 0 0 39 1951 0 -150 -200 -130 -80 -70 0 -60 20 150 90 190 -19 7000 1952 -140 -190 -100 -120 -40 -10 0 0 0 -20 -80 -70 -64 7000 1953 0 -150 0 -190 -90 -110 0 -70 130 170 90 330 11 7000 1954 170 -100 -30 -150 -250 -50 -40 0 0 180 100 20 -12 7000 1955 150 -200 -260 -160 -160 0 40 110 10 190 110 0 -13 7000 1956 -100 -300 -40 -260 -100 -30 -90 -80 30 70 -40 30 -75 7000 1957 150 -120 -130 -100 -90 30 -70 -20 0 30 -50 0 -30 7000 1958 -170 -230 -210 -160 -260 -140 0 40 190 120 280 40 -41 7000 1959 -170 140 170 -150 -30 10 10 20 170 70 70 0 25 7000 1960 -90 -120 -120 -160 -210 -10 -160 -110 -20 230 200 150 -35 7000 1961 -70 30 60 -70 -130 -20 -90 -100 140 100 60 40 -5 7000 1962 10 -40 -220 -140 -170 40 -50 0 30 210 110 120 -8 7000 1963 110 0 -110 -180 -170 -60 20 -120 0 170 50 50 -20 7000 1964 170 -20 -100 -280 -130 70 -30 -60 100 150 200 100 14 7000 1965 -10 -140 -100 -110 -70 30 20 -30 50 170 -40 -50 -22 7000 1966 70 -190 -200 -300 -90 -10 40 80 150 0 180 -110 -31 7000 1967 30 70 60 0 -70 50 0 -50 110 200 20 50 39 7000 1968 -80 10 70 -100 -100 30 30 50 -10 100 40 0 3 7000 1969 -250 -230 -80 -150 -200 -40 20 0 20 120 130 60 -49 7000 1970 0 -130 -310 -180 -130 -10 -20 -70 -40 0 30 140 -60 7000 1971 160 -190 -110 -140 -80 -80 -40 80 100 100 150 90 5 7000 1972 20 60 -100 -160 -200 -140 -20 10 0 140 -100 110 -31 7000 1973 110 20 0 -210 -120 70 -60 10 50 70 130 0 6 7000 1974 50 -230 110 -100 -250 -100 -60 -50 50 -100 -80 100 -54 7000 1975 160 80 -10 -180 -360 -180 0 40 220 240 0 10 1 7000 1976 -80 -10 -230 -40 -30 40 -60 50 100 50 140 -400 -40 7000 1977 -140 -310 -230 -290 -310 -80 -110 -130 60 -20 -80 180 -120 7000 1978 90 -60 -40 -160 -180 -170 -140 -30 -20 110 340 130 -11 7000 1979 -80 -140 -50 -300 -210 -70 -80 30 90 110 150 220 -27 7000 1980 100 100 -90 -240 -150 -120 -100 -90 -20 90 40 -80 -47 7000 1981 110 30 -140 -60 -160 -80 -120 110 -30 -80 110 80 -20 7000 1982 0 50 -90 -120 -160 -10 -40 40 140 -40 240 230 19 7000 1983 190 70 -60 -230 -170 -60 50 180 80 160 380 210 67 7000 1984 80 80 -20 -20 -130 -110 -40 10 0 -70 -20 110 -11 7000 1985 -20 -160 -140 -150 -170 -90 -50 40 120 310 150 20 -11 7000 1986 -60 -30 80 -160 -110 60 80 -90 140 220 230 150 43 7000 1987 70 -30 -170 -160 -130 -120 80 20 30 230 200 270 25 7000 1988 230 -220 -150 -90 -110 30 -20 30 160 350 350 370 79 7000 1989 220 230 -10 -190 0 80 190 220 260 280 260 380 160 7000 1990 20 150 180 0 170 30 70 140 80 310 250 270 140 7000 1991 250 60 -100 -20 -10 50 150 160 290 300 250 260 137 7000 1992 400 220 150 -100 30 90 140 40 0 200 140 380 142 7000 1993 3031 - 450 250 90 -40 -60 10 -10 0 70 160999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. UGORSKII SHAR (UGORSKII SHAR PROLIV) 030308 69 49 N 60 45 EK7042002 40 0 0 39 1950 170 100 110 -140 10 50 -10 -90 -70 40 10 20 17 7000 1951 50 -150 -210 -120 -50 -40 50 -10 80 260 170 290 28 7000 1952 -10 -230 -220 -140 -100 -60 40 80 70 40 -60 -50 -52 7000 1953 0 -160 0 -220 -110 -70 30 -40 120 180 90 380 19 7000 1954 90 0 30 -130 -240 0 0 10 10 190 110 0 6 7000 1955 150 -160 -120 -120 -80 30 70 140 30 250 200 10 35 7000 1956 -130 -300 -40 -280 -140 -50 -120 -120 30 80 10 130 -76 7000 1957 110 -120 -20 30 -100 0 -110 -80 -70 -40 -60 0 -38 7000 1958 -80 -140 -270 -230 -270 -110 0 -10 160 80 240 40 -49 7000 1959 -160 130 80 -180 -10 40 60 70 160 100 110 70 38 7000 1960 -50 -60 -130 -180 -200 -20 -110 -60 -70 150 110 130 -41 7000 1961 60 110 80 -60 -110 -20 -200 -50 180 130 50 100 22 7000 1962 120 50 -140 -110 -130 60 -60 -30 -10 140 70 90 4 7000 1963 100 60 -60 -150 -150 -30 40 -80 60 220 100 180 24 7000 1964 90 -130 -100 -280 -60 90 20 -60 90 150 290 100 17 7000 1965 60 -50 -80 -180 -150 -40 50 -20 40 170 -10 -40 -20 7000 1966 120 -70 -70 -180 10 80 130 160 200 50 160 -70 44 7000 1967 90 110 60 -10 -90 80 30 -40 130 220 60 90 60 7000 1968 -90 -30 170 -30 -70 40 110 120 50 140 20 50 41 7000 1969 -150 -130 -50 -120 -210 -20 60 70 20 100 90 20 -26 7000 1970 10 -130 -290 -180 -110 50 0 30 90 0 90 170 -22 7000 1971 140 -240 -200 -230 -100 -100 10 110 140 130 150 100 -6 7000 1972 10 70 -110 -180 -200 -170 20 40 30 170 -160 170 -25 7000 1973 160 40 10 -210 -130 50 0 80 70 130 190 -20 31 7000 1974 40 -240 -100 -90 -240 -90 -30 -20 80 -90 -70 90 -62 7000 1975 90 90 20 -170 -150 -70 100 110 230 270 220 170 76 7000 1976 -50 60 -160 -90 -160 -60 20 80 90 30 140 -70 -15 7000 1977 -120 -220 -120 -160 -110 -30 -50 -40 200 10 70 240 -26 7000 1978 100 -140 -150 -260 -160 -110 -40 -100 20 180 360 70 -18 7000 1979 -70 -180 -280 -290 -170 170 210 -80 170 180 120 240 3 7000 1980 40 70 -200 -240 -60 20 10 20 150 90 70 20 -1 7000 1981 30 -10 -110 -30 -150 -90 -70 0 20 -90 100 -20 -36 7000 1982 40 130 -190 -70 -180 20 80 140 210 10 210 260 54 7000 1983 150 70 -40 -150 -140 -30 120 220 120 150 460 220 96 7000 1984 60 80 -10 -10 -150 -10 -20 30 50 -20 -70 90 1 7000 1985 -10 -160 -130 -100 -110 -80 -200 -10 -30 180 0 -140 -65 7000 1986 -100 -70 30 -200 -150 30 30 -90 80 180 180 110 3 7000 1987 50 -110 -180 -90 -60 -40 30 -40 10 260 160 210 18 7000 1988 90 -160 -140 -90 -100 -20 -50 -30 130 210 110 110 6 7000 1989 160 210 80 -230 0 110 100 70 170 190 140 160 96 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. AMDERMA 030310 69 45 N 61 42 EK7042002 51 0 0 39 1950 180 130 110 -160 -20 10 -10 -100 -70 80 0 0 12 7000 1951 0 -160 -220 -160 -60 0 50 -20 80 250 150 260 16 7000 1952 -60 -220 -230 -170 -120 -80 10 40 30 100 -80 -70 -70 7000 1953 -40 -190 -10 -170 -140 -90 0 -50 140 180 50 340 3 7000 1954 40 -90 -50 -180 -280 -90 -50 0 -50 150 60 -40 -48 7000 1955 100 -200 -160 -160 -130 -20 30 110 0 180 130 -40 -12 7000 1956 -160 -360 -80 -300 -120 -80 -110 -200 0 60 -60 100 -108 7000 1957 150 -140 -120 -80 -150 -60 -190 -150 -70 60 -110 -60 -76 7000 1958 -130 -260 -340 -270 -280 -140 -40 -30 100 60 200 -10 -94 7000 1959 -180 160 160 -220 -110 -50 -10 30 160 60 70 30 7 7000 1960 -100 -70 -280 -250 -300 30 -50 30 0 270 30 -50 -62 7000 1961 -70 50 90 -50 -60 -10 -110 -40 170 130 60 100 21 7000 1962 100 10 -200 -170 -160 0 -90 -30 -10 130 60 70 -24 7000 1963 60 -10 -110 -210 -160 -90 10 -100 30 170 50 90 -22 7000 1964 120 -160 -140 -330 -160 0 0 -40 70 140 310 160 -2 7000 1965 0 -90 -110 -180 -130 40 10 -30 90 190 -20 -30 -21 7000 1966 130 -100 -110 -220 0 80 140 180 230 50 180 -100 39 7000 1967 40 70 10 -30 -110 50 20 0 160 240 80 100 52 7000 1968 -70 0 100 -90 -80 50 100 20 30 80 40 0 15 7000 1969 -200 -270 -90 -150 -200 -50 -10 0 10 100 120 40 -57 7000 1970 10 -140 -290 -200 -130 40 -30 -60 0 -30 40 90 -58 7000 1971 40 -330 -260 -190 -20 -40 10 90 170 140 150 90 -10 7000 1972 30 100 -80 -130 -130 -110 0 50 30 200 -90 200 6 7000 1973 90 -10 -20 -230 -140 80 20 10 120 170 130 -40 15 7000 1974 20 -230 -90 -120 -270 -110 -60 -70 100 -150 -100 70 -83 7000 1975 130 90 -20 -220 -170 0 50 0 150 200 130 200 45 7000 1976 -60 60 -160 -110 -200 -70 -50 30 130 70 120 -20 -23 7000 1977 -180 -280 -130 -200 -90 -40 -20 -190 20 -120 -70 190 -91 7000 1978 40 -160 -180 -290 -190 -100 -60 -90 -30 60 260 20 -59 7000 1979 -140 -170 -350 -350 -200 0 -50 -100 110 90 0 110 -87 7000 1980 -50 -30 -230 -180 -110 30 -60 40 170 210 100 40 -6 7000 1981 120 0 -150 -60 -190 -90 -90 -80 30 -110 110 70 -37 7000 1982 -10 50 -250 -150 -250 -80 50 150 240 90 110 180 10 7000 1983 140 30 -10 -120 -210 -60 70 190 50 80 330 180 56 7000 1984 30 80 -60 -50 -160 -90 -130 -70 -40 -110 -50 170 -40 7000 1985 -30 -180 -90 -120 -120 -30 -150 -30 -10 140 -10 -70 -58 7000 1986 -100 -80 -50 -350 -260 -10 40 -80 130 230 220 150 -13 7000 1987 30 -90 -180 -120 -60 10 20 -60 -30 290 160 200 15 7000 1988 130 -240 -180 -130 -110 0 -10 0 130 250 210 230 24 7000 1989 150 160 -70 -210 0 60 130 140 190 210 210 220 99 7000 1990 -30 30 120 0 190 0 0 70 20 260 190 180 87 7000 1991 140 20 -120 10 80 50 130 110 210 290 220 200 112 7000 1992 30 313031 - 320 130 20 -310 9099999 140 70 -3099999999999999999999 7000 1993 31 XX 99999 260 30 -50 -50 -30 -40 0 160 200 340 130 85 7000 1994 3031 - 20 0 -109999999999 100 50 90 140 320 220 21099999 7000 1995 30 30 - 170 140 -40 -30 -4099999 90 130 70 23099999 19099999 7000 1996 31 XX 99999 -30 -100 -160 -100 50 130 210 -10 310 190 50 50 7000 1997 230 40 0 20 -110 110 170 140 170 190 240 200 117 7000 1998 80 30 -20 -90 0 60 50 90 120 80 0 260 56 7000 1999 3130 - -10 0 -210 -809999999999 240 160 230 250 220 25099999 7000 2000 60 160 60 0 40 120 20 150 220 150 20 140 95 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. UST KARA 030315 69 15 N 64 31 EK7042002 45 0 0 39 1950 140 100 90 -140 -20 130 -20 -120 -90 130 -20 -50 11 7000 1951 -10 -130 -170 -130 0 110 50 -10 80 190 110 200 25 7000 1952 -40 -200 -210 -180 -70 90 -40 10 -10 30 180 210 -19 7000 1953 -20 -210 -20 -160 -60 -60 -40 -90 120 120 30 300 -6 7000 1954 30 -50 0 -190 -220 140 -70 -70 -150 110 110 100 -21 7000 1955 200 -140 -210 -70 -10 50 10 80 70 250 50 0 25 7000 1956 -160 -370 -30 -130 100 0 -10 -100 60 80 -40 100 -40 7000 1957 50 -70 -50 0 0 350 -110 -170 -80 -60 -70 110 -8 7000 1958 -60 -90 -190 -180 -230 70 -30 -70 110 80 170 -10 -36 7000 1959 -170 130 160 -170 -10 150 -170 50 150 90 110 -10 25 7000 1960 -110 -120 -150 -190 -230 230 -90 -30 -60 170 210 150 -18 7000 1961 40 100 50 -80 -100 130 -300 -150 120 100 -10 90 -2 7000 1962 80 0 -170 -120 -160 130 -190 -130 -90 60 -20 0 -52 7000 1963 70 -30 -120 -200 -170 200 10 -70 90 150 70 110 9 7000 1964 170 -100 -70 -250 30 200 -40 -60 50 150 110 60 21 7000 1965 -50 -190 -150 -240 -190 230 70 40 110 110 -50 -130 -36 7000 1966 80 -190 -240 -360 -50 380 50 80 160 -10 200 -160 -5 7000 1967 -60 40 -100 -90 -170 370 50 -80 80 200 10 100 28 7000 1968 -130 -140 70 -110 -120 100 100 60 -10 100 70 -10 -1 7000 1969 -210 -270 -120 -190 -220 290 0 0 -10 60 60 -90 -58 7000 1970 -110 -160 -320 -200 -110 320 -40 -130 -90 -50 70 140 -57 7000 1971 100 -330 -240 -230 -150 280 20 120 190 130 100 40 4 7000 1972 20 60 -170 -190 -230 120 20 50 -10 130 -190 140 -21 7000 1973 130 -30 -50 -300 -100 210 -10 0 50 70 40 -90 -7 7000 1974 -10 -260 -90 -110 -270 140 -100 -110 50 -80 -90 50 -73 7000 1975 110 40 -40 -240 -140 380 90 30 170 230 180 120 77 7000 1976 -70 60 -170 -100 -170 220 -30 60 90 50 120 -80 -3 7000 1977 -190 -270 -140 -30 210 -10 -40 -120 140 -20 30 200 -19 7000 1978 40 -140 -130 -200 -210 90 90 -70 -70 20 230 190 -13 7000 1979 40 -20 -230 -190 -280 380 -150 -260 -110 90 0 -110 -71 7000 1980 -150 -70 -270 -210 -100 280 -20 -20 40 40 -80 -50 -51 7000 1981 150 60 -130 -30 -160 220 -140 -110 10 -90 80 100 -5 7000 1982 20 30 -220 -120 -230 40 140 170 250 200 180 100 46 7000 1983 130 -60 -200 -330 -310 100 0 140 90 60 50 40 -24 7000 1984 40 220 240 -210 -140 220 -40 20 -90 -160 -70 150 14 7000 1985 -10 -230 -250 -320 -180 -30 -90 -30 50 180 40 -20 -73 7000 1986 50 80 240 -200 -100 140 100 -30 90 190 240 160 80 7000 1987 50 -100 -130 -20 -20 340 30 -50 -50 220 110 210 50 7000 1994 3128 30313130313031 - 9999999999 -320 -380 -2909999999999999999999999999999999999999999 7000 1995 31283130 30 - 99999999999999999999 -13099999 100 170 120 130 180 28099999 7000 1996 270 80 -10 -80 30 260 50 210 -110 320 30 50 92 7000 1997 200 10 -10 60 -30 340 120 60 -10 80 180 270 106 7000 1998 140 90 150 -130 -120 360 90 70 90 50 -10 180 80 7000 1999 31 XX -70 10 -130 10 0 430 140 30 3099999 30 30 46 7000 2000 -80 -100 -10 10 150 100 -130 -10 60 10 40 30 6 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MORZHOVAIA (HARASAVEI MYS) 030318 71 25 N 67 35 EK7042002 41 2 0 39 1954 -30 -70 -50 -190 -280 60 -20 0 -50 180 70 -80 -38 7000 1955 120 -210 -160 -160 -130 200 60 80 40 190 140 0 16 7000 1956 -90 -290 -20 -290 -100 200 -210 -190 -20 10 -70 20 -87 7000 1957 70 -290 -170 -160 -160 170 -180 -110 -10 20 0 40 -64 7000 1958 -100 -180 -290 -240 -310 -10 -90 -30 80 10 200 -30 -83 7000 1959 -90 150 240 -190 -120 150 -20 0 90 40 0 100 28 7000 1960 -70 -140 -170 -210 -270 100 -10 40 0 160 220 150 -16 7000 1961 20 130 150 -40 -120 260 -190 -160 30 60 80 100 25 7000 1962 110 30 -190 -160 -140 190 -130 -50 0 130 80 100 -3 7000 1963 110 10 -20 -130 -160 20 -80 -150 40 190 70 100 0 7000 1964 290 -40 -50 -270 -280 40 50 -80 40 130 200 60 8 7000 1965 30 -130 -90 -180 -190 60 -10 -130 0 60 -70 -100 -62 7000 1966 70 -120 -130 -260 0 40 0 80 170 50 250 -70 7 7000 1967 50 110 20 40 -100 190 30 -10 170 260 90 120 80 7000 1968 -50 20 140 -60 -120 10 110 130 30 90 50 10 30 7000 1969 -130 -150 -80 -170 -190 220 -60 0 60 190 200 -10 -10 7000 1970 -20 -70 -380 -250 -150 110 -30 -90 -20 10 90 100 -59 7000 1971 60 -350 -250 -270 -160 10 40 100 400 240 230 90 14 7000 1972 70 130 -60 -100 -190 -170 -120 0 -90 170 -230 110 -40 7000 1973 1140 0 10 -230 -130 250 70 70 40 150 210 -60 128 7000 1974 0 -260 -110 -70 -310 80 -50 -140 40 -110 -70 100 -74 7000 1975 140 80 -40 -260 -220 30 -30 -10 230 340 170 110 45 7000 1976 -50 120 -140 -140 -270 -70 30 210 40 70 110 -70 -14 7000 1977 -190 -220 -90 -200 -80 0 -30 -70 330 -20 90 270 -17 7000 1978 80 -170 -160 -210 -190 200 -190 -160 30 160 290 -20 -28 7000 1979 -120 -170 -320 -370 -230 40 -20 -30 40 50 0 -90 -101 7000 1980 -80 -40 -300 -270 -220 210 10 70 220 310 -20 40 -6 7000 1981 190 130 30 160 50 170 -130 -150 -30 -100 200 270 65 7000 1982 170 270 -60 0 -110 210 280 440 440 150 210 330 193 7000 1983 340 180 30 -100 -10 210 200 330 190 220 430 270 191 7000 1984 100 270 30 0 -60 200 70 110 50 30 30 210 86 7000 1985 30 -120 -70 -270 -210 110 0 80 170 380 250 120 40 7000 1986 -50 90 170 -180 -220 70 -60 -140 60 90 160 160 12 7000 1987 0 -110 -80 -150 -250 20 -110 -210 -60 210 190 290 -21 7000 1988 120 -250 -190 -200 -200 -30 -130 -90 110 140 80 370 -21 7000 1989 270 220 40 -50 140 390 130 10 170 90 130 220 146 7000 1990 -180 -60 0 -120 -20 140 -90 0 -30 220 -10 10 -11 7000 1991 3031 - -80 -200 -340 -390 -250 20 -60 -1209999999999 -20 -23099999 7000 1992 30 XX -200 -30 -60 -340 0 100 110 -70 -140 -8099999 -70 -71 7000 1993 31 3130 - -190 -22099999 -520 -610 40 -70 -100 609999999999 29099999 7000 1994 303131 313031 - -210 0 10 -210 440999999999999999 8099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Unreasonable data value of 1140 deleted for January 1973. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ZHELANIA II (ZHELANIA MYS) 030321 76 57 N 68 33 EK7042002 46 0 0 39 1951 140 50 10 0 -20 100 80 -20 90 240 40 160 73 7000 1952 -30 -70 -70 -30 80 70 150 70 110 140 0 -40 32 7000 1953 -60 -20 80 0 40 60 90 140 220 180 140 330 101 7000 1954 70 10 -20 -50 -180 20 120 100 120 170 130 30 43 7000 1955 160 -140 -180 -50 -110 20 110 170 80 180 100 20 31 7000 1956 -150 -170 10 -250 -90 -30 -80 -70 110 100 20 100 -41 7000 1957 200 -100 -80 -100 -140 -30 -60 10 -10 50 50 110 -7 7000 1958 50 -50 -80 30 -100 0 50 80 50 40 210 80 30 7000 1959 -30 270 160 -130 -30 50 50 -20 20 0 0 30 29 7000 1960 -60 -90 -110 -110 -110 60 -10 10 20 140 210 110 5 7000 1961 70 110 120 -40 -40 60 -30 -60 150 70 70 130 50 7000 1962 140 70 -60 -10 -90 40 20 60 100 210 150 150 65 7000 1963 110 30 -30 -80 -90 -60 90 -100 20 160 50 120 19 7000 1964 150 70 30 -120 30 90 160 70 140 150 50 40 72 7000 1965 40 -60 0 -40 -20 100 90 30 100 100 40 20 34 7000 1966 120 -110 -150 -260 -30 0 20 60 120 -50 10 -120 -32 7000 1967 -20 50 10 -10 -80 10 40 10 140 200 70 60 40 7000 1968 -50 -40 40 -110 -110 30 0 -10 -50 -10 -10 50 -22 7000 1969 -190 -170 -110 -160 -160 -60 -10 0 -40 20 70 40 -63 7000 1970 -40 -120 -280 -180 -80 90 -10 0 -30 0 20 80 -45 7000 1971 100 -170 -160 -180 -50 -60 -10 30 60 100 60 40 -19 7000 1972 30 50 -110 -100 -210 -180 -20 -30 -70 40 -190 140 -54 7000 1973 160 30 0 -240 -90 50 60 -30 0 -60 -10 -50 -15 7000 1974 -60 -200 -60 -70 -180 -70 -10 -20 -30 -90 -70 80 -64 7000 1975 120 80 -40 -160 -160 -70 -40 -20 40 20 -20 100 -13 7000 1976 -40 60 -110 -130 -200 -80 -50 0 -30 -100 10 -80 -63 7000 1977 -260 -210 -140 -200 -140 -120 -60 -170 -30 -80 -100 50 -121 7000 1978 0 -170 -100 -220 -160 -80 -70 -60 -20 70 280 60 -38 7000 1979 -60 -110 -300 -320 -200 -10 -60 -180 -10 40 0 110 -92 7000 1980 -90 0 -210 -130 -130 -20 -30 -70 -10 60 -70 -80 -65 7000 1981 -10 -80 -230 -110 -130 -60 -20 -20 10 -100 150 20 -49 7000 1982 -40 100 -130 20 -60 -50 120 10 60 -10 30 70 9 7000 1983 90 70 -40 -230 -200 -80 -30 70 -80 60 60 80 -19 7000 1984 -40 -70 -230 -250 -210 -150 -130 -140 -170 -150 -110 -20 -139 7000 1985 -200 -280 -170 -170 -240 -110 -120 -50 -50 10 -50 -180 -133 7000 1986 -170 -120 -30 -190 -200 -20 -110 -90 30 160 120 30 -49 7000 1987 10 -20 -90 -110 -30 0 170 50 90 240 20 40 32 7000 1988 150 -80 -80 -110 -170 10 70 40 140 160 170 380 57 7000 1989 340 240 -50 -10 90 120 90 210 180 240 190 220 155 7000 1990 90 190 230 130 180 90 120 280 200 300 -20 100 158 7000 1991 31XX 120 100 -70 -140 -130 -100 90 90 130 30 -18099999 -6 7000 1992 31 XX 99999 80 -50 -350 -110 -70 80 0 -90 60 70 300 -7 7000 1993 31 3130 - 250 60 0 -40 -110 -10 11099999 1309999999999 6099999 7000 1994 31 31 - 99999 200 160 200 60 190 -60 60 099999 330 11099999 7000 1995 303130 3031 - 130 230 20999999999999999 50 -30 -220 50999999999999999 7000 1996 31 31303130313130313031 - 99999 1309999999999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. POPOVA (BELYI OSTROV) 030325 73 20 N 70 03 EK7042002 38 0 0 39 1951 31283130313031 313031 - 99999999999999999999999999999999999 50 16099999999999999999999 7000 1952 31293130313031 3031 - 99999999999999999999999999999999999 110 250 60999999999999999 7000 1953 312831303130 - 999999999999999999999999999999 160 140 330 160 340 56099999 7000 1954 31283130313031 - 99999999999999999999999999999999999 -30 50 230 300 35099999 7000 1955 31283130313031 - 99999999999999999999999999999999999 260 150 310 140 -22099999 7000 1956 31293130313031 - 99999999999999999999999999999999999 -150 70 10 40 12099999 7000 1957 31283130313031 3031 - 99999999999999999999999999999999999 09999999999 70 20099999 7000 1958 31283130313031 3031 - 99999999999999999999999999999999999 90 50 -220999999999999999 7000 1959 31283130313031 3031 - 99999999999999999999999999999999999 200 180 40999999999999999 7000 1960 31293130313031 313031 - 99999999999999999999999999999999999 -130 -7099999999999999999999 7000 1961 31283130313031 313031 - 99999999999999999999999999999999999 -150 25099999999999999999999 7000 1962 31283130313031 3031 - 99999999999999999999999999999999999 0 30 320999999999999999 7000 1963 31283130313031 3031 - 99999999999999999999999999999999999 -230 50 280999999999999999 7000 1964 31293130313031 3031 - 99999999999999999999999999999999999 -50 50 190999999999999999 7000 1965 31283130313031 3031 - 99999999999999999999999999999999999 -90 -20 30999999999999999 7000 1966 31283130313031 3031 - 99999999999999999999999999999999999 80 170 -150999999999999999 7000 1967 312831303130 3031 - 999999999999999999999999999999 -40 10 250 -640999999999999999 7000 1968 31293130313031 3031 - 99999999999999999999999999999999999 60 -30 190999999999999999 7000 1969 31283130313031 3031 - 99999999999999999999999999999999999 20 30 210999999999999999 7000 1970 31283130313031 313031 - 99999999999999999999999999999999999 -70 1099999999999999999999 7000 1971 31283130313031 3031 - 99999999999999999999999999999999999 50 190 130999999999999999 7000 1972 31293130313031 3031 - 99999999999999999999999999999999999 -90 -100 210999999999999999 7000 1973 31283130313031 313031 - 99999999999999999999999999999999999 -20 -21099999999999999999999 7000 1974 31283130313031 313031 - 99999999999999999999999999999999999 -150 -5099999999999999999999 7000 1975 31283130313031 3031 - 99999999999999999999999999999999999 -260 10 -100999999999999999 7000 1976 31293130313031 3031 - 99999999999999999999999999999999999 -120 -70 -290999999999999999 7000 1977 312831303130 3031 - 999999999999999999999999999999 -60 -260 100 -250999999999999999 7000 1978 31283130313031 3031 - 99999999999999999999999999999999999 -60 0 50999999999999999 7000 1979 31283130313031 3031 - 99999999999999999999999999999999999 -250 -10 -40999999999999999 7000 1980 31293130313031 313031 - 99999999999999999999999999999999999 -150 -12099999999999999999999 7000 1981 31283130313031 3031 - 99999999999999999999999999999999999 -190 -290 -170999999999999999 7000 1982 31283130313031 313031 - 99999999999999999999999999999999999 -190 1099999999999999999999 7000 1983 31283130313031 313031 - 99999999999999999999999999999999999 200 5099999999999999999999 7000 1984 31293130313031 313031 - 99999999999999999999999999999999999 -180 -19099999999999999999999 7000 1985 312831303130 3031 - 999999999999999999999999999999 -420 -280 -220 -220999999999999999 7000 1986 31283130313031 3031 - 99999999999999999999999999999999999 -660 -210 0999999999999999 7000 1988 31293130313031 313031 - 99999999999999999999999999999999999 30 35099999999999999999999 7000 1989 31283130313031 30313031 - 99999999999999999999999999999999999 -1109999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. TADIBE-IAHA 030328 70 22 N 72 34 EK7042002 35 0 0 39 1955 -20 -80 -80 20 -40 310 80 150 30 160 30 120 57 7000 1956 -60 -160 70 -180 -10 390 20 -180 50 -10 -180 -230 -40 7000 1957 140 -370 -160 -100 30 -540 -10 -90 -60 -130 0 120 -94 7000 1958 -90 -180 -190 -90 -160 240 100 90 20 -140 180 100 -10 7000 1959 10 370 370 0 100 490 0 50 -130 -90 -10 180 110 7000 1960 -60 0 0 -20 -80 170 -190 70 70 130 -50 -150 -10 7000 1961 -140 0 -40 -190 -100 520 120 -60 270 160 -20 70 49 7000 1962 110 60 -80 10 0 490 -60 30 -160 10 -60 40 32 7000 1963 -40 60 40 -70 0 440 80 -210 160 40 -100 100 41 7000 1964 120 -60 130 -10 60 430 140 -80 -140 40 -20 -70 45 7000 1965 30 -170 -190 -190 -150 380 150 -110 -70 -10 -100 -210 -53 7000 1966 -50 -230 -230 -380 -80 270 120 -10 100 40 150 40 -21 7000 1967 260 230 170 130 270 630 110 60 170 230 -30 10 186 7000 1968 -50 -10 160 -130 -30 390 310 50 70 190 70 110 95 7000 1969 -130 -190 10 -30 -110 390 260 70 20 130 120 50 50 7000 1970 -140 -280 -350 -140 -70 490 340 70 -50 -50 250 170 21 7000 1971 130 -320 -120 -120 -10 380 190 30 220 200 10 50 56 7000 1972 80 130 40 -150 -200 220 150 250 170 180 -130 330 90 7000 1973 400 220 110 -60 60 540 140 80 230 -60 -100 -100 121 7000 1974 -40 -200 80 -10 -10 410 250 -10 -150 -110 -190 -60 -2 7000 1975 90 30 70 -200 -50 320 170 130 80 170 180 -70 77 7000 1976 60 30 -30 -90 -120 310 60 60 80 -70 20 -100 17 7000 1977 -80 -70 -110 -130 100 320 -50 -120 -20 -60 -100 80 -20 7000 1978 50 -100 -20 -110 -60 410 220 110 -100 -130 -50 -20 17 7000 1979 -50 -130 -200 -250 -100 480 280 0 20 20 -40 90 11 7000 1980 -90 -90 -240 -150 -70 -570 210 -40 80 100 -80 -40 -81 7000 1981 20 60 -130 -30 -110 270 0 -200 -120 -220 -90 -20 -49 7000 1982 -40 100 -150 -20 -30 340 -10 -90 180 50 -130 -80 8 7000 1983 30 -80 -140 -260 -90 310 130 120 0 -80 10 -90 -11 7000 1984 -150 60 -110 -160 -120 50 -70 -150 -180 -290 -40 220 -79 7000 1985 -130 -340 -320 -440 -430 -100 -30 60 -230 70 -80 -400 -196 7000 1986 -510 -420 -440 -650 -530 50 30 -40 -80 -130 -340 120 -243 7000 1987 -40 -100 -90 -120 -90 280 240 -80 -70 240 30 -50 13 7000 1988 -40 -290 -250 -240 -290 100 -170 -230 50 180 90 160 -77 7000 1989 170 140 -60 -110 -30 290 0 60 110 100 -70 50 53 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SE-LAHA 030331 70 09 N 72 34 EK7042002 24 0 0 39 1967 90 140 80 30 170 410 60 -40 180 150 -60 -90 92 7000 1968 -130 -110 100 -70 -80 290 160 40 -20 90 -20 30 24 7000 1969 -230 -190 -10 -30 -80 340 240 20 70 80 60 80 30 7000 1970 30 -110 -170 -130 -90 380 220 70 10 100 130 -20 36 7000 1971 -20 -450 -210 -210 -90 330 180 70 260 200 130 30 21 7000 1972 90 210 -80 -70 -130 140 50 90 -30 70 -330 190 17 7000 1973 290 140 50 -130 -30 510 10 -160 -60 -40 -110 -90 31 7000 1974 -50 -240 20 -50 -70 240 300 -150 -100 -50 -210 -100 -37 7000 1975 50 110 50 -210 -80 370 40 30 60 160 -130 -130 26 7000 1976 -110 50 -90 -130 -180 270 20 20 50 -60 -70 -170 -34 7000 1977 -220 -100 -190 -160 50 310 -50 -70 0 40 -40 70 -30 7000 1978 40 -120 -60 -100 -50 370 160 -70 -90 -70 130 150 25 7000 1979 320 -80 -130 -140 210 720 210 40 -30 80 -70 -200 78 7000 1980 -160 -60 -190 -120 -60 370 390 30 50 30 -90 -80 9 7000 1981 -60 50 -70 60 -90 290 60 -170 -70 -270 -130 -130 -46 7000 1982 -150 -90 -370 -160 -120 310 0 -80 90 80 -120 -10 -52 7000 1983 90 -40 -70 -220 -90 150 200 170 -80 -220 -30 -120 -21 7000 1984 -190 -10 -210 -250 -170 120 -60 -100 -110 -150 -130 -50 -110 7000 1985 -40 -150 -50 -180 -140 100 -190 90 -130 130 -30 -300 -74 7000 1986 -90 20 100 -110 -80 410 230 130 -10 -30 -150 -40 32 7000 1987 -280 -310 -300 -360 -270 170 310 10 -30 330 80 20 -51 7000 1988 110 -160 -100 -90 -100 120 50 -40 60 160 50 70 12 7000 1989 130 210 -90 -120 -70 550 50 80 0 90 -30 70 71 7000 1992 312931 303131 313031 - 999999999999999 -230 10999999999999999 6099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ANTIPAIUTA 030335 69 05 N 76 51 EK7042002 24 0 0 39 1965 -60 -110 -110 -180 -70 720 180 0 110 -70 -90 -60 21 7000 1966 -130 -180 -180 -250 -150 650 110 110 60 -130 -160 -130 -32 7000 1967 -120 -170 -170 -240 -140 660 120 80 130 140 -150 -120 2 7000 1968 220 160 170 100 210 1020 460 100 20 210 190 230 257 7000 1969 70 20 20 -50 60 860 310 50 40 60 40 70 129 7000 1970 230 170 180 110 220 1040 470 110 -40 210 200 240 262 7000 1971 60 -420 -190 -180 60 690 120 -80 150 90 -40 -40 20 7000 1972 30 210 -150 -180 -140 590 130 160 -210 170 -340 80 29 7000 1973 210 20 0 -130 -100 840 130 50 30 -60 -170 -170 53 7000 1974 -110 -330 -70 -130 -100 550 340 -180 -170 -60 -280 -180 -58 7000 1975 140 40 10 -250 -110 750 180 -40 10 -50 200 -170 58 7000 1976 -130 -30 -100 -200 -170 770 100 60 60 -130 -130 -220 -11 7000 1977 -310 -350 -40 -100 170 920 -100 -220 -130 -240 -280 -140 -68 7000 1978 -160 -340 -230 -290 -250 610 230 50 -320 -410 -20 -100 -102 7000 1979 -220 -390 -460 -580 -320 740 200 -140 -260 -270 -180 -80 -162 7000 1980 -290 -310 -400 -320 -190 580 120 -140 -80 -30 -210 -220 -124 7000 1981 -190 -10 -160 -50 -140 720 130 -260 -190 -420 -280 -160 -86 7000 1982 -110 50 -170 -70 10 780 20 -120 200 20 -150 -90 29 7000 1983 -40 -170 -170 -330 -140 630 190 70 -170 -360 -60 -60 -51 7000 1984 -190 30 -140 -180 -120 580 30 -160 -230 -380 -90 140 -61 7000 1985 -120 -240 -130 -250 -210 520 20 120 -280 10 -40 -200 -66 7000 1986 -130 -90 30 -180 -50 650 50 -50 -110 -200 -20 40 -5 7000 1987 -160 -240 -210 -240 -100 700 400 -130 -120 330 -40 -30 15 7000 1988 0 -230 -200 -120 -10 790 230 40 0 -10 -30 0 38 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. VISE (VISE OSTROV) 030338 79 30 N 76 59 EK7042002 48 0 0 39 1953 -120 -40 -20 -130 -80 0 10 50 130 110 70 250 20 7000 1954 50 -20 -20 -80 -210 -20 80 20 30 80 200 20 11 7000 1955 50 -240 -280 -130 -140 -20 80 150 0 110 20 -20 -33 7000 1956 -150 -90 20 -250 -80 -20 -60 -70 10 0 -70 20 -61 7000 1957 140 -150 -140 -70 -60 0 50 60 -40 30 30 70 -5 7000 1958 10 -70 -180 -70 -140 10 60 120 60 40 160 40 4 7000 1959 -40 240 140 -160 -100 0 10 -60 0 0 -20 0 -1 7000 1960 -100 -110 -160 -170 -190 -20 -20 -10 -30 100 160 100 -37 7000 1961 50 60 10 -120 -40 40 30 20 120 50 50 100 31 7000 1962 -10 -90 -100 -20 -120 40 30 110 -10 160 110 60 14 7000 1963 60 160 50 -30 -50 -10 170 30 140 120 120 150 75 7000 1964 190 140 150 -140 0 80 130 10 40 150 80 -20 68 7000 1965 -60 -170 -100 -40 -40 30 50 0 20 100 30 30 -11 7000 1966 50 -100 -180 -220 -40 -10 0 40 90 -120 -120 -150 -63 7000 1967 -30 30 -30 10 -140 -110 -50 -10 110 200 80 90 12 7000 1968 20 10 130 -10 -220 -50 100 20 -20 -40 40 -10 -2 7000 1969 -170 -220 -130 -100 -110 70 100 0 20 10 30 60 -36 7000 1970 -90 -180 -310 -180 -80 130 10 20 -50 0 10 120 -49 7000 1971 210 -150 -110 -150 -50 -40 40 70 -50 -80 70 60 -14 7000 1972 80 40 -120 -100 -190 -130 70 20 -60 20 -150 220 -24 7000 1973 250 60 -20 -250 -60 80 80 30 60 -10 -30 60 21 7000 1974 70 -70 40 -40 -120 0 80 40 -20 -70 -70 70 -7 7000 1975 110 50 -40 -200 -140 -40 140 70 130 110 30 150 31 7000 1976 30 50 -100 -120 -190 -40 160 170 70 -10 80 -60 3 7000 1977 -250 -200 -120 -120 -80 -60 10 -50 130 50 70 120 -41 7000 1978 50 -80 -70 -150 -80 -10 10 10 20 70 210 -50 -5 7000 1979 -140 -110 -270 -260 -160 -20 40 -20 60 70 -10 140 -56 7000 1980 -90 0 -220 -140 -150 -20 0 10 40 20 -50 0 -50 7000 1981 100 10 -120 -50 -30 -40 100 10 0 -100 150 80 9 7000 1982 30 140 -110 -10 -120 -60 110 110 170 20 40 100 34 7000 1983 100 -70 -150 -190 -110 40 130 190 20 50 50 120 16 7000 1984 0 10 -110 -150 -60 -30 20 30 20 0 30 100 -12 7000 1985 -80 -150 -50 -170 -200 -60 -40 20 30 10 30 -100 -63 7000 1986 -90 -40 50 -110 -120 70 -110 0 100 130 140 120 12 7000 1987 90 20 -50 -90 -30 -10 160 30 70 220 60 20 41 7000 1988 140 -110 -110 -130 -190 -10 40 10 120 130 150 360 34 7000 1989 320 220 -80 -20 70 100 60 190 170 210 170 210 135 7000 1990 80 160 210 110 160 70 100 260 170 290 -40 90 139 7000 1991 110 70 -90 -160 -140 -60 10 -20 70 -20 -220 -50 -42 7000 1992 150 50 -90 -400 -150 -130 40 -40 -120 10 40 280 -29 7000 1993 3130 - 220 40 -30 -70 -150 -80 10 -70 109999999999 -1099999 7000 1994 31 313031 - 99999 190 140 190 50 180 -80 50 -1099999999999999999999 7000 1995 303130 3130313031 - 130 200 0999999999999999 40999999999999999999999999999999 7000 1996 31 3130 30 313031 31 - 99999 1209999999999 7099999 170999999999999999 609999999999 7000 1997 3128313031303131 - 9999999999999999999999999999999999999999 110 130 100 2099999 7000 1998 28 31 3131 30 - -6099999 -60 -13099999 -1109999999999 60 -5099999 35099999 7000 1999 31 XX 170 80 -310 -15099999 40 40 20 50 0 210 210 32 7000 2000 31 31 3130 - 99999 -40 -120 -40 10 9099999 60 309999999999 -13099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. LESKINA (LESKINA MYS) 030340 72 19 N 79 34 EK7042002 38 0 0 39 1951 312831303130 313031 - 999999999999999999999999999999 80 220 20099999999999999999999 7000 1952 312931303130 313031 - 999999999999999999999999999999 240 100 9099999999999999999999 7000 1953 312831303130 3031 - 999999999999999999999999999999 50 90 190 0999999999999999 7000 1954 312831303130 3031 - 999999999999999999999999999999 140 50 40 120999999999999999 7000 1955 312831303130 313031 - 999999999999999999999999999999 120 200 2099999999999999999999 7000 1956 312931303130 313031 - 999999999999999999999999999999 -30 -190 -5099999999999999999999 7000 1957 312831303130 313031 - 999999999999999999999999999999 40 60 20099999999999999999999 7000 1958 312831303130 313031 - 999999999999999999999999999999 0 210 2099999999999999999999 7000 1959 312831303130 3031 - 999999999999999999999999999999 130 150 -60 -40999999999999999 7000 1960 312931303130 3031 - 999999999999999999999999999999 110 90 -30 50999999999999999 7000 1961 312831303130 3031 - 999999999999999999999999999999 50 -100 200 210999999999999999 7000 1962 312831303130 3031 - 999999999999999999999999999999 -70 -40 -50 10999999999999999 7000 1963 312831303130 3031 - 999999999999999999999999999999 180 -170 140 140999999999999999 7000 1964 312931303130 3031 - 999999999999999999999999999999 140 10 -30 100999999999999999 7000 1965 312831303130 3031 - 999999999999999999999999999999 0 -70 -120 -30999999999999999 7000 1966 312831303130 3031 - 999999999999999999999999999999 0 40 90 -50999999999999999 7000 1967 312831303130 3031 - 999999999999999999999999999999 10 120 240 280999999999999999 7000 1968 312931303130 3031 - 999999999999999999999999999999 60 -60 -100 -140999999999999999 7000 1969 312831303130 3031 - 999999999999999999999999999999 -60 -70 -180 -140999999999999999 7000 1970 312831303130 3031 - 999999999999999999999999999999 0 0 -150 -60999999999999999 7000 1971 312831303130 3031 - 999999999999999999999999999999 70 -10 180 -50999999999999999 7000 1972 312931303130 3031 - 999999999999999999999999999999 90 160 50 320999999999999999 7000 1973 312831303130 3031 - 999999999999999999999999999999 150 130 80 -30999999999999999 7000 1974 312831303130 3031 - 999999999999999999999999999999 30 -220 -290 350999999999999999 7000 1975 312831303130 3031 - 999999999999999999999999999999 60 -100 80 120999999999999999 7000 1976 312931303130 313031 - 999999999999999999999999999999 20 50 1099999999999999999999 7000 1977 312831303130 313031 - 999999999999999999999999999999 0 -290 -16099999999999999999999 7000 1978 312831303130 313031 - 999999999999999999999999999999 -140 -130 -21099999999999999999999 7000 1979 312831303130 313031 - 999999999999999999999999999999 -50 -190 -25099999999999999999999 7000 1980 312931303130 313031 - 999999999999999999999999999999 40 -130 2099999999999999999999 7000 1981 312831303130 313031 - 999999999999999999999999999999 -70 -200 -25099999999999999999999 7000 1982 312831303130 313031 - 999999999999999999999999999999 -70 -200 7099999999999999999999 7000 1983 312831303130 313031 - 999999999999999999999999999999 0 50 -19099999999999999999999 7000 1984 312931303130 313031 - 999999999999999999999999999999 -120 -230 -22099999999999999999999 7000 1986 312831303130 313031 - 999999999999999999999999999999 -180 -240 -9099999999999999999999 7000 1987 31283130313031 313031 - 99999999999999999999999999999999999 -160 -17099999999999999999999 7000 1988 312931303130 313031 - 999999999999999999999999999999 30 -140 1099999999999999999999 7000 1989 31283130313031 313031 - 99999999999999999999999999999999999 50 13099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. DIKSON 030345 73 30 N 80 24 EK7042002312 48 0 0 39 1950 40 -10 -80 -120 20 190 -10 -90 -70 230 190 100 33 7000 1951 30 -60 -130 -170 -180 240 90 80 120 380 60 150 52 7000 1952 -170 -210 -210 -170 -30 40 200 100 90 0 -90 -110 -46 7000 1953 -160 -90 80 -120 -60 110 0 30 130 20 200 440 49 7000 1954 -30 -30 -10 -80 -300 0 60 -110 -20 80 140 0 -25 7000 1955 90 -410 -510 -290 -410 60 100 160 -50 90 -80 -60 -107 7000 1956 -200 -260 0 -260 -80 140 -150 -260 -60 -90 -120 -100 -120 7000 1957 60 -220 -90 -40 -120 40 -40 -10 -40 -110 -170 -100 -69 7000 1958 -170 -290 -240 -120 -170 120 40 160 -10 -30 90 -80 -57 7000 1959 -170 290 290 -80 -90 180 110 60 -110 -120 40 60 37 7000 1960 -260 -200 -150 -150 -200 150 -50 -140 -190 50 70 140 -77 7000 1961 -60 10 40 -160 -170 150 20 -180 140 130 60 70 4 7000 1962 50 10 -160 -10 -140 60 0 -20 -30 70 60 -10 -10 7000 1963 -40 10 -60 -100 -120 0 180 -250 0 250 70 140 7 7000 1964 130 50 80 -120 40 190 100 -50 -30 40 -60 -50 27 7000 1965 10 -270 -70 -110 -120 190 50 -160 -170 -60 -200 -190 -90 7000 1966 -10 -250 -230 -320 80 320 220 160 190 -140 40 0 7 7000 1967 50 100 20 60 30 180 70 100 290 380 340 130 145 7000 1968 -30 -70 40 -70 -80 190 130 20 -60 80 -120 70 9 7000 1969 -110 -180 -30 -30 -110 100 70 60 -80 140 120 250 18 7000 1970 -110 -310 -400 -230 -60 240 100 -20 -80 0 70 140 -54 7000 1971 70 -290 -130 -210 -80 10 100 50 180 30 30 110 -9 7000 1972 90 120 -180 -30 -190 -50 170 150 70 210 -410 100 5 7000 1973 150 80 70 -270 -40 290 110 40 -100 -70 -80 -160 1 7000 1974 -60 -300 40 -20 -120 90 170 -20 30 -50 -190 100 -25 7000 1975 100 20 10 -240 -290 100 60 -100 240 190 80 220 32 7000 1976 -120 80 -30 -70 -200 120 140 190 110 -120 100 -80 9 7000 1977 -280 -280 -210 -140 -30 100 70 -260 -20 -260 -130 50 -115 7000 1978 -20 -160 -60 -140 -110 70 -70 -190 -100 40 320 -80 -42 7000 1979 -260 -170 -280 -290 -140 150 50 -240 -100 -110 -70 150 -109 7000 1980 -190 -30 -280 -100 -140 150 30 -100 30 310 -90 -130 -46 7000 1981 120 60 -150 40 10 130 60 -60 -140 -150 220 70 17 7000 1982 -60 100 -160 -10 -120 -30 110 10 190 -90 -10 40 -4 7000 1983 30 -60 -200 -280 -100 120 140 230 30 0 190 10 10 7000 1984 -10 100 0 -50 -10 120 -90 -80 -40 -130 0 210 1 7000 1985 -100 -170 -20 -170 -250 20 -80 -130 -20 230 110 -200 -65 7000 1986 -180 60 120 -90 -120 170 -80 -320 -180 100 200 50 -24 7000 1987 -80 -110 -50 -130 -40 0 140 -50 -70 380 260 20 24 7000 1988 50 -330 -220 -180 -290 0 20 -70 20 200 200 370 -18 7000 1989 240 290 40 -10 150 390 280 210 300 190 -10 70 178 7000 1990 -160 -70 -10 -10 70 40 -130 -10 -330 -70 -260 -160 -91 7000 1991 31 XX -270 -280 -450 -210 -230 4099999 70 150 200 50 190 -66 7000 1992 280 160 130 -160 170 290 210 -150 -200 -60 -20 250 76 7000 1993 350 220 150 120 50 180 120 -120 -60 30 220 80 111 7000 1994 313031 - -30 -50 -20 -90 60 230 130999999999999999 470 34099999 7000 1995 31 3131 - 340 170 120 12099999 2809999999999 330 220 220 34099999 7000 1996 380 220 230 30 160 200 270 200 -80 310 360 -140 179 7000 1997 31303130313130313031 - 150 -409999999999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. UEDINENIA (UEDINENIA OSTROV) 030348 77 30 N 82 12 EK7042002 43 0 0 39 1953 -130 50 120 -70 -70 -60 -20 -10 70 70 150 320 35 7000 1954 70 -40 0 -100 -270 -70 40 -70 -80 -10 190 -60 -33 7000 1955 70 -300 -330 -170 -180 30 100 190 -30 90 0 -100 -51 7000 1956 -190 -210 -20 -370 -170 -50 -40 -120 -100 -70 -110 -130 -131 7000 1957 210 -90 -120 -50 -60 -40 30 30 -100 0 0 -20 -17 7000 1958 -10 -110 -220 -70 -210 -40 10 120 -30 0 110 -80 -44 7000 1959 -190 280 180 -150 -60 40 -10 -90 -90 -100 20 220 2 7000 1960 90 -50 -60 -120 -150 30 10 -60 -80 10 10 80 -24 7000 1961 40 90 50 -60 -10 70 20 -10 120 40 60 90 41 7000 1962 140 0 -170 -50 -130 -50 -10 -20 -60 40 50 60 -17 7000 1963 120 250 150 -40 -40 -20 150 -40 150 10 -60 220 70 7000 1964 280 180 140 -90 60 130 150 0 -30 60 -30 -50 67 7000 1965 80 -120 0 -60 -70 50 20 0 30 110 10 -90 -2 7000 1966 0 -190 -210 -290 10 10 50 40 30 -30 60 -30 -45 7000 1967 0 20 -20 0 -90 -10 0 -10 90 270 20 10 23 7000 1968 -80 -50 60 -50 -100 30 80 80 -50 10 10 170 10 7000 1969 -60 -120 -30 -60 -120 60 90 40 60 120 120 90 17 7000 1970 -50 -180 -260 -160 -80 100 -20 0 -40 30 40 170 -37 7000 1971 210 -30 -50 -130 0 0 50 40 100 60 150 120 44 7000 1972 120 150 -70 -50 -150 -10 50 0 0 0 -120 260 15 7000 1973 250 60 40 -50 50 200 120 -30 -60 90 90 120 74 7000 1974 150 20 70 -30 -120 -40 50 10 -40 -10 -50 70 7 7000 1975 210 200 80 -90 -60 30 80 60 210 160 90 120 90 7000 1976 0 120 -120 -90 -60 60 50 80 10 -30 -160 100 -4 7000 1977 -50 -90 -50 -90 -80 -50 0 -90 40 30 100 200 -10 7000 1978 60 -110 -90 -200 -160 -40 50 -30 -20 20 280 170 -5 7000 1979 -30 -90 -240 -270 -150 40 0 -30 110 160 110 110 -23 7000 1980 -90 -10 -250 -170 -170 -40 -30 0 60 110 60 10 -44 7000 1981 10 -30 -240 -40 -40 -20 60 -70 -40 -120 150 100 -24 7000 1982 60 150 -80 40 -70 0 100 0 120 -20 20 80 32 7000 1983 110 0 -80 -190 -100 40 100 100 -30 70 200 120 29 7000 1984 0 20 -150 -210 -180 -200 -80 0 10 -10 30 120 -54 7000 1985 -90 -100 20 -150 -140 30 40 20 30 60 -10 -130 -35 7000 1986 -20 200 130 -100 -40 30 -10 -60 70 200 210 200 67 7000 1987 150 110 90 20 60 -290 -20 0 0 50 20 90 24 7000 1988 160 -80 -50 -50 -120 110 120 10 150 140 140 290 69 7000 1989 260 220 -10 -140 -40 30 60 50 110 110 140 250 86 7000 1990 70 220 310 220 250 90 150 80 -40 160 90 70 139 7000 1991 -110 -170 -340 -200 -260 -210 60 60 20 80 0 180 -73 7000 1992 240 90 20 -290 30 60 80 20 0 170 130 350 76 7000 1993 3130 - 230 60 -90 -170 -240 -200 -70 -60 309999999999 -3099999 7000 1994 303130 - -120 -30 -190 -300 -170 -100 0 160999999999999999 -12099999 7000 1995 303130313130313031 - -140 -180 -28099999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SOPOCHNAIA KARGA 030351 71 52 N 82 42 EK7042002 41 0 0 39 1958 -140 -310 -370 -260 -300 480 20 110 -20 -100 10 -110 -82 7000 1959 -230 220 270 -150 -170 1160 60 -30 -320 -120 -30 130 63 7000 1960 -240 -170 -210 -230 -270 690 -10 -30 -270 -30 70 100 -51 7000 1961 -50 0 50 -80 20 940 120 -310 60 50 20 90 75 7000 1962 90 40 -110 0 -30 690 -50 -130 -160 -40 -60 -180 3 7000 1963 -240 -130 -60 -210 -80 690 130 -390 -220 70 0 100 -29 7000 1964 90 -50 0 -220 -40 550 100 -130 -250 -40 -90 -70 -12 7000 1965 50 -150 -170 -150 -120 540 10 -160 -300 -180 -220 -220 -89 7000 1966 -70 -260 -310 -410 -20 540 100 60 20 -190 -60 20 -47 7000 1967 100 120 -30 0 130 430 50 110 210 190 250 120 139 7000 1968 30 0 160 -70 -20 530 130 -60 -160 20 -100 -20 37 7000 1969 -200 -310 -140 -130 -180 590 30 -20 -150 -70 -90 240 -35 7000 1970 -120 -330 -430 -220 -90 550 100 10 -120 -30 -40 110 -50 7000 1971 60 -330 -110 -150 10 540 110 -60 170 30 10 70 31 7000 1972 40 100 -210 -70 -150 470 160 110 0 150 -410 60 21 7000 1973 140 -10 -40 -290 -80 710 30 -30 -50 -60 -100 -170 4 7000 1974 -130 -300 10 -70 -60 570 310 -50 -80 -70 -190 -20 -5 7000 1975 -10 -50 -10 -240 -90 630 80 -100 190 170 20 180 64 7000 1976 -60 30 -110 -110 -200 460 300 120 20 -300 -270 -180 -26 7000 1977 -300 -290 -200 -170 -20 660 100 -320 -100 -250 -230 0 -93 7000 1978 -30 -240 -220 -280 -140 700 -90 -70 -230 -110 10 -220 -77 7000 1979 -210 -240 -380 -390 -200 740 40 -80 -80 -50 -230 -80 -97 7000 1980 -300 -160 -360 -110 -90 570 10 -250 -90 40 0 -30 -65 7000 1981 30 40 -160 0 0 500 50 -130 -200 -460 0 0 -29 7000 1982 -80 60 -200 -50 0 540 70 -80 250 -120 -330 -190 -13 7000 1983 -210 -140 -250 -130 -10 610 190 370 100 -210 10 10 28 7000 1984 -30 90 -80 -130 30 -390 20 -130 -80 -320 -50 160 -76 7000 1985 -140 -150 0 -160 -150 620 80 -150 -170 90 0 -160 -24 7000 1986 -250 0 -300 -590 -90 600 -140 -260 -110 -90 350 170 -61 7000 1987 150 160 90 -190 -90 290 200 -70 -110 380 -10 -100 58 7000 1988 90 -210 -130 -110 -150 500 160 -100 200 260 20 -40 41 7000 1989 -70 0 -270 -330 -170 400 220 110 190 130 140 250 50 7000 1990 -230 -90 40 -60 180 590 -10 250 -380 -110 -110 160 20 7000 1991 0 90 -210 -20 20 570 100 150 -90 160 100 190 88 7000 1992 340 300 230 -120 150 630 340 -160 -90 0 40 330 166 7000 1993 400 150 0 -50 -30 390 30 -300 -280 -100 330 170 58 7000 1994 -90 -50 -110 -170 80 1280 160 220 -20 260 130 80 147 7000 1995 313031 3031 - 160 40 20 90999999999999999 -40 10 -80999999999999999 7000 1996 312931 - 999999999999999 50 110 660 360 -50 -350 -150 50 -2099999 7000 1997 31 XX 160 -40 -30 7099999 200 -120 -10 180 -80 20 120 43 7000 1998 30313130 3031 - -10 40 -50 -170 -3099999999999999999999 -270999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. IZVESTIA TSIK (IZVESTIA TSIK OSTROVA) 030360 75 57 N 82 57 EK7042002 47 0 0 39 1954 150 130 120 40 -160 30 150 70 70 130 240 90 88 7000 1955 10 -230 -290 -160 -240 -50 60 130 -30 60 -80 -50 -71 7000 1956 -160 -220 20 -300 -120 -40 -20 -160 0 -20 -140 -60 -101 7000 1957 120 -90 -130 -80 -130 -60 -20 10 10 10 -130 10 -39 7000 1958 -160 -170 -220 -150 -260 -90 -50 10 30 50 150 10 -71 7000 1959 -100 370 300 -100 -100 60 120 150 -30 0 80 90 68 7000 1960 -70 -80 -40 -130 -190 -60 20 -20 30 80 -10 100 -30 7000 1961 -70 10 -40 -170 -180 -70 -10 -40 170 80 -20 100 -20 7000 1962 150 70 -160 -40 -150 -60 -20 50 40 130 90 90 15 7000 1963 40 200 80 10 -80 -150 150 -90 250 200 30 150 65 7000 1964 190 150 90 -130 30 0 40 -20 -40 200 30 30 48 7000 1965 90 -150 -10 -60 -130 70 10 -10 -30 60 -60 -70 -23 7000 1966 190 -170 -250 -300 0 -30 0 30 70 -40 120 40 -27 7000 1967 110 170 60 40 -50 10 10 -10 110 150 70 20 57 7000 1968 -60 -30 50 -100 -120 50 70 30 0 50 -30 120 3 7000 1969 -140 -200 -70 -120 -200 -60 -50 -20 30 130 180 190 -26 7000 1970 -40 -210 -340 -240 -120 70 -50 20 -40 70 100 240 -44 7000 1971 220 -60 -50 -160 -80 -90 40 70 170 150 90 80 33 7000 1972 130 150 -90 -30 -130 -170 70 90 30 190 -210 180 18 7000 1973 190 80 70 -290 -110 80 50 40 120 80 10 -60 22 7000 1974 40 -170 30 -50 -170 -60 50 -50 -60 -40 -60 -320 -71 7000 1975 280 170 110 -90 -60 40 60 80 290 430 180 160 138 7000 1976 0 170 -20 -20 -130 -20 120 150 90 -10 0 -100 18 7000 1977 -200 -260 -190 -180 -60 -10 -10 -60 140 10 0 150 -55 7000 1978 80 -110 -80 -240 -190 -50 -60 -30 -10 70 360 90 -14 7000 1979 -30 -60 -280 -330 -200 -20 -80 -90 -10 50 90 380 -48 7000 1980 60 110 -180 -120 -120 30 30 -10 80 120 30 30 4 7000 1981 240 170 -120 20 -50 -20 -10 -50 10 -30 180 80 34 7000 1982 70 170 -130 -30 -170 -130 80 90 180 -10 70 130 26 7000 1983 80 30 -90 -210 -120 -10 40 160 50 100 240 130 34 7000 1984 -100 0 -160 -230 -170 -110 -100 -50 -10 -50 -30 30 -82 7000 1985 -230 -180 -60 -250 -260 -90 0 50 100 260 140 -90 -50 7000 1986 -140 -40 100 -140 -180 20 -50 -50 30 100 140 60 -13 7000 1987 -20 -100 -80 -200 -110 -150 60 40 100 250 150 60 1 7000 1988 250 -60 -70 -110 -200 50 90 -10 140 170 140 330 61 7000 1989 300 290 -10 -160 -40 40 60 90 230 220 170 260 120 7000 1990 -20 130 190 70 120 -20 -30 80 -90 110 50 120 59 7000 1991 30 20 -190 -20 -80 -90 10 60 70 180 110 240 29 7000 1992 300 140 90 -280 60 -10 40 40 70 50 60 280 71 7000 1993 380 190 20 0 -120 -70 30 -110 -70 -70 180 0 29 7000 1994 -190 -120 -160 -280 -200 -130 -30 40 -60 150 100 50 -68 7000 1995 303130313130 30 - 50 -40 -130999999999999999999999999999999 3099999 5099999 7000 1996 31 3130 3130313031 - 99999 -409999999999 -130 -120 -10999999999999999999999999999999 7000 1997 3128313031303131 - 9999999999999999999999999999999999999999 0 80 150 13099999 7000 1998 28 31 3131 3130 - -7099999 -120 -22099999 -1509999999999 1009999999999 11099999 7000 1999 -90 -100 -370 -130 -170 40 90 70 60 -10 80 100 -36 7000 2000 31 XX 60 110 -70 -30 -10 5099999 50 140 40 -90 -60 17 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. STERLEGOVA (STERLEGOVA MYS) 030365 75 25 N 88 54 EK7042002 46 2 0 39 1950 30 -30 -110 -150 -40 90 -50 -70 -50 140 80 20 -12 7000 1951 40 -70 -200 -180 -200 40 0 40 80 340 20 70 -1 7000 1952 -200 -240 -180 -120 10 50 230 70 110 80 -60 -60 -25 7000 1953 -130 -70 50 -180 -120 90 -20 70 150 30 180 450 42 7000 1954 140 90 30 -50 -310 -100 40 -100 -50 80 150 20 -6 7000 1955 260 -240 -360 -140 -320 -90 40 160 -90 90 -50 0 -60 7000 1956 -110 -210 -30 -360 -190 -60 -190 -260 -100 -140 -200 -110 -163 7000 1957 140 -170 -90 -30 -30 50 50 110 0 -140 -140 -60 -25 7000 1958 -140 -270 -310 -180 -290 -100 -40 70 -10 -40 150 -40 -99 7000 1959 -150 330 250 -120 -130 110 150 70 -110 -120 0 110 31 7000 1960 -120 -70 -60 -80 -80 40 -20 -60 -90 -20 0 100 -38 7000 1961 -90 10 30 -210 -220 -10 -40 -180 110 190 160 150 -9 7000 1962 -10 -50 -190 -20 -170 -80 -40 -30 -30 30 60 0 -44 7000 1963 -60 20 0 -90 -120 -40 200 -50 30 140 70 210 26 7000 1964 160 150 160 -120 20 20 100 -60 -70 90 -30 -20 34 7000 1965 20 -300 -70 -100 -130 60 20 -140 -210 -110 -150 -200 -108 7000 1966 -70 -310 -380 -460 -100 -80 -30 150 240 -80 110 40 -79 7000 1967 60 140 10 20 -40 70 20 90 330 450 380 230 146 7000 1968 20 -20 50 -80 -110 50 70 30 -140 50 -120 100 -8 7000 1969 -100 -220 -130 -150 -230 -30 0 10 -100 200 200 260 -23 7000 1970 -70 -190 -290 -150 -60 120 -10 -50 -100 -80 60 230 -48 7000 1971 120 -160 -50 -140 -20 0 100 20 120 60 130 160 30 7000 1972 140 160 -110 -10 -200 -130 130 160 0 210 -340 150 14 7000 1973 360 0 -10 -350 -110 170 110 10 -50 -20 -90 -100 -6 7000 1974 0 -210 40 -110 -160 -60 40 -10 40 -190 -70 150 -44 7000 1975 220 100 80 -130 -80 90 60 -70 140 100 110 470 91 7000 1976 -10 150 0 -70 -230 -10 100 430 150 -130 110 -30 38 7000 1977 -230 -220 -170 -150 -110 -10 10 -280 -40 -220 -90 280 -102 7000 1978 0 -130 -430 -530 -380 -170 -110 -120 90 0 380 -40 -121 7000 1979 -180 -80 -260 -310 -190 10 -20 -250 -110 -100 0 190 -109 7000 1980 -100 50 -230 -180 -190 0 -40 -110 20 240 -10 -70 -52 7000 1981 f 180 90 -180 960 -70 0 90 -20 -140 -210 280 130 91 7000 1982 50 190 -80 30 -70 -10 200 -80 360 -80 -10 50 44 7000 1983 70 -10 -140 -250 -140 30 100 250 80 90 290 170 46 7000 1984 30 90 -10 -60 -70 70 120 -120 0 -80 -30 130 5 7000 1985 -90 -50 20 -180 -240 -30 -120 -170 -50 250 220 -160 -50 7000 1986 -120 40 170 -80 -170 70 -150 -290 -150 100 190 120 -23 7000 1987 50 -80 -60 -200 -110 -200 60 -10 -20 450 280 90 22 7000 1988 360 -50 -40 -40 -170 90 160 -90 90 270 230 460 107 7000 1989 330 370 110 -40 80 200 210 170 350 320 180 270 212 7000 1990 10 130 210 170 210 50 20 120 -280 -30 20 130 64 7000 1991 0 0 -170 0 -80 -20 90 200 210 180 200 430 87 7000 1992 410 240 210 -160 120 90 350 60 -120 0 10 280 125 7000 1993 270 100 -120 -100 -160 20 170 -230 -110 -30 320 -10 9 7000 1994 -200 -80 -100 -190 -100 -30 100 60 -90 310 320 300 26 7000 1995 3031303131 3031 - 220 200 09999999999999999999999999 190 10999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Suspicious spike (with value = 960) in April 1981 flagged. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ISACHENKO (ISACHENKO OSTROV) 030370 77 09 N 89 12 EK7042002 40 0 0 39 1954 140 90 20 -40 -230 -40 30 -10 10 60 220 10 21 7000 1955 20 -290 -350 -150 -230 -40 40 90 -110 10 -100 -80 -98 7000 1956 -210 -290 -60 -350 -190 -70 -150 -200 -70 -150 -230 -120 -173 7000 1957 -80 -430 -160 -70 -170 -80 -40 -40 -50 -110 -120 -60 -115 7000 1958 -210 -160 -250 -180 -350 -80 -90 10 -50 -100 -10 -80 -129 7000 1959 -200 350 120 -130 -150 90 70 -20 -70 -110 0 120 3 7000 1960 -130 -70 -60 -130 -170 70 -40 -20 -50 10 -20 50 -47 7000 1961 -80 30 0 -140 -130 10 -60 -80 80 0 0 50 -27 7000 1962 30 -40 -170 -60 -170 -70 -20 -20 0 80 10 -10 -37 7000 1963 0 90 0 -40 -50 -80 140 -30 120 90 20 240 42 7000 1964 180 110 110 -110 40 40 120 0 -30 90 30 -20 47 7000 1965 40 -150 -50 -80 -100 120 -10 -60 -20 50 -80 -100 -36 7000 1966 120 -100 -200 -280 10 -10 -30 0 110 0 30 -30 -31 7000 1967 60 100 40 0 -50 10 0 -160 20 150 30 10 17 7000 1968 0 -30 -30 -150 -110 10 20 0 -70 -40 -120 10 -42 7000 1969 -350 -370 -70 -240 -210 -10 10 -20 -30 40 190 280 -63 7000 1970 80 -50 -250 -130 0 150 30 40 -30 30 30 210 10 7000 1971 190 -50 -60 -130 30 0 60 40 100 80 40 80 33 7000 1972 90 110 -50 80 -40 0 160 120 80 90 -190 210 55 7000 1973 220 40 20 -260 -40 100 20 -10 30 -10 -110 -100 -8 7000 1974 -20 -220 -20 -50 -140 -10 50 -10 -10 -190 -100 50 -55 7000 1975 100 60 30 -160 -110 -50 30 60 250 170 240 170 66 7000 1976 -60 120 20 -20 -80 70 110 160 160 50 150 50 60 7000 1977 -70 -10 70 90 150 230 210 0 140 60 100 310 107 7000 1978 190 -120 -90 -220 -190 -40 -100 -70 -50 20 310 110 -20 7000 1979 -30 -70 -300 -310 -180 0 -60 -110 -30 10 60 250 -64 7000 1980 0 110 -130 -60 -100 70 20 -20 50 70 0 20 2 7000 1981 230 170 -90 40 20 30 20 -40 -10 -140 130 150 41 7000 1982 120 230 -50 20 -50 10 150 50 190 0 40 130 69 7000 1983 160 50 -50 -160 -90 50 60 90 -20 120 240 190 54 7000 1984 70 100 -60 -160 -90 -40 -60 0 10 -60 -20 130 -15 7000 1985 -110 -140 -20 -180 -210 -30 -30 0 40 180 20 -60 -44 7000 1986 40 180 180 -90 -120 70 -20 -40 40 100 140 60 44 7000 1987 20 -40 -40 -140 -70 -80 100 -30 20 160 50 -20 -5 7000 1988 160 -90 -80 -90 -180 120 40 -10 70 100 130 320 41 7000 1989 290 270 20 -130 -10 120 150 90 130 170 140 280 126 7000 1990 31283130313031 - 99999999999999999999999999999999999 80 -30 30 10 6099999 7000 1991 -20 -20 -160 -10 -10 -20 0 110 100 80 10 140 17 7000 1992 180 140 0 -230 60 50 180 90 210 120 -30 230 84 7000 1993 30 31 - 390 300 240 270 20 0 10 -8099999 0 1809999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. GOLOMIANYI (GOLOMIANYI OSTROV) 030374 79 33 N 90 37 EK7042002 47 0 0 39 1954 60 0 -10 -90 -270 -70 20 0 10 40 220 -10 -9 7000 1955 50 -250 -310 -150 -170 -30 30 100 -30 70 -90 -50 -68 7000 1956 -190 -170 -10 -260 -110 -30 -20 -90 0 0 -70 -10 -79 7000 1957 120 -110 -140 -80 -80 -60 0 -30 -130 -70 -70 0 -53 7000 1958 150 -80 -220 -110 -150 0 50 0 10 -10 40 -50 -31 7000 1959 -80 250 230 -60 -130 -30 30 -20 50 70 40 50 32 7000 1960 -90 50 0 0 -90 110 -10 20 30 170 90 90 30 7000 1961 -20 60 20 -70 -20 0 -60 -10 110 70 80 100 21 7000 1962 180 150 0 140 70 20 0 -20 -80 0 10 0 38 7000 1963 50 170 40 -20 30 50 190 -60 60 100 10 200 68 7000 1964 210 160 40 -150 30 90 150 10 50 180 60 20 71 7000 1965 40 -100 0 -50 -40 60 10 20 50 130 60 50 20 7000 1966 180 30 -60 -190 100 100 80 20 80 10 0 -50 25 7000 1967 70 100 0 50 0 30 20 0 110 130 20 20 45 7000 1968 0 0 20 -100 -50 70 140 -50 -110 -30 -180 -130 -35 7000 1969 -210 -200 -70 -160 -290 -90 -80 -50 -60 -40 20 90 -94 7000 1970 -20 -90 -210 -80 0 160 20 30 -30 80 100 140 9 7000 1971 70 -180 -90 -120 0 0 20 0 60 30 -60 -30 -24 7000 1972 80 20 -10 160 0 -60 40 0 -70 40 -180 100 10 7000 1973 90 -30 -20 -260 -70 40 50 0 40 0 -60 -50 -22 7000 1974 -40 -180 -10 0 -50 -30 40 20 -10 -90 -110 10 -36 7000 1975 100 60 10 -140 -120 -20 50 -60 50 90 30 110 13 7000 1976 -50 80 -70 -110 -190 -70 0 40 0 -40 0 -80 -41 7000 1977 -240 -150 -50 -80 -40 -10 40 -90 10 -80 -20 130 -48 7000 1978 -10 -90 -160 -260 -210 -110 -160 -90 -90 -10 130 -20 -90 7000 1979 -340 -40 -330 -250 -180 -50 -40 -90 0 90 0 140 -91 7000 1980 -120 -40 -210 -80 -80 80 30 30 80 40 -30 -50 -30 7000 1981 60 80 -80 30 10 10 80 30 -10 -100 170 230 42 7000 1982 130 190 -30 20 -40 50 210 130 170 -20 30 120 79 7000 1983 140 140 70 -140 0 140 140 70 -10 80 270 320 102 7000 1984 270 230 20 -150 -40 -190 -70 -10 0 -20 30 120 16 7000 1985 -30 40 -70 -160 -190 -10 -20 0 -20 -40 -10 -20 -45 7000 1986 -30 0 -30 -80 -60 10 -100 -40 -120 -190 -40 20 -55 7000 1987 80 20 -70 -80 -30 0 120 30 30 120 20 0 20 7000 1988 120 -120 -110 -80 -180 30 60 -50 40 70 60 230 6 7000 1989 220 260 30 -90 0 100 130 70 100 40 10 150 84 7000 1990 -20 90 210 100 170 10 130 100 -60 60 10 50 71 7000 1991 20 20 -120 50 10 20 120 170 160 230 100 250 86 7000 1992 270 210 40 -240 20 20 110 0 -60 20 -10 200 49 7000 1993 3130313031 - 260 150 40 20 -40 60 0999999999999999999999999999999 7000 1994 31 31 - 99999 20 -30 -160 -30 30 60 100 099999 110 4099999 7000 1995 303130 313031 - 50 40 -30999999999999999 -30 40 2099999999999999999999 7000 1996 31 3130 30 313031 31 - 99999 109999999999 -3099999 20999999999999999 -109999999999 7000 1997 31283130313031313031 - 99999999999999999999999999999999999999999999999999 70 4099999 7000 1998 28 31 3131 30 - -2099999 -120 -10099999 -409999999999 -160 -12099999 12099999 7000 1999 31 XX 0 -20 -250 -5099999 70 80 30 50 80 70 120 16 7000 2000 31 XX 0 50 -60 0 30 10099999 10 110 -50 -90 -70 2 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. PRAVDY (PRAVDY OSTROV) 030378 76 16 N 94 46 EK7042002 45 0 0 39 1950 -30 -100 -100 -150 -40 0 -120 -100 -80 110 50 20 -45 7000 1951 -70 -230 -280 -270 -240 -10 110 140 120 350 -10 -70 -37 7000 1952 -320 -350 -250 -190 -50 0 200 60 100 50 -110 -110 -80 7000 1953 -170 -70 70 -100 -40 100 0 90 160 30 90 360 44 7000 1954 120 90 80 0 -170 0 60 -50 20 160 330 30 55 7000 1955 20 -380 -400 -90 -250 -50 -40 150 0 190 -50 40 -69 7000 1956 -70 -150 40 -260 -80 80 -110 -140 -60 -100 -170 -30 -87 7000 1957 170 -160 -140 -80 -90 -20 -20 10 -100 -190 -190 -100 -75 7000 1958 -150 -240 -280 -180 -260 -60 -70 -70 80 50 110 -70 -95 7000 1959 -140 220 130 -120 -150 130 60 -40 -160 -80 40 120 -1 7000 1960 -120 -80 -90 -80 -120 80 -20 -120 -140 -20 0 130 -48 7000 1961 -50 40 10 -170 -140 10 -80 -180 110 190 130 150 1 7000 1962 140 40 -150 -30 -140 -30 0 0 -20 -10 80 140 1 7000 1963 30 200 100 -30 -50 -170 80 -130 10 190 110 350 57 7000 1964 240 130 150 -90 70 90 120 -60 -180 100 -50 -30 41 7000 1965 20 -280 -80 -70 -120 80 -30 -240 -220 -180 -180 -180 -122 7000 1966 10 -200 -250 -280 0 -20 -60 0 270 0 70 60 -32 7000 1967 140 130 0 30 -40 30 -40 0 300 410 340 210 125 7000 1968 60 -60 10 -100 -100 30 20 50 -10 110 -90 40 -3 7000 1969 -180 -230 -120 -100 -200 -40 -20 -10 -40 170 10 160 -49 7000 1970 30 -140 -270 -140 -40 110 10 0 -60 -70 0 160 -33 7000 1971 70 -220 -70 -150 -20 -10 50 20 210 160 120 140 27 7000 1972 100 70 -160 0 -200 -120 60 150 20 330 -270 80 6 7000 1973 130 0 20 -280 -70 50 30 -40 -150 -40 -100 -200 -54 7000 1974 -60 -160 -40 -120 -180 -50 50 -50 -20 -40 -80 110 -52 7000 1975 180 30 10 -180 -100 -20 50 -110 140 100 20 390 43 7000 1976 250 70 -30 -110 -230 -20 40 180 170 -140 60 -80 13 7000 1977 -230 -190 -170 -90 -40 0 0 -240 -70 -240 -130 10 -116 7000 1978 -50 -180 -180 -310 -250 -90 -90 -130 -80 -40 300 70 -86 7000 1979 80 100 -150 -340 -200 0 -30 -190 -140 -40 -10 170 -63 7000 1980 -40 150 -180 -130 -120 70 10 -50 80 220 -20 -70 -8 7000 1981 230 170 -50 0 -70 70 70 -110 -80 -100 250 170 45 7000 1982 100 240 -10 80 -30 -10 170 -20 320 0 10 130 80 7000 1983 80 50 -60 -180 -50 120 130 270 130 50 310 280 95 7000 1984 150 150 0 -40 10 -140 50 80 150 70 190 250 77 7000 1985 0 -50 70 -130 -150 -50 -50 -130 -20 320 280 -70 2 7000 1986 -80 120 200 -30 -120 110 -110 -200 -60 80 150 -20 2 7000 1987 -70 -180 -30 -170 -80 -90 70 30 110 460 210 -20 22 7000 1988 200 -130 -50 -10 -160 80 130 -130 170 320 200 390 85 7000 1989 380 430 140 -70 20 140 180 190 220 250 210 200 190 7000 1990 90 170 310 260 350 210 90 130 -100 140 110 60 152 7000 1991 -200 -170 -130 0 -140 -30 100 250 290 350 300 350 82 7000 1992 280 20 -50 -520 -210 -200 -150 -140 -180 -60 -60 160 -92 7000 1993 31XX 170 0 -110 0 -90 -30 -40 -370 -100 -160 31099999 -40 7000 1994 3031 - 240 370 280 170 290 280 310 400 360 -220999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. RUSSKII (RUSSKII OSTROV) 030380 77 10 N 96 26 EK7042002 39 2 0 39 1951 -60 -110 -250 -170 -70 60 -10 100 20 420 100 100 12 7000 1952 -140 -270 -150 -80 -10 -50 170 30 80 90 -40 -50 -34 7000 1953 -80 -40 140 0 60 200 70 140 200 100 150 390 112 7000 1954 110 130 140 80 -130 50 170 0 30 190 230 260 105 7000 1955 70 -200 -290 0 30 20 -100 90 0 120 60 -30 -18 7000 1956 -210 -180 -30 -300 -150 -30 -70 -180 -120 -100 -110 -60 -128 7000 1957 90 -200 -160 -110 -80 -20 0 0 -20 -30 -40 0 -46 7000 1958 -130 -90 -250 -150 -280 -30 -50 60 -60 -60 50 -30 -85 7000 1959 -110 260 170 -80 -80 120 120 -10 -90 -70 70 220 42 7000 1960 -60 -30 -40 -70 -100 100 60 -20 -70 30 30 60 -9 7000 1961 -100 0 -70 -220 -150 -30 -50 -150 0 -30 30 50 -61 7000 1962 90 -30 -190 -40 -160 -70 -20 -40 -80 0 0 100 -37 7000 1963 0 110 50 -30 0 -60 100 -110 10 40 0 220 27 7000 1964 190 110 130 -90 50 110 160 20 -80 50 40 40 61 7000 1965 70 -140 0 0 -30 130 110 -30 -30 50 -30 -20 8 7000 1966 30 -170 -230 -290 10 40 60 0 150 40 100 120 -10 7000 1967 270 260 50 130 40 80 50 30 220 400 240 100 155 7000 1968 50 0 110 -50 -30 90 130 90 -40 20 -70 90 33 7000 1969 -170 -200 -60 -60 -110 30 30 -20 -30 10 90 270 -17 7000 1970 60 -110 -220 -70 20 170 80 90 0 0 20 70 10 7000 1971 150 -130 0 -70 -10 20 70 50 120 110 60 60 37 7000 1972 110 190 20 130 50 70 150 130 70 280 -80 160 107 7000 1973 240 130 170 -100 40 210 140 30 40 -50 -100 -130 51 7000 1974 -120 -290 -70 -110 -150 -30 40 -20 -80 -30 -50 30 -72 7000 1975 130 100 70 -150 -100 -30 50 -20 170 140 60 350 64 7000 1976 29 XX 10099999 -40 -80 -180 -30 90 140 280 -50 90 -80 -41 7000 1977 -280 -240 -150 -130 -80 -40 -40 -240 0 -100 -120 10 -117 7000 1978 0 -100 -140 -270 -240 -30 -60 -10 -60 0 210 60 -53 7000 1979 80 140 -160 -340 -200 -20 -10 -130 -110 0 0 160 -50 7000 1980 -30 20 -110 -60 -40 90 40 0 50 80 -100 -50 -9 7000 1981 60 -10 -80 30 20 110 90 40 50 120 40 100 48 7000 1982 50 -10 -50 20 -70 -20 80 40 50 110 40 100 29 7000 1983 -40 -120 -110 -220 -100 40 60 -50 -20 -20 0 50 -43 7000 1984 0 -70 -60 -100 -30 -30 40 0 10 40 20 70 -9 7000 1985 -10 -90 -80 -150 -170 -30 20 -20 0 10 10 60 -37 7000 1986 312831 313130313031 - 999999999999999 -40 -90 9099999999999999999999999999999999999 7000 1987 3128 313130313031 - 9999999999 270 190 250 24099999999999999999999999999999999999 7000 1988 312931 3130313031 - 999999999999999 -70 -20 270 330999999999999999999999999999999 7000 1989 3128 3130313031 - 9999999999 50 -70 0 130 140999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Unreasonable data value of -770 deleted from February 1976. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KRASNOFLOTSKIE (KRASNOFLOTSKIE OSTROVA) 030385 78 36 N 98 50 EK7042002 34 2 0 39 1954 50 -10 0 -70 -250 -60 30 -70 -60 0 190 -40 -25 7000 1955 0 -310 -330 -150 -150 0 30 100 40 100 -180 -110 -78 7000 1956 -230 -180 20 -250 -170 -20 10 -130 -30 -70 -200 -130 -115 7000 1957 60 -110 -80 0 60 90 150 80 20 -10 -40 20 21 7000 1958 -30 -90 -190 -90 -140 -100 -10 90 -950 20 120 10 -112 7000 1959 -60 280 140 -100 -110 50 50 -60 -110 -90 0 200 14 7000 1960 -60 80 20 0 -20 110 20 10 -20 90 50 70 29 7000 1961 0 30 -80 -130 -50 -30 -50 -110 30 -10 0 30 -31 7000 1962 150 50 10 -10 -110 -50 -10 10 -20 60 60 70 17 7000 1963 50 150 40 -90 -70 -60 110 -80 30 30 -40 150 18 7000 1964 120 50 20 -190 -20 30 80 -50 -80 50 10 0 2 7000 1965 50 -140 -20 -60 -80 80 30 10 0 80 10 -10 -3 7000 1966 30 -100 -140 -180 100 60 60 40 80 40 20 40 5 7000 1967 120 140 40 70 0 70 70 -10 80 100 10 -30 54 7000 1968 -80 -110 50 -30 -30 100 110 20 -80 -10 -180 -50 -23 7000 1969 -260 -280 -90 -100 -110 20 10 -10 0 -40 20 20 -67 7000 1970 0 -120 -220 -50 0 170 50 30 0 10 80 30 -1 7000 1971 50 -250 -140 -200 -60 -20 70 40 100 40 150 0 -17 7000 1972 0 50 -70 0 -30 -20 120 20 -20 70 -160 130 8 7000 1973 110 -70 -90 -290 -110 10 90 70 60 90 -30 0 -12 7000 1974 -40 -180 -40 -120 -130 -20 100 110 -30 0 -90 -10 -36 7000 1975 50 30 0 -90 -70 -20 80 40 60 180 90 110 39 7000 1976 -30 70 -20 -10 50 220 60 30 -20 -60 10 -100 16 7000 1977 -280 -210 -80 0 20 -20 20 -60 10 -60 90 210 -29 7000 1978 290 0 -30 -110 -110 0 0 60 0 0 110 30 20 7000 1979 90 120 -310 -270 -120 60 30 10 0 60 60 200 -7 7000 1980 20 80 -60 -40 -20 130 100 90 120 110 0 -40 40 7000 1981 110 40 -100 20 50 20 70 -10 0 -120 20 180 23 7000 1982 80 120 -90 40 30 30 110 70 100 10 -40 20 39 7000 1983 90 40 -80 -140 -10 70 120 120 -20 20 200 190 50 7000 1984 50 50 20 -40 30 70 40 50 30 -30 80 160 43 7000 1985 20 80 110 -50 -60 80 50 90 150 80 -30 50 47 7000 1986 160 220 270 -30 -90 90 20 30 10 110 50 -90 62 7000 1987 -100 -40 40 -90 0 0 120 20 10 240 -110 -90 1 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Unreasonable data value of -950 deleted from September 1958. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. GEIBERGA (GEIBERGA OSTROV) 030387 77 36 N101 31 EK7042002 45 0 0 39 1951 -40 -90 -190 -150 -90 20 0 60 0 240 40 30 -13 7000 1952 -190 -280 -220 -210 -70 -110 140 0 40 50 -120 -110 -89 7000 1953 -220 -150 -40 -90 -50 80 50 60 110 30 100 340 19 7000 1954 80 70 90 40 -130 30 130 -10 -20 30 210 0 43 7000 1955 0 -330 -310 -40 -210 -20 70 150 -20 40 -70 -90 -67 7000 1956 -190 -190 -20 -270 -130 -30 -30 -210 -110 -90 -150 -90 -125 7000 1957 50 -240 -190 -110 -130 -110 -40 -50 -70 -80 -110 -60 -94 7000 1958 -130 -180 -250 -160 -210 -30 -20 80 -70 -60 30 -90 -90 7000 1959 -140 250 200 -20 0 160 120 -40 -70 -50 50 190 53 7000 1960 70 110 -30 -50 -80 90 20 -60 -60 20 -10 50 5 7000 1961 -20 130 -60 -150 -80 -10 -10 -120 40 20 100 50 -10 7000 1962 110 60 -20 40 -20 10 10 0 -20 60 20 30 23 7000 1963 70 190 90 -40 -50 -100 70 -100 10 50 -50 180 26 7000 1964 60 10 20 -180 -20 20 80 -50 -160 20 -30 -40 -22 7000 1965 0 -230 -110 -120 -110 10 -10 -100 -120 -30 -50 -60 -76 7000 1966 -50 -160 -230 -310 -50 -90 -120 0 100 50 0 -30 -73 7000 1967 90 80 -50 0 -40 0 60 50 160 270 240 100 80 7000 1968 50 40 120 -90 -230 -10 130 40 -50 50 -120 60 0 7000 1969 -180 -240 -60 -60 -90 40 20 -20 -40 10 20 120 -39 7000 1970 -30 -140 -300 -80 0 160 50 70 -10 -30 -10 60 -21 7000 1971 60 -200 -50 -80 20 10 80 30 120 110 80 30 19 7000 1972 20 0 -180 -20 -100 -80 90 60 0 160 -140 130 -4 7000 1973 130 -50 -60 -280 -90 70 40 -20 -10 0 -70 -80 -34 7000 1974 -70 -230 -50 -110 -150 -30 40 -20 -90 -40 -50 50 -61 7000 1975 80 30 0 -140 -70 -10 80 30 130 160 60 270 52 7000 1976 20 130 10 -40 -140 0 80 120 220 -20 70 -90 29 7000 1977 -280 -210 -140 -80 -50 10 60 -150 40 -70 -130 -20 -84 7000 1978 -20 -110 -140 -220 -140 -10 -30 -40 -50 -60 180 -10 -54 7000 1979 -90 -60 -240 -230 -140 0 20 -150 -120 -30 -20 150 -76 7000 1980 -70 80 -110 -80 -80 80 60 10 60 110 -60 -50 -5 7000 1981 140 80 -100 40 30 50 90 40 0 -130 100 80 34 7000 1982 20 140 -70 30 -90 -30 90 80 260 -60 -60 0 25 7000 1983 10 -20 -80 -150 -40 80 150 120 -20 100 270 210 53 7000 1984 80 160 90 -30 40 70 30 70 30 -50 20 180 57 7000 1985 -40 -100 0 -150 -170 -10 -40 -100 -80 90 120 -80 -46 7000 1986 -100 90 180 40 -60 110 0 -40 -30 30 20 0 19 7000 1987 -40 -60 -30 -140 -60 -40 80 -10 30 220 130 30 10 7000 1988 160 -40 -60 -10 -150 40 120 -10 90 170 110 240 55 7000 1989 210 190 20 -40 20 190 240 150 200 110 20 110 118 7000 1990 -40 40 200 180 280 160 200 160 -90 70 0 50 102 7000 1991 -30 20 -140 30 -20 0 90 130 40 190 110 290 60 7000 1992 270 150 150 -100 150 180 280 100 60 80 60 280 139 7000 1993 30 31 - 340 200 140 90 20 90 260 -1099999 -10 1609999999999 7000 1994 312831 31 - 999999999999999 -190 -20 2099999 210 80 220 180 8099999 7000 1995 31 303130313130313031 - 99999 -40 -11099999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SOLNECHNAIA (SOLNECHNAIA BUKHTA) 030390 78 12 N103 16 EK7042002 39 0 0 39 1951 -160 -140 -250 -230 -130 -10 -30 40 -30 170 30 -10 -62 7000 1952 -230 -310 -250 -220 -70 -110 110 -20 20 60 -140 -160 -109 7000 1953 -220 -150 -30 -110 -60 40 -40 20 80 20 20 200 -18 7000 1954 -120 80 90 -40 -130 -10 0 -10 -10 -100 -80 -100 -37 7000 1955 110 -220 -300 -140 -80 0 140 50 -40 20 -50 -80 -48 7000 1956 -210 -220 -100 -320 -170 -70 -100 -160 -90 -120 -250 -250 -171 7000 1957 -60 -310 -280 -200 -170 -120 -50 -90 -70 -60 -50 -60 -125 7000 1958 -200 -200 -290 -210 -240 -60 -30 60 20 -90 20 -120 -112 7000 1959 -200 200 160 -100 -80 120 80 -20 -50 -20 -50 10 3 7000 1960 -120 120 80 -30 -10 170 -80 10 60 60 -90 -60 8 7000 1961 -120 -60 -110 -200 -110 -50 -20 -40 150 20 -60 -60 -55 7000 1962 90 -120 -230 -40 -100 -20 10 30 -40 30 -70 -20 -39 7000 1963 -20 150 100 -80 -40 10 220 40 50 20 -80 -50 26 7000 1964 -100 -30 -90 -180 -60 0 100 40 30 160 100 140 10 7000 1965 170 -90 10 -60 -40 0 40 60 0 20 80 -10 16 7000 1966 40 -120 -240 -300 -70 -100 -110 60 90 80 50 -80 -58 7000 1967 90 120 -40 50 10 30 60 60 140 170 200 150 86 7000 1968 -80 -140 60 -50 0 60 120 100 -10 10 -10 -10 5 7000 1969 -140 -230 -60 -10 -10 120 60 60 -10 -60 80 80 -9 7000 1970 10 -140 -230 -70 0 170 80 100 70 130 230 200 47 7000 1971 210 -80 70 40 200 140 130 60 110 60 40 10 84 7000 1972 30 70 -120 -10 20 40 110 50 -30 10 -120 190 20 7000 1973 160 0 -80 -260 -70 70 60 0 80 10 -60 -60 -12 7000 1974 -140 -230 -90 -120 -130 30 120 50 -70 -100 -180 -60 -75 7000 1975 -30 -20 -70 -130 -200 -110 0 -10 70 90 10 -10 -34 7000 1976 -110 -10 -70 -80 -140 -10 60 30 0 -40 50 -60 -32 7000 1977 -230 -100 -150 -20 -20 40 120 50 30 10 -50 20 -25 7000 1978 -50 -80 -80 -140 -100 40 60 90 -30 10 190 100 1 7000 1979 -50 -30 -250 -190 -70 70 120 60 70 60 60 180 3 7000 1980 -40 60 -90 -20 10 190 190 150 160 110 50 -10 63 7000 1981 140 100 -40 90 120 120 180 140 40 -70 50 160 86 7000 1982 100 200 0 100 30 90 190 170 170 80 50 110 107 7000 1983 130 50 -20 -80 60 150 200 140 20 50 200 190 91 7000 1984 150 120 90 100 110 170 190 140 50 10 90 180 117 7000 1985 20 40 190 30 -60 80 80 100 50 140 150 0 68 7000 1986 -20 110 140 60 10 200 150 40 100 40 100 90 84 7000 1987 60 -60 -90 -130 250 310 120 140 50 200 110 110 90 7000 1988 260 50 50 0 -120 110 230 50 110 180 130 210 105 7000 1989 180 210 20 -110 -80 90 110 150 80 120 110 110 82 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. FEDOROVA (CHELUSKIN MYS) 030392 77 43 N104 18 EK7042002 46 0 0 39 1950 20 -60 -150 -180 -100 10 -80 -10 20 120 -80 -110 -50 7000 1951 -80 -130 -230 -190 -100 30 0 120 90 370 90 80 5 7000 1952 -180 -230 -180 -210 -70 -80 140 20 70 80 -110 -100 -70 7000 1953 -140 -80 80 -90 -30 100 40 130 180 70 110 290 56 7000 1954 90 80 100 20 -160 -10 100 -70 20 80 220 30 41 7000 1955 40 -210 -290 -130 -170 0 80 130 -20 80 -40 -60 -48 7000 1956 -160 -180 0 -300 -140 -80 -20 -190 -50 -80 -100 -100 -116 7000 1957 60 -240 -220 -110 -110 -50 0 30 0 -90 -50 40 -60 7000 1958 -40 -100 -170 -160 -240 -20 -20 60 50 10 130 80 -35 7000 1959 -40 270 240 -20 -10 160 60 -60 -40 -110 70 250 63 7000 1960 110 250 80 -20 -30 180 30 -100 -90 -20 -50 -10 27 7000 1961 -140 -60 -140 -210 -140 -40 -40 -150 80 90 120 140 -41 7000 1962 260 100 0 70 -70 0 -10 -20 -60 10 0 -10 22 7000 1963 20 110 40 -70 -60 -60 120 -70 80 110 -30 200 32 7000 1964 120 70 40 -190 0 30 160 30 -80 0 -80 -30 6 7000 1965 40 -220 -60 -100 -70 70 30 -140 -20 -20 -60 -60 -50 7000 1966 -90 -250 -250 -270 70 20 40 10 180 -40 -20 10 -48 7000 1967 130 120 -30 70 10 80 40 100 260 390 250 110 127 7000 1968 60 -20 70 -90 -90 50 90 80 -30 40 -90 50 11 7000 1969 -180 -250 -100 -120 -170 20 30 30 -30 60 40 180 -39 7000 1970 -30 -130 -200 -90 -10 140 30 30 0 -70 -30 90 -22 7000 1971 80 -190 -50 -150 -10 20 120 100 160 190 50 80 35 7000 1972 120 60 -150 -30 -170 -120 80 110 10 300 -180 130 14 7000 1973 160 -40 -70 -230 -20 120 30 40 -20 -60 -150 -210 -37 7000 1974 -130 -210 0 -100 -150 -40 50 -90 -90 -140 -190 0 -90 7000 1975 50 30 -20 -180 -100 -40 80 -10 120 160 100 370 47 7000 1976 110 150 0 -70 -140 0 80 220 220 -60 110 -80 44 7000 1977 -270 -190 -140 -80 -70 10 30 -130 60 -140 -130 20 -86 7000 1978 -20 -80 -80 -230 -160 -40 -30 -90 -30 -10 260 10 -42 7000 1979 -90 -90 -310 -300 -210 -20 40 -180 -130 -80 -50 100 -110 7000 1980 -150 50 -140 -80 -120 100 70 -20 50 180 -30 90 0 7000 1981 330 140 -70 80 40 70 140 -10 -10 -140 190 160 76 7000 1982 50 200 0 110 20 80 160 -10 40 -80 -70 90 48 7000 1983 110 40 -50 -130 -10 110 170 190 70 10 160 220 75 7000 1984 80 100 40 -40 60 150 50 20 90 0 50 130 61 7000 1985 -130 -180 -20 -180 -210 -20 -100 -130 -60 80 170 -140 -76 7000 1986 -110 20 140 40 0 170 -10 -100 -30 70 50 -20 18 7000 1987 -10 -90 -40 -150 -20 -90 40 -10 30 360 160 70 22 7000 1988 290 60 -70 -40 -190 70 140 -30 150 170 90 270 76 7000 1989 300 370 180 10 80 200 170 90 280 210 140 30 170 7000 1995 3128313031 313130313031 - 9999999999999999999999999 7099999999999999999999999999999999999 7000 1996 31293130 30313130313031 - 99999999999999999999 409999999999999999999999999999999999999999 7000 1997 3128313031303131 313031 - 9999999999999999999999999999999999999999 19099999999999999999999 7000 1998 3128313031 313130313031 - 9999999999999999999999999 2099999999999999999999999999999999999 7000 1999 3128313031303131303130 - 9999999999999999999999999999999999999999999999999999999 23099999 7000 2000 31 31 31 31 - 99999 170 40 170 220 34099999 50 8099999 -509999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KOSYSTYI (KOSYSTYI MYS) 030394 73 39 N109 44 EK7042002 36 0 0 39 1954 110 170 250 30 150 170 230 -10 70 80 200 160 134 7000 1955 150 -90 -310 -150 -220 350 160 190 90 300 -30 270 60 7000 1956 180 80 110 -80 40 320 200 100 90 210 30 -90 99 7000 1957 130 -170 -110 -10 -40 40 120 80 220 120 110 120 52 7000 1958 -30 -130 -220 -100 -200 120 350 220 190 160 240 180 66 7000 1959 40 200 90 -50 -50 300 280 150 170 90 80 210 125 7000 1960 -70 -10 10 0 -30 330 330 230 270 -30 -130 -10 74 7000 1961 -70 30 -110 -90 -10 150 340 100 200 160 130 -10 68 7000 1962 70 -90 -160 -60 -160 -100 220 90 190 290 60 40 34 7000 1963 160 140 130 30 70 210 380 0 0 30 30 260 120 7000 1964 260 220 120 -90 30 80 400 80 -10 90 80 150 118 7000 1965 0 -120 -30 -20 -60 180 220 30 -30 120 140 20 38 7000 1966 50 -20 -130 -200 50 200 290 170 200 70 210 70 81 7000 1967 190 110 30 50 100 310 220 210 230 250 200 60 163 7000 1968 20 -60 30 -20 0 180 270 140 90 270 70 150 96 7000 1969 -50 -180 0 -10 -80 320 210 110 110 130 -40 150 57 7000 1970 -70 -200 -270 -210 -190 60 190 110 100 70 40 -20 -31 7000 1971 -110 -330 -170 -200 -90 140 180 -10 170 170 20 30 -15 7000 1972 10 -50 -240 -150 -170 0 190 140 -10 230 -30 90 2 7000 1973 190 -80 -190 -250 -220 80 150 -40 40 60 10 -70 -26 7000 1974 10 -170 -150 -160 -130 80 220 -60 -50 100 130 -140 -26 7000 1975 -70 -30 -40 -210 -180 170 230 0 0 50 -10 60 -2 7000 1976 -120 -170 -240 -240 -310 -40 170 50 90 -80 -130 -240 -105 7000 1977 -360 -290 -190 -200 -190 140 100 -30 60 80 -120 -40 -86 7000 1978 -20 -140 -100 -180 -180 120 0 -10 -150 -130 60 -100 -69 7000 1979 -210 -240 -410 -410 -290 -160 -20 -20 -70 0 -40 90 -147 7000 1980 -60 -60 -210 -250 -200 90 140 60 20 60 100 -140 -38 7000 1981 0 0 -200 -50 -60 190 120 10 10 -70 -100 60 -8 7000 1982 -190 -30 -220 -140 -170 30 180 -30 30 0 -50 -30 -52 7000 1983 -40 -160 -210 -270 -150 150 80 -10 -90 -80 60 -40 -63 7000 1984 -160 -150 -150 -180 -110 140 -30 -130 -20 -50 -160 130 -72 7000 1985 -160 -160 0 -200 -170 400 20 -40 -60 40 50 -230 -43 7000 1986 -210 -60 -110 -80 -60 270 80 -80 -180 -10 -30 -30 -42 7000 1987 -40 -130 -120 -190 -110 -20 250 -80 -80 140 40 -90 -35 7000 1988 -70 -230 -220 -180 -310 50 60 -70 30 0 -30 -160 -94 7000 1989 -240 -230 -440 -510 -600 -370 -120 20 -50 -260 -260 -290 -279 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SVIATOI NOS (SVIATOI NOS MYS) 030397 72 50 N140 44 EK7042002 37 0 0 39 1951 -90 -100 -160 -160 -60 130 30 90 -20 70 -140 -10 -34 7000 1952 -170 -250 -140 -120 -100 10 80 0 -50 100 10 -90 -59 7000 1953 -160 -30 20 0 -180 130 30 120 30 60 130 70 18 7000 1954 -10 -30 40 -30 -140 10 190 150 110 0 140 140 48 7000 1955 40 -250 -240 -100 -100 110 110 250 210 110 -80 -60 2 7000 1956 -100 0 0 -160 -60 60 90 -60 -80 160 40 -80 -16 7000 1957 50 -160 -190 -60 -120 0 140 260 10 90 10 -90 -4 7000 1958 -150 -180 -200 -60 -190 40 0 150 -20 130 0 -100 -48 7000 1959 -210 130 -10 -70 -70 120 90 -130 -250 130 10 260 -1 7000 1960 -100 -60 -20 40 -70 100 -40 0 10 -60 -10 -10 -19 7000 1961 -210 -20 -260 -280 -60 70 -10 -110 -240 180 280 -30 -58 7000 1962 -50 -90 -280 -100 -140 110 150 170 -80 130 130 -30 -6 7000 1963 -120 -60 30 -60 -10 130 220 20 50 110 -80 150 33 7000 1964 60 140 30 -130 50 -10 30 -120 -220 -110 -260 -10 -46 7000 1965 -200 -300 -230 -10 -20 110 -170 -120 -400 180 30 -140 -105 7000 1966 -10 -20 -130 -160 0 200 100 -70 50 -120 140 80 5 7000 1967 -70 -40 -90 0 20 80 180 280 200 410 120 -30 89 7000 1968 -10 -190 0 -40 80 140 110 170 0 10 -90 100 25 7000 1969 -80 -200 -90 -60 -80 260 80 110 120 270 -50 100 33 7000 1970 -200 -300 -220 -60 0 250 90 130 200 -290 20 40 -28 7000 1971 -130 -100 -30 -180 -20 110 -10 50 200 120 0 110 11 7000 1972 30 -100 -230 -150 -80 40 130 180 -80 410 -50 30 12 7000 1973 170 -110 -170 -200 -110 120 110 -50 40 50 -50 -40 -19 7000 1974 130 -250 -160 -260 -130 70 190 -90 -20 -70 150 120 -25 7000 1975 200 230 120 0 -70 -80 130 10 10 190 270 200 100 7000 1976 -180 -150 -140 -190 -210 70 210 300 100 -50 70 -130 -25 7000 1977 -220 -200 -200 -70 -80 80 20 -10 150 -360 -210 -120 -102 7000 1978 -160 -310 -230 -320 -200 0 40 -220 -260 -130 110 30 -136 7000 1979 -110 -120 -280 -240 -100 0 90 -160 -10 -40 30 130 -67 7000 1980 -100 40 0 -170 -150 310 -70 0 0 360 -80 -250 -10 7000 1981 40 130 -120 -30 -50 -130 40 100 150 -110 190 290 41 7000 1982 220 300 110 150 150 310 250 20 340 -60 100 210 173 7000 1983 260 360 -30 -180 -50 150 160 20 200 -40 40 70 78 7000 1984 110 160 40 10 120 210 190 180 270 -120 -50 250 114 7000 1985 20 110 370 40 20 170 120 -100 240 220 50 -240 84 7000 1986 0 60 160 70 60 440 310 210 250 380 180 -100 168 7000 1987 -80 -280 -120 -140 -100 60 50 0 -10 10 -10 -20 -52 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. PESCHANYI (PESCHANYI MYS) 030405 79 26 N102 29 EK7042002 32 0 0 39 1962 -30 -110 -170 -70 -150 0 50 90 -20 -120 -140 -80 -62 7000 1963 -30 80 10 -20 -100 -90 130 40 100 60 10 150 28 7000 1964 0 -80 -10 -140 100 70 100 0 -50 20 -70 0 -4 7000 1965 60 0 -90 -100 -80 30 30 -10 -30 110 10 -10 -7 7000 1966 0 -110 -190 -240 80 70 60 10 80 -60 -60 -90 -37 7000 1967 30 60 -70 10 -30 0 60 40 120 160 20 0 33 7000 1968 -80 -120 0 -110 -50 10 -10 -30 -200 -80 -180 -10 -71 7000 1969 -230 -250 -130 -150 -150 0 0 -10 0 -90 -10 10 -83 7000 1970 -60 -200 -300 -170 -90 90 10 20 -40 30 0 0 -58 7000 1971 30 -210 -120 -180 -30 0 50 40 90 60 10 -20 -22 7000 1972 0 -10 -80 -70 -120 -70 80 20 -80 20 -220 70 -38 7000 1973 80 -70 -80 -320 -120 20 -20 -40 0 20 -130 -60 -59 7000 1974 -60 -210 -60 -120 -160 -40 70 0 -130 -160 -150 -30 -86 7000 1975 30 -70 -140 -250 -190 -150 40 60 -40 -90 0 50 -62 7000 1976 -60 50 -60 -90 -150 -30 80 100 10 -100 20 -90 -27 7000 1977 -270 -160 -160 -140 -90 -80 0 -70 30 -50 0 290 -58 7000 1978 20 -20 30 20 130 140 50 50 -20 50 180 0 53 7000 1979 -130 -100 -300 -250 -150 0 40 -20 10 40 -80 90 -70 7000 1980 -130 -30 -80 -90 -130 50 80 120 80 50 -40 -40 -13 7000 1981 110 50 -120 20 60 60 100 10 10 -110 90 120 33 7000 1982 50 160 -40 -10 -70 10 160 110 140 0 -10 60 46 7000 1983 30 0 -70 -130 -10 100 170 130 0 20 140 190 48 7000 1984 30 30 0 -70 10 20 10 110 100 -20 40 260 44 7000 1985 100 50 70 -130 -140 10 20 40 40 140 70 -90 15 7000 1986 -50 90 190 90 20 190 120 50 70 40 20 0 69 7000 1987 0 -50 -30 -120 -60 -40 70 60 70 150 50 10 10 7000 1988 170 -20 -60 -50 -170 10 140 40 120 160 290 430 89 7000 1989 440 430 350 220 250 340 300 0 80 -30 -150 -320 157 7000 1990 -240 -30 90 90 190 60 110 100 -20 10 30 180 48 7000 1991 110 80 60 -20 150 50 80 60 0 60 90 110 70 7000 1992 130 50 10 -220 40 20 70 110 50 -20 -60 60 21 7000 1993 31303130313130313031 - 130 209999999999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ANDREIA (ANDREIA OSTROV) 030410 76 48 N110 45 EK7042002 49 3 0 39 1951 90 40 -30 20 60 110 110 140 40 190 -10 -40 60 7000 1952 -280 -340 -240 -250 -150 -130 90 340 30 40 -150 -30 -87 7000 1953 -70 -110 -30 -140 -150 10 -20 40 130 10 50 220 -4 7000 1954 -140 -120 -60 -60 -170 40 70 -120 -60 -60 100 20 -47 7000 1955 70 -260 -340 -140 -200 -20 40 160 -60 70 -230 -210 -92 7000 1956 -220 -220 -20 -320 -230 -120 -80 -190 -40 -140 -240 -260 -173 7000 1957 -120 -460 -460 -320 -230 -90 -60 -10 -20 -70 -170 -100 -174 7000 1958 -190 -350 -390 -280 -250 -30 -10 150 120 100 -120 -220 -121 7000 1959 -300 60 20 -210 -200 40 30 -20 -60 -30 -40 -90 -68 7000 1960 -140 -100 -100 -130 -140 60 20 -10 -60 -110 -80 -20 -67 7000 1961 -140 -110 -230 -350 -250 -140 30 -120 -30 80 10 -70 -110 7000 1962 -10 -70 -160 20 -20 30 90 -40 -10 70 90 60 4 7000 1963 0 70 20 -70 -90 -110 100 -70 -60 110 -40 260 10 7000 1964 100 80 60 -140 -40 60 170 -30 -30 130 -70 10 25 7000 1965 -40 -220 0 140 0 190 160 -120 -80 10 -50 -90 -7 7000 1966 -40 -180 -280 -350 -150 -90 90 10 120 60 30 10 -63 7000 1967 140 80 -120 60 -20 40 60 120 300 420 360 280 143 7000 1968 50 -60 60 -90 -40 40 90 90 30 160 10 130 40 7000 1969 -190 -280 -140 -130 -140 50 0 40 70 100 0 120 -40 7000 1970 60 -80 -290 -120 -40 130 20 -10 60 -50 30 70 -18 7000 1971 0 -270 -130 -160 -10 20 20 10 100 190 30 70 -9 7000 1972 80 50 -180 -90 -120 -80 120 140 -30 310 -140 130 17 7000 1973 180 -90 -130 -270 -60 100 0 10 160 20 -40 -20 -11 7000 1974 80 -120 -30 -90 -90 20 150 -60 -30 -90 -90 50 -24 7000 1975 110 130 70 -130 -80 -30 140 50 130 190 130 190 75 7000 1976 50 80 -20 -40 -130 20 120 270 230 -40 190 140 72 7000 1977 60 10 80 -50 -80 10 100 -70 100 -90 -50 100 10 7000 1978 10 -60 -80 -190 -180 -40 -10 -90 -60 -20 200 -20 -45 7000 1979 -160 -150 -330 -250 -90 0 20 -160 -200 -60 -30 130 -106 7000 1980 -110 70 -150 -150 -70 90 40 10 130 200 -20 -70 -3 7000 1981 40 -10 -60 40 80 170 270 110 50 -70 190 140 80 7000 1982 -50 90 -90 0 -70 -20 120 60 320 20 80 60 42 7000 1983 90 -40 -90 -180 -30 110 140 200 130 70 180 190 65 7000 1984 70 10 20 -70 30 70 30 50 90 10 20 200 45 7000 1985 -80 -90 70 -90 -110 40 -20 -110 -40 120 110 -110 -26 7000 1986 -100 30 70 -20 -120 120 40 -20 -10 100 50 0 11 7000 1987 -80 -140 -80 -200 -80 -40 50 60 160 420 160 10 21 7000 1988 130 -70 -70 -60 -210 20 30 70 180 190 70 190 40 7000 1989 170 160 10 -70 -10 120 110 180 310 180 40 60 105 7000 1990 -70 0 150 120 240 150 230 180 -140 40 -30 70 80 7000 1991 -40 10 -110 110 10 0 180 140 140 230 120 360 97 7000 1992 220 90 60 -200 90 110 230 100 40 80 30 220 90 7000 1993 30 31 - 280 130 50 -50 10 110 280 16099999 -50 2009999999999 7000 1994 31 XX 99999 30 -50 -150 -110 0 120 190 40 310 280 330 91 7000 1995 303130313130313031 - 130 180 4099999999999999999999999999999999999999999999999999 7000 1996 31293130 30 3130313031 - 99999999999999999999 -6099999 200999999999999999999999999999999 7000 1997 3128313031303131 - 9999999999999999999999999999999999999999 20 100 130 13099999 7000 1998 28 31 3131 3130 - 12099999 50 -20099999 1109999999999 1509999999999 33099999 7000 1999 3130313130313031 - 130 180 40 -30999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Feb10 : New coordinates for staions ANDREIA are 76 48 N 110 45 E Ref. letter from 09.02.03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MALYI TAIMYR (MALYI TAIMYR OSTROV) 030414 78 05 N106 49 EK7042002 42 0 0 39 1950 60 0 -90 -130 -50 50 -10 -60 -60 160 -20 -70 -18 7000 1951 -120 -80 -140 -120 0 110 90 70 0 150 100 50 10 7000 1952 -160 -240 -180 -170 0 -40 70 -10 20 100 -110 -190 -75 7000 1953 -170 -150 -50 -130 -120 0 -30 30 120 50 -50 180 -26 7000 1954 20 0 50 -20 -110 0 90 20 50 30 90 -60 13 7000 1955 40 -170 -260 -90 -110 20 20 70 -30 50 -20 -200 -56 7000 1956 -130 -150 70 -210 -100 0 70 -130 -40 -40 -120 -190 -80 7000 1957 20 -260 -220 -120 -90 -60 -10 -50 -30 -60 -70 -30 -80 7000 1958 -110 -70 -180 -200 -210 -20 30 70 20 -20 -20 -180 -74 7000 1959 -310 0 30 -230 -130 10 -150 -30 -50 -20 -60 -60 -84 7000 1960 -180 -120 -10 0 -30 150 90 60 60 120 10 0 13 7000 1961 -80 -90 -150 -140 -30 80 90 -50 90 0 50 20 -17 7000 1962 30 -40 -150 0 -40 70 20 40 0 50 -50 0 -6 7000 1963 -50 90 50 -60 -60 -40 120 -40 70 60 10 140 24 7000 1964 50 -30 30 -90 30 110 170 30 50 160 -20 50 46 7000 1965 80 10 210 -90 -10 90 120 10 -40 100 40 -50 40 7000 1966 -10 -10 -110 -210 30 70 40 30 40 -10 -70 -150 -30 7000 1967 60 50 -50 50 -10 30 20 30 60 100 130 60 44 7000 1968 -10 -60 90 20 80 0 50 30 -130 -10 -90 50 3 7000 1969 -160 -220 -60 -50 -60 -10 10 30 40 -30 0 20 -40 7000 1970 0 -110 -210 -10 50 190 90 50 0 20 60 60 16 7000 1971 40 -260 -120 -140 -10 40 40 10 40 30 0 -50 -30 7000 1972 -20 10 -110 -10 -30 0 90 20 0 60 -150 140 0 7000 1973 190 -30 -70 -220 -70 80 50 -60 80 40 -30 -10 -4 7000 1974 0 -230 -100 -120 -110 10 60 -20 -100 -90 -30 -20 -61 7000 1975 20 -10 -20 -190 -60 -40 40 20 20 120 90 60 5 7000 1976 10 60 -40 -30 -50 70 110 60 60 0 30 -120 13 7000 1977 -290 -210 -100 -90 -100 -20 40 -70 30 -10 -60 -50 -77 7000 1978 -80 70 -30 -100 -120 -10 0 -10 -50 -30 140 20 -18 7000 1979 -100 -70 -250 -260 -120 10 70 -40 -40 -10 0 110 -58 7000 1980 -80 10 -40 -30 -40 110 130 50 50 70 20 -10 20 7000 1981 90 80 -70 80 110 90 90 30 20 -90 80 170 56 7000 1982 60 180 -10 80 30 80 120 110 150 80 20 120 84 7000 1983 80 30 -40 -40 50 200 180 100 -30 60 230 140 80 7000 1984 -30 30 40 -50 50 100 70 90 0 -120 50 120 29 7000 1985 -70 -130 0 -110 -70 50 30 30 10 50 70 -30 -13 7000 1986 -60 70 50 0 -20 170 80 40 80 20 40 40 42 7000 1987 10 -50 -20 -100 -10 50 110 70 50 140 110 100 39 7000 1988 220 -60 -90 -70 -150 130 160 80 110 110 60 160 56 7000 1989 150 110 30 40 40 140 100 20 150 60 -10 40 72 7000 1990 -70 0 170 90 190 110 100 160 -40 80 40 110 79 7000 1991 20 80 -10 250 340 370 200 110 30 150 230 240 168 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. PREOBRAZHENIA (PREOBRAZHENIA OSTROV) 030418 74 40 N112 56 EK7042002 41 2 0 39 1951 70 20 -50 0 40 90 90 120 20 220 100 70 66 7000 1952 -150 -230 -70 -140 20 -20 40 -20 -10 -90 -150 -130 -78 7000 1953 -180 -20 80 20 0 110 -30 110 40 -50 -100 -10 -3 7000 1954 -60 -50 10 -100 -90 130 150 130 90 -40 170 120 39 7000 1955 70 -240 -260 -30 -210 -50 10 -380 70 170 30 90 -60 7000 1956 -90 -110 0 -190 -90 50 20 50 -30 90 10 -90 -31 7000 1957 80 -260 -220 -120 -150 -50 80 120 110 -40 -100 -70 -50 7000 1958 -180 -190 -280 -130 -190 60 60 150 30 210 10 -90 -44 7000 1959 -160 110 10 -150 -160 270 240 -40 -10 20 80 220 35 7000 1960 -120 -160 -180 -210 -230 -10 90 120 90 -10 -70 -100 -65 7000 1961 -190 -70 -280 -230 -100 -30 40 -10 120 110 170 -80 -46 7000 1962 -10 -120 -290 -140 -160 -100 20 90 0 120 -30 -50 -55 7000 1963 -120 10 0 -140 -110 -90 120 20 150 170 -20 250 21 7000 1964 80 80 60 -180 -90 10 200 0 -30 180 20 60 33 7000 1965 -70 -250 -180 -170 -190 40 20 -80 -160 100 90 10 -69 7000 1966 20 -110 -180 -260 20 80 70 80 110 40 130 10 2 7000 1967 220 140 20 0 -80 -10 150 130 210 310 240 100 119 7000 1968 40 -90 50 -60 10 60 150 150 30 200 30 120 59 7000 1969 -70 -180 -30 -80 -210 120 -180 120 160 210 -30 240 7 7000 1970 -10 -170 -270 -150 -40 130 110 190 180 110 140 170 34 7000 1971 100 -200 -70 -210 -50 50 80 70 240 180 70 50 28 7000 1972 40 -80 -210 -100 -70 -70 100 120 30 260 -80 190 12 7000 1973 300 -100 -130 -200 -120 70 90 90 50 70 -30 -120 -1 7000 1974 -70 -230 -140 -180 -160 -10 110 40 -10 90 120 180 -20 7000 1975 80 30 -40 -160 -150 -20 0 130 120 90 60 70 18 7000 1976 -220 -240 -290 -80 -160 40 110 200 140 -50 80 -90 -47 7000 1977 -230 -180 -140 -110 -140 20 80 80 150 10 -90 40 -42 7000 1978 40 -160 -150 -230 -170 10 -30 0 -10 -10 250 80 -31 7000 1979 -40 -20 -170 -280 -210 -100 0 -20 -70 0 10 120 -65 7000 1980 -180 -50 -180 -200 -160 40 30 80 120 150 40 -60 -31 7000 1981 140 0 -230 -50 -10 30 140 130 130 10 60 220 48 7000 1982 0 100 -130 -60 -100 -10 140 120 290 60 -10 10 33 7000 1983 60 -40 -130 -150 20 130 250 240 200 90 140 70 74 7000 1984 -30 -90 -100 -140 -40 0 20 160 50 0 50 210 8 7000 1985 -10 10 30 -200 -140 0 110 70 190 50 250 40 33 7000 1986 -50 30 -20 -120 -110 180 20 60 -20 70 -10 -40 -1 7000 1987 -130 -100 -60 -180 -60 10 90 60 120 -10 40 60 -13 7000 1988 60 -90 -60 -40 -210 70 270 70 20 190 170 70 44 7000 1989 -90 -340 -110 -120 -100 170 -100 80 -70 -270 -190 -140 -105 7000 1990 f -240 -20 120 90 210 150 140 180 50 160 120 100 89 7000 1991 f 650 80 40 120 50 110 80 130 110 180 80 260 159 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Possible new gauge in 1990. Years 1990 and 1991 flagged. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MARII PRONCHISHEVOI (BUKHTA) 030420 75 32 N113 26 EK7042002 20 0 0 39 1951 90 40 -30 20 60 110 110 140 40 240 120 90 86 7000 1952 -100 -180 -10 -80 80 40 100 40 50 -30 -90 -70 -20 7000 1953 -120 40 140 80 60 170 -20 170 100 220 170 260 106 7000 1954 110 60 100 -10 -170 10 100 190 270 260 220 180 110 7000 1955 90 -220 -400 -210 -230 -20 -30 180 80 230 180 50 -24 7000 1956 -160 -100 -100 -300 -160 40 -50 -130 -130 20 -60 -40 -97 7000 1957 70 -370 -190 -90 -100 -20 110 50 140 -70 -170 10 -50 7000 1958 0 -60 -160 -70 -170 230 140 100 60 70 130 50 27 7000 1959 -40 290 150 -50 80 370 120 -120 -110 -50 50 160 69 7000 1960 -160 -90 -160 -190 -220 -100 70 -10 -30 10 -60 10 -77 7000 1961 -190 -90 -320 -320 -190 -120 -70 -120 10 30 150 40 -100 7000 1962 30 -100 -260 -100 -140 -80 10 -20 -60 50 0 -20 -57 7000 1963 -60 30 40 -90 -50 -50 140 -120 40 -40 -130 200 -7 7000 1964 90 140 50 -170 -70 30 180 -20 -50 150 -10 140 39 7000 1965 -40 -180 -60 -20 -40 140 90 -130 -200 80 20 -80 -34 7000 1966 -70 -180 -260 -340 -50 -20 60 0 100 -40 50 -70 -68 7000 1967 120 50 -110 -10 -80 -10 150 230 290 390 270 130 119 7000 1968 210 -40 80 -50 10 70 140 80 -10 140 -20 90 60 7000 1969 -130 -230 -70 -90 -160 100 30 100 140 190 20 220 12 7000 1970 -30 -190 -290 -150 -60 110 10 50 80 10 70 100 -23 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ANABAR 030425 73 13 N113 30 EK7042002 9 0 0 39 1991 120 260 160 260 190 790 50 280 170 250 -80 40 206 7000 1992 0 40 -30 -410 -410 350 250 280 250 260 90 70 62 7000 1993 -80 -180 -100 -390 -250 390 10 100 -100 -80 0 -190 -72 7000 1994 -310 -290 -360 -270 -180 870 230 240 190 210 120 180 53 7000 1995 -80 -120 -420 -380 -330 870 860 110 190 -20 -40 -30 51 7000 1996 10 -160 -70 -70 -30 260 540 100 -40 -80 -110 -270 8 7000 1998 -380 -250 -300 -320 -270 -110 40 -50 90 -120 -140 -60 -155 7000 1999 -110 -230 -350 -240 -130 570 -10 70 210 -50 70 -160 -30 7000 2000 -200 -180 -350 -320 -170 840 60 -200 -90 -160 -250 -240 -106 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. TERPIAI-TUMSA 030430 73 33 N118 40 EK7042002 43 0 0 39 1956 -210 -60 -90 -240 -150 40 60 -40 -20 120 -80 -160 -69 7000 1957 40 -250 -260 -110 -170 50 110 80 130 -40 -90 -70 -47 7000 1958 -170 -130 -240 -160 -250 60 50 -50 30 20 -70 -150 -89 7000 1959 -170 90 0 -160 -170 250 90 -40 -30 90 110 150 17 7000 1960 -250 -190 -250 -280 -210 10 90 90 40 0 -70 -100 -93 7000 1961 -220 -80 -300 -280 -110 -50 0 -50 30 130 120 -110 -77 7000 1962 -50 -110 -260 -140 -150 -60 30 80 50 -60 40 20 -51 7000 1963 -190 -40 10 -130 -100 -60 120 -30 130 130 -30 60 -10 7000 1964 170 170 70 -130 50 30 150 50 -120 90 -50 140 52 7000 1965 -30 -110 -230 -130 -170 170 10 -170 -220 80 30 -70 -70 7000 1966 0 10 -200 -250 -30 70 60 -10 150 30 150 0 -2 7000 1967 100 10 -80 0 40 20 110 210 240 310 290 10 105 7000 1968 0 -70 20 -130 -100 60 70 200 40 250 -120 30 22 7000 1969 -110 -230 -130 -80 -150 60 90 90 200 230 10 70 6 7000 1970 -330 -440 -330 -100 -70 70 70 140 110 60 -10 110 -58 7000 1971 80 -160 -30 -150 -20 100 60 0 310 160 10 120 41 7000 1972 50 -20 -150 -110 -70 -40 100 170 10 260 -70 90 19 7000 1973 250 -30 -130 -180 -120 180 190 50 100 110 -10 -180 20 7000 1974 -130 -240 -140 -190 -140 0 170 -20 10 60 -30 -80 -59 7000 1975 -100 -20 -30 -190 -100 0 100 80 90 60 0 210 9 7000 1976 -110 -80 -90 -90 -110 30 180 260 100 20 40 -130 2 7000 1977 -240 -220 -160 -100 -150 180 90 110 190 0 -100 -30 -35 7000 1978 -60 -230 -130 -180 -140 290 60 30 -50 -60 220 80 -13 7000 1979 -50 -100 -290 -370 -250 -110 50 -110 -130 20 -110 50 -116 7000 1980 -170 -30 -140 -190 -150 160 40 10 90 240 80 -90 -13 7000 1981 150 150 -180 0 20 90 170 150 140 -80 50 0 54 7000 1982 -110 20 -110 -80 -390 -70 10 80 220 0 -100 -130 -56 7000 1983 -130 -30 -140 -160 -70 270 190 200 110 90 150 30 43 7000 1984 -70 -180 -100 -110 -10 180 170 100 190 30 0 160 31 7000 1985 -150 -60 50 -170 -140 -10 30 -10 50 80 160 -190 -30 7000 1986 -240 -80 -20 -210 -370 150 80 50 10 210 90 0 -27 7000 1987 20 -100 -50 -160 -40 160 280 110 170 370 150 70 83 7000 1988 90 -60 -50 10 -130 100 170 150 300 210 70 80 79 7000 1989 40 -20 -120 -160 -180 70 300 300 430 100 90 -10 70 7000 1990 0 -30 120 60 160 170 230 400 -10 280 30 90 127 7000 1991 -40 -10 -60 60 0 180 150 360 100 200 60 -10 83 7000 1992 -110 -190 -200 -220 -30 90 180 330 50 40 70 90 10 7000 1993 90 30 40 -20 10 130 260 270 20 40 20 10 76 7000 1994 28313031 - 5099999999999999999999 120 100 50 80 10 0 7099999 7000 1995 0 50 -20 -110 -20 60 -30 -200 70 120 100 150 14 7000 1996 180 210 110 110 150 210 480 -200 -370 -40 -100 -110 53 7000 1997 313031 3031 - -290 -40 80 140999999999999999 -240 -230 -70999999999999999 7000 1998 3128 303130313130313031 - 9999999999 8099999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. UST OLENEK 030435 73 00 N119 52 EK7042002 34 0 0 39 1950 -180 -170 -260 -250 -260 990 140 50 150 190 -30 -140 19 7000 1951 -80 -90 -160 0 50 1310 170 110 -10 120 -90 -40 107 7000 1952 -260 -330 -180 -190 -130 1190 100 80 120 10 -40 -100 22 7000 1953 -300 -130 -60 -100 90 630 -110 90 30 -30 -20 -30 5 7000 1954 -150 -210 -170 -280 -370 980 140 -50 110 -90 -10 60 -4 7000 1955 -20 -340 -410 -250 -300 1430 50 190 280 20 -120 -130 33 7000 1956 -300 -190 -200 -340 -210 850 -40 -120 -160 20 -160 -250 -93 7000 1957 -50 -380 -310 -210 -230 990 40 80 70 -100 -180 -170 -37 7000 1958 -310 -300 -360 -220 -280 1190 40 -40 40 20 -170 -270 -56 7000 1959 -360 -20 -160 -250 -240 960 0 -250 -300 -140 -100 40 -70 7000 1960 -350 -290 -150 -130 -150 760 30 60 -40 -130 -180 -190 -64 7000 1961 -270 -130 -340 -210 -190 940 50 -50 -70 30 30 -160 -32 7000 1962 -140 -240 -370 -260 -250 1220 170 -10 -110 40 -50 -70 -6 7000 1963 -140 -190 -150 -290 -250 1020 140 -100 20 50 -40 80 12 7000 1964 -20 -30 -70 -280 -70 1330 100 20 -240 -30 -90 210 68 7000 1965 -60 -220 -280 -250 -260 1170 70 -220 -330 20 -70 -300 -62 7000 1966 -280 -340 -320 -430 -180 1330 90 -60 130 -60 60 -100 -14 7000 1967 0 -120 -200 -100 -60 1620 80 100 120 160 200 -60 144 7000 1968 160 -30 -120 -90 -80 1450 90 120 0 130 -150 -70 116 7000 1969 -240 -340 -190 -170 -230 980 -10 30 150 120 -220 -40 -13 7000 1970 -310 -370 -380 -230 -160 910 160 60 120 -140 -20 -110 -39 7000 1971 -240 -370 -230 -270 -150 1170 0 -100 180 90 -110 -30 -5 7000 1972 -100 -150 -260 -190 -130 1110 -10 50 -110 130 -200 -10 10 7000 1973 80 -240 -300 -330 -270 1320 350 0 -20 -100 -170 -340 -2 7000 1974 -240 -340 -240 -290 -240 1460 230 -60 -120 40 -80 -80 4 7000 1975 10 -40 -130 -280 210 1050 -40 0 -50 -160 -200 -60 25 7000 1976 -220 -230 -200 -180 -250 900 120 190 20 -170 0 -220 -21 7000 1977 -300 -320 -260 -180 -20 1010 20 50 90 -260 -250 -110 -44 7000 1978 -240 -320 -250 -300 -240 910 -50 -100 -200 -210 140 -120 -82 7000 1979 -290 -330 -460 -450 -300 860 -50 -150 -200 -60 -120 -20 -131 7000 1980 -280 -140 -210 -330 -260 770 -90 30 60 150 -150 -370 -70 7000 1995 312831 - 999999999999999 -230 -250 1070 120 160 180 -60 60 9099999 7000 1996 303130313130313031 - 250 430 35099999999999999999999999999999999999999999999999999 7000 1998 3128313031 3031 - 9999999999999999999999999 890 480 230 400 190999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. DUNAI (DUNAI OSTROV) 030440 73 56 N124 30 EK7042002 50 0 0 39 1951 -40 -30 -60 20 -80 160 20 190 40 220 -50 20 35 7000 1952 -150 -190 -70 -90 -100 50 90 -10 90 20 0 -10 -30 7000 1953 -180 -10 10 -40 -140 100 -10 90 50 30 90 50 3 7000 1954 -40 -70 20 -90 -200 -30 140 70 140 -60 80 130 8 7000 1955 40 -260 -310 -160 -210 40 80 280 260 60 -100 -60 -27 7000 1956 -230 -120 -120 -260 -130 30 120 10 -90 70 -40 -120 -73 7000 1957 80 -220 -180 -70 -100 100 310 250 20 30 -30 -100 9 7000 1958 -180 -190 -240 -120 -190 200 120 20 120 90 -70 -110 -46 7000 1959 -190 140 -30 -100 -90 160 60 -230 -270 150 70 220 -10 7000 1960 -220 -150 -120 -120 -140 -30 70 130 80 -210 -140 -20 -72 7000 1961 -250 -110 -320 -90 -40 80 160 -70 10 50 -180 -270 -86 7000 1962 -170 -130 -290 -210 -160 -110 -80 -60 -50 90 10 -40 -100 7000 1963 -200 10 20 -140 0 200 240 -70 150 150 -50 160 39 7000 1964 130 90 -10 -120 70 -80 110 -50 -250 60 -120 100 -5 7000 1965 -60 -160 -140 -120 -180 10 -40 -230 -340 120 30 -140 -104 7000 1966 -90 -150 -240 -300 -30 10 80 -70 180 0 130 -20 -41 7000 1967 90 0 -100 20 -10 50 110 230 330 430 320 30 125 7000 1968 40 -100 10 -130 10 0 100 270 50 300 -40 110 53 7000 1969 -90 -190 -90 -60 -150 110 30 70 180 290 -60 160 18 7000 1970 -140 -230 -240 -100 60 230 100 50 190 -50 120 10 1 7000 1971 -130 -60 -70 -190 -40 100 20 10 300 230 0 40 18 7000 1972 -60 -160 -220 -130 -90 -30 90 150 -50 270 -100 100 -18 7000 1973 200 -120 -160 -240 -180 60 110 10 40 30 -90 -130 -38 7000 1974 -80 -280 -170 -230 -160 20 150 -40 -60 50 -10 -50 -70 7000 1975 -10 40 -40 -140 -150 -60 20 40 120 200 170 220 34 7000 1976 -100 -120 -100 -100 -120 90 160 310 190 -20 110 -120 15 7000 1977 -220 -200 -180 -70 -90 40 60 80 190 -130 -170 -110 -66 7000 1978 -140 -250 -160 -210 -120 30 -20 -140 -190 -90 200 -70 -96 7000 1979 -400 -120 -210 -160 -70 -160 -40 -200 -110 -60 -130 30 -136 7000 1980 -210 -30 -130 -240 -180 60 -60 -40 70 300 -40 -160 -55 7000 1981 90 50 -90 -20 80 80 180 160 180 -70 150 200 83 7000 1982 -60 140 100 30 10 80 170 80 230 -130 -70 60 52 7000 1983 80 -270 -270 -420 -230 -70 200 210 150 -90 -50 120 -51 7000 1984 0 10 -20 -80 80 10 -150 -50 70 -190 -150 200 -23 7000 1985 30 160 30 -80 -90 70 160 -60 40 120 310 280 80 7000 1986 60 200 270 350 630 530 240 10 -60 -70 -160 -170 152 7000 1987 -140 -240 80 -170 -170 30 60 80 180 0 -70 -50 -33 7000 1988 -10 -20 -20 -40 -60 130 150 110 120 120 60 80 52 7000 1989 -10 -20 -20 -40 -60 130 150 250 470 180 70 -100 83 7000 1990 -200 -50 170 130 220 280 180 260 -100 100 0 50 88 7000 1991 -60 -60 -90 70 50 80 120 230 260 250 -50 360 98 7000 1992 140 60 -30 -200 40 90 200 260 80 160 70 90 81 7000 1993 210 90 110 -190 -80 -20 150 -50 -80 40 100 -490 -18 7000 1994 -620 -340 -280 -270 -150 -70 90 220 270 350 260 180 -28 7000 1995 -30 -60 -280 -270 -170 60 130 260 270 110 10 100 11 7000 1996 3131303130 - 120 150 -10 -120 -20 -709999999999999999999999999 -58099999 7000 1997 -60 30 -130 -50 -180 40 50 160 340 180 70 50 41 7000 1998 -110 60 90 170 110 210 120 40 130 -60 -50 30 61 7000 1999 10 -20 -170 -10 60 300 -30 -90 460 230 440 220 116 7000 2000 190 220 -40 -150 -90 120 10 -100 310 210 -140 -130 33 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SAGYLLAH-ARY 030443 73 09 N128 53 EK7042002 19 0 0 39 1962 -160 -230 -330 -130 -100 1080 200 0 -170 -60 -120 -150 -14 7000 1963 -90 -40 -30 -180 -150 390 60 -360 -130 50 -200 20 -55 7000 1964 -100 0 -90 -270 -60 870 210 10 -230 -120 -360 -140 -24 7000 1965 -250 -340 -290 -220 -260 1280 120 -90 -210 -10 -50 -210 -44 7000 1966 -90 -140 -210 -290 90 980 90 -90 -10 -150 -30 -160 -1 7000 1967 -60 -90 -120 -90 250 990 10 40 20 140 100 -100 91 7000 1968 -60 -190 -90 -210 110 1050 60 90 -140 50 -230 -10 36 7000 1969 -170 -280 -210 -180 -220 540 110 130 230 230 -220 0 -2 7000 1970 -240 -370 -350 -200 -180 870 110 30 60 -160 -110 -140 -56 7000 1971 -250 -250 -220 -300 -40 1000 30 -40 200 80 -150 -80 -2 7000 1972 -70 -120 -160 -100 -40 980 70 80 -80 90 -210 -80 30 7000 1973 70 -150 -190 -220 30 790 150 150 0 -140 -240 -230 2 7000 1974 -80 -240 -110 -210 -90 950 410 30 -160 -150 -160 -130 6 7000 1975 0 10 -50 -140 230 970 80 -80 -20 -10 -20 60 85 7000 1976 -90 -60 -50 -110 -120 910 240 130 50 -230 -60 -110 41 7000 1977 -120 -140 -130 -30 100 740 100 -80 90 -190 -240 -110 -1 7000 1978 -20 -130 -90 -180 -100 950 290 90 -190 -190 -10 -80 28 7000 1979 -100 -60 -170 -230 -20 1070 -30 -170 -90 -140 -200 0 -13 7000 1980 -110 -20 -90 -230 -140 800 210 0 -70 220 -230 -310 2 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. TIKSI (TIKSI BUKHTA) 030447 71 35 N128 55 EK7042002313 52 0 0 39 1949 150 50 0 40 -110 150 180 320 120 10 -70 30 73 7000 1950 50 10 -230 -310 -290 70 370 170 200 180 0 -120 9 7000 1951 -120 -130 -210 -210 -80 160 40 110 -30 90 -200 -20 -49 7000 1952 -210 -280 -150 -150 -110 40 130 20 100 30 -10 -60 -53 7000 1953 -210 -100 0 -30 -160 140 60 170 60 60 130 70 16 7000 1954 -20 -30 50 -50 -160 0 180 110 130 -80 100 120 29 7000 1955 60 -210 -240 -110 -160 140 140 170 160 40 -120 -80 -16 7000 1956 -190 -90 -80 -230 -110 40 130 0 -100 50 -50 -130 -63 7000 1957 30 -230 -210 -90 -130 60 270 210 -10 0 -60 -130 -22 7000 1958 -160 -190 -230 -140 -210 170 90 -10 90 60 -70 -50 -54 7000 1959 -120 110 -40 -130 -120 140 190 -10 -110 -80 20 210 4 7000 1960 -80 -30 -80 -80 -80 50 100 30 -10 -170 -100 -110 -47 7000 1961 -190 -60 -330 -270 -40 90 120 150 -80 40 60 -90 -50 7000 1962 -100 -130 -280 -90 -80 150 150 120 -30 10 10 -80 -29 7000 1963 -160 -80 -10 -120 -50 70 180 10 -50 0 -140 100 -20 7000 1964 10 70 -10 -140 60 30 250 50 -140 -80 -160 20 -3 7000 1965 -210 -230 -200 -130 -150 60 50 -60 -410 20 90 -70 -102 7000 1966 -10 -60 -160 -180 40 180 200 -40 90 -130 140 -30 3 7000 1967 40 -10 -190 -20 -50 220 200 250 190 210 150 20 84 7000 1968 0 -100 30 -110 10 140 160 190 -20 50 -150 20 20 7000 1969 -110 -220 -120 -50 -110 170 110 40 140 240 -30 80 13 7000 1970 -300 -420 -320 -80 -40 210 80 180 160 -120 -20 -10 -55 7000 1971 -150 -220 -140 -140 0 170 70 90 140 0 -110 60 -18 7000 1972 -30 -140 -140 -80 0 100 140 210 -50 190 -90 -140 -1 7000 1973 100 -90 -130 -120 -40 150 190 130 50 50 110 -100 26 7000 1974 -60 -240 -140 -210 -170 70 230 10 -70 -120 20 -130 -66 7000 1975 -50 -70 -120 -130 -170 -30 160 180 80 10 20 120 1 7000 1976 -180 -90 -70 -170 -110 190 250 320 130 -60 60 -100 14 7000 1977 -180 -160 -180 -40 -10 130 140 90 250 -150 -130 -20 -21 7000 1978 -260 -220 -140 -160 -60 120 140 20 -110 -130 120 50 -52 7000 1979 -130 -140 -130 -250 -70 50 130 50 10 -30 -50 80 -39 7000 1980 -90 100 -30 -160 -110 240 50 60 0 140 -40 -220 -6 7000 1981 20 30 -210 -40 40 140 180 100 150 -90 80 80 40 7000 1982 -140 30 -110 -70 -30 140 220 130 220 -150 -40 10 17 7000 1983 170 110 -60 -110 20 260 280 140 220 -10 50 20 91 7000 1984 -40 -130 -30 -50 70 260 150 120 150 10 -50 -20 37 7000 1985 -380 -100 60 -340 -90 -10 0 10 -10 0 100 -160 -77 7000 1986 -370 -380 -380 -510 -260 290 110 50 -90 150 -100 -110 -132 7000 1987 -200 -230 -130 -310 -130 190 120 160 260 340 230 250 48 7000 1988 330 300 160 50 -190 110 180 180 200 90 -100 30 111 7000 1989 150 30 -50 -50 -100 270 290 170 260 80 -30 40 89 7000 1990 50 -20 70 90 130 200 300 140 -40 150 340 440 156 7000 1991 120 100 -60 50 20 140 90 180 120 80 -60 260 87 7000 1992 -150 -110 -170 -270 0 150 210 320 40 -30 -110 -20 -11 7000 1993 20 -90 30 -280 -150 90 210 -40 -50 -140 180 -50 -22 7000 1994 -330 -370 -250 -150 10 280 220 330 120 70 120 -30 4 7000 1995 -120 -20 -150 -160 -30 60 170 250 160 -120 -110 -130 -17 7000 1996 70 60 -20 -170 -20 130 230 30 -50 0 100 -70 24 7000 1997 -130 -150 -60 20 -120 120 140 230 330 100 140 -60 47 7000 1998 -260 -80 -40 -170 -130 160 200 170 80 -40 100 110 9 7000 1999 20 -140 -200 -150 -60 210 20 40 300 -50 100 90 15 7000 2000 370 10 -130 -140 30 330 290 -50 190 120 -10 -110 75 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. BYKOV MYS (BYKOV MYS) 030449 72 00 N129 07 EK7042002 13 0 0 39 1975 31283130313031 30 3031 - 99999999999999999999999999999999999 18099999 70999999999999999 7000 1976 3129313031 - 9999999999999999999999999 460 220 230 120 -80 0 -11099999 7000 1977 -140 -110 -150 -170 -160 340 80 0 110 -290 -280 -140 -76 7000 1978 31 XX 99999 -260 -180 -250 -150 540 110 -30 -210 -220 0 -200 -77 7000 1979 -130 -40 -90 -80 70 560 -200 -310 -90 -120 -160 -30 -53 7000 1980 31XX -270 -130 -170 -300 -290 360 60 -10 -120 30 -16099999 -91 7000 1991 -100 -90 -120 0 -20 660 80 140 80 10 -100 260 67 7000 1992 40 0 -70 -220 0 740 210 270 -50 -20 -80 0 68 7000 1993 90 -30 10 -240 -200 600 240 0 20 10 210 -90 51 7000 1994 -220 -140 -190 -160 -20 620 200 320 150 200 70 110 79 7000 1995 30313130313031 - -110 -80 -260 -250 -1409999999999999999999999999999999999999999 7000 1996 3129313031303131 - 9999999999999999999999999999999999999999 -30 -60 160 -11099999 7000 1998 -60 -170 -250 -40 -50 970 290 90 -130 -10 -110 -80 38 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MALYSHEVA (MALYSHEVA OSTROV) 030452 72 04 N129 50 EK7042002 26 0 0 39 1954 312831303130 313031 - 999999999999999999999999999999 120 -140 3099999999999999999999 7000 1955 312831303130 313031 - 999999999999999999999999999999 0 -40 -6099999999999999999999 7000 1957 312831303130 30313031 - 999999999999999999999999999999 0 109999999999999999999999999 7000 1958 312831303130 313031 - 999999999999999999999999999999 70 -60 -11099999999999999999999 7000 1959 312831303130 313031 - 999999999999999999999999999999 -10 -130 -6099999999999999999999 7000 1960 312931303130 313031 - 999999999999999999999999999999 -30 -160 -14099999999999999999999 7000 1961 312831303130 313031 - 999999999999999999999999999999 180 50 -22099999999999999999999 7000 1962 312831303130 313031 - 999999999999999999999999999999 120 -70 -31099999999999999999999 7000 1963 31283130313031 313031 - 99999999999999999999999999999999999 -190 -23099999999999999999999 7000 1964 31293130313031 313031 - 99999999999999999999999999999999999 -160 -40099999999999999999999 7000 1965 3128313031 3031 - 9999999999999999999999999 460 10 -220 -430 -180999999999999999 7000 1966 312831303130 313031 - 999999999999999999999999999999 70 -180 -12099999999999999999999 7000 1967 312831303130 313031 - 999999999999999999999999999999 0 70 -6099999999999999999999 7000 1968 3129313031 313031 - 9999999999999999999999999 1060 -40 -100 -25099999999999999999999 7000 1969 3128313031 3031 - 9999999999999999999999999 510 -20 -150 -140 -80999999999999999 7000 1970 312831303130 3031 - 999999999999999999999999999999 120 -160 -130 -360999999999999999 7000 1971 312831303130 3031 - 999999999999999999999999999999 -80 -130 -10 -200999999999999999 7000 1972 3129313031 3031 - 9999999999999999999999999 940 30 -30 -230 -100999999999999999 7000 1973 312831303130 3031 - 999999999999999999999999999999 -20 0 -160 -410999999999999999 7000 1974 3128313031 3031 - 9999999999999999999999999 1030 190 -80 -290 -380999999999999999 7000 1975 3128313031 3031 - 9999999999999999999999999 870 -30 -120 -90 -170999999999999999 7000 1976 3129313031 3031 - 9999999999999999999999999 770 140 -40 -70 -420999999999999999 7000 1977 3128313031 3031 - 9999999999999999999999999 630 20 -160 -50 -480999999999999999 7000 1978 3128313031 3031 - 9999999999999999999999999 1210 200 -100 -340 -350999999999999999 7000 1979 3128313031 3031 - 9999999999999999999999999 1190 -130 -240 -200 -340999999999999999 7000 1980 3129313031 313031 - 9999999999999999999999999 860 110 -140 -34099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MUOSTAH ( MUOSTAH OSTROV) 030455 71 33 N130 02 EK7042002 45 0 0 39 1951 -170 -180 -260 -260 -130 100 0 50 -40 0 -240 -70 -99 7000 1952 -210 -270 -150 -150 -120 50 130 10 100 30 0 -60 -53 7000 1953 -320 -240 -100 -140 -280 30 -50 180 170 -100 0 -80 -77 7000 1954 -10 -20 60 -30 -150 -50 200 120 150 -60 110 160 40 7000 1955 150 -120 -170 -20 -100 220 100 170 200 80 -160 -120 20 7000 1956 -240 -130 -150 -320 -160 -30 130 0 -70 -90 -160 -350 -131 7000 1957 -10 -340 -280 -160 -160 20 230 140 10 -40 -100 -180 -70 7000 1958 -160 -210 -250 -160 -270 190 130 40 120 100 -110 -60 -53 7000 1959 -120 110 -40 -140 -140 60 210 120 130 -60 0 140 22 7000 1960 -70 -40 -80 -60 -200 100 160 100 200 -120 -150 -170 -28 7000 1961 -200 -70 -360 -370 -50 -50 260 110 -100 30 50 -130 -73 7000 1962 -100 -140 -300 -80 -100 160 160 230 -10 30 0 -120 -22 7000 1963 -160 -100 0 -130 -60 50 190 10 -30 10 -190 120 -23 7000 1964 20 60 -20 -190 30 90 210 110 -190 -160 -270 10 -24 7000 1965 -220 -180 -220 -140 -200 60 30 -130 -410 100 70 -80 -109 7000 1966 -180 -230 -210 -240 -10 160 190 -100 10 -80 180 -20 -43 7000 1967 70 0 -70 30 50 330 150 130 210 250 210 -20 112 7000 1968 40 -110 0 -130 0 230 210 370 80 440 -100 60 93 7000 1969 -100 -210 -100 -80 -130 180 180 140 110 250 -20 170 34 7000 1970 -100 -70 -370 -120 -60 240 90 90 160 -170 10 30 -23 7000 1971 -170 -170 -30 -20 30 220 60 70 80 -40 -90 40 -1 7000 1972 -10 -160 -170 -80 -80 60 190 210 -50 180 -70 40 6 7000 1973 130 -90 -150 -190 -90 220 210 100 -30 -50 -90 -130 -13 7000 1974 -50 -230 -170 -190 -150 50 220 0 30 0 -80 -50 -50 7000 1975 60 20 -50 -240 -180 0 130 130 110 60 40 170 21 7000 1976 -100 -110 -90 -90 -110 190 260 370 140 -90 20 110 42 7000 1977 -220 -120 -60 -100 20 130 120 60 220 -110 10 -100 -12 7000 1978 -150 -280 -170 -180 -100 150 110 0 -150 -100 70 0 -65 7000 1979 -70 -120 -260 -240 -10 110 120 20 70 -110 -90 -50 -52 7000 1980 -260 30 -70 -300 -270 270 20 60 -10 180 50 -150 -38 7000 1981 0 0 -220 -80 0 380 160 120 220 -250 -210 -270 -14 7000 1982 -340 -100 -130 -80 -30 230 170 110 190 -240 -110 -30 -30 7000 1983 -30 -100 -180 -170 -60 210 240 120 200 -60 40 -70 12 7000 1984 -110 -300 -220 -160 50 400 140 160 150 0 -130 150 12 7000 1985 -110 -10 140 -30 -20 170 130 -40 -10 30 70 -250 5 7000 1986 -130 -130 0 -10 -10 520 130 40 -30 70 150 140 62 7000 1987 140 50 70 0 20 220 170 80 170 410 360 320 168 7000 1988 80 -310 -220 -190 -370 -110 200 230 250 0 -30 0 -38 7000 1989 0 -70 -160 -80 -70 240 180 290 410 250 120 260 115 7000 1990 430 380 510 480 590 440 140 -40 -220 30 -130 -100 208 7000 1991 -160 -170 -210 -60 -50 350 130 140 210 120 30 20 30 7000 1992 -380 -340 -290 -290 170 370 300 10 -140 80 -60 110 -37 7000 1993 150 100 150 0 -40 30 340 -170 -260 -470 70 240 12 7000 1994 250 270 390 420 570 550 210 180 140 0 0 40 251 7000 1995 31 30 - 30 30 130 160 80 -3099999 240 120 -55099999 -18099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. NAIBA 030460 70 51 N130 45 EK7042002 7 0 0 39 1979 -160 -190 -290 -370 -270 -60 60 10 -110 -110 -50 -240 -148 7000 1980 -250 -190 -300 -390 -300 70 10 -150 -160 -120 -200 -230 -184 7000 1991 -50 90 120 -30 40 140 40 140 200 170 -160 230 78 7000 1992 -150 -10 10 -30 60 20 -390 140 90 -30 -100 -30 -35 7000 1993 70 -140 130 -60 -20 120 410 300 350 320 210 160 157 7000 1994 3031 - 20 130 150 100 270 240 240 300 170 150999999999999999 7000 1995 3128 - 9999999999 -360 220 60 -60 80 250 110 110 -20 -17099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. BUORHAIA (BUORHAIA MYS) 030464 71 57 N132 46 EK7042002 23 0 0 39 1954 -80 -90 0 -110 -220 -50 130 -10 110 -140 60 110 -24 7000 1955 -10 -260 -330 -190 -240 10 70 110 210 40 -140 -150 -72 7000 1956 -270 -180 -180 -330 -210 -80 60 -30 -90 -20 -70 -210 -134 7000 1957 90 -170 -180 -40 -90 120 320 260 30 40 -30 -90 23 7000 1958 -170 -210 -250 -150 -160 170 30 -20 90 60 -50 -120 -65 7000 1959 -170 90 -80 -170 -210 90 10 -80 10 -130 50 140 -39 7000 1960 -190 -140 -150 -150 -130 0 50 40 -10 -190 -150 -190 -101 7000 1961 -280 -170 -480 -430 -210 -50 -10 -60 -190 -90 -70 -140 -182 7000 1962 -140 -220 -390 -190 -150 10 90 60 -100 40 -20 -140 -95 7000 1963 -210 -140 -80 -160 -130 -10 80 -90 -130 -70 -260 50 -95 7000 1964 -40 70 -20 -160 10 -10 220 30 -270 -80 -280 -20 -45 7000 1981 -110 -60 -300 -110 10 90 60 40 160 -170 120 180 -8 7000 1982 290 450 190 -80 140 50 40 90 80 -290 -70 -70 66 7000 1983 -60 -100 -260 -250 -120 130 150 -10 230 -70 -100 -280 -62 7000 1984 -210 -130 -120 50 10 150 50 40 90 -90 -130 50 -20 7000 1985 -210 0 210 150 150 270 100 -40 60 300 270 -330 77 7000 1986 -160 -50 90 0 -20 200 60 230 -10 360 640 490 154 7000 1987 490 440 460 480 500 580 300 110 180 240 150 130 337 7000 1988 30 -110 -110 -80 -200 30 120 270 220 60 -100 290 36 7000 1989 400 100 90 20 -40 280 350 210 350 80 20 -30 153 7000 1990 0 -30 20 30 150 150 230 240 230 160 -190 -130 73 7000 1991 3031 - -170 -120 -220 -140 -110 10 30 390 510 200999999999999999 7000 1993 3128313031 30313031 - 9999999999999999999999999 10 220 209999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. UADEI 030468 71 31 N136 25 EK7042002 33 0 0 39 1953 312831303130 - 999999999999999999999999999999 -90 -100 -20 -110 -130 -24099999 7000 1954 31 XX -290 -240 -120 -210 -280 480 210 -30 -6099999 -200 -180 -83 7000 1955 31303130 313031 - -380 -56099999999999999999999 -140 20 1099999999999999999999 7000 1956 3129313031 - 9999999999999999999999999 490 -120 -170 -290 -30 -260 -36099999 7000 1957 313031 - -200 -410 -450 -290 -320 770 220 210 -2099999999999999999999 7000 1958 312831303130 313031 - 999999999999999999999999999999 260 30 8099999999999999999999 7000 1959 31283130313031 313031 - 99999999999999999999999999999999999 210 -3099999999999999999999 7000 1960 312931303130 30313031 - 999999999999999999999999999999 80 509999999999999999999999999 7000 1961 312831303130 30313031 - 999999999999999999999999999999 90 2509999999999999999999999999 7000 1962 31283130313031 30313031 - 99999999999999999999999999999999999 609999999999999999999999999 7000 1963 31283130313031 313031 - 99999999999999999999999999999999999 -260 -34099999999999999999999 7000 1964 312931303130 30313031 - 999999999999999999999999999999 50 -709999999999999999999999999 7000 1965 312831303130 3031 - 999999999999999999999999999999 -140 -430 -530 -160999999999999999 7000 1966 312831303130 313031 - 999999999999999999999999999999 -50 -80 -3099999999999999999999 7000 1967 312831303130 313031 - 999999999999999999999999999999 -10 70 099999999999999999999 7000 1968 3129313031 3031 - 9999999999999999999999999 800 470 500 230 220999999999999999 7000 1969 3128313031 313031 - 9999999999999999999999999 570 70 10 -6099999999999999999999 7000 1970 3128313031 313031 - 9999999999999999999999999 990 40 -20 -9099999999999999999999 7000 1971 3128313031 313031 - 9999999999999999999999999 600 -170 -90 -9099999999999999999999 7000 1972 3129313031 3031 - 9999999999999999999999999 460 170 70 -350 50999999999999999 7000 1973 3128313031 3031 - 9999999999999999999999999 510 10 -10 -60 -130999999999999999 7000 1974 3128313031 3031 - 9999999999999999999999999 580 60 -170 -360 -360999999999999999 7000 1975 3128313031 3031 - 9999999999999999999999999 620 -90 -100 -280 -140999999999999999 7000 1976 3129313031 3031 - 9999999999999999999999999 600 280 170 70 -390999999999999999 7000 1977 3128313031 3031 - 9999999999999999999999999 290 200 -40 40 -610999999999999999 7000 1978 3128313031 313031 - 9999999999999999999999999 760 180 -200 -50099999999999999999999 7000 1979 3128313031 3031 - 9999999999999999999999999 620 -120 -290 -390 -500999999999999999 7000 1980 3129313031 313031 - 9999999999999999999999999 270 -130 -100 -28099999999999999999999 7000 1988 312931303130 31 - 999999999999999999999999999999 40 310 170 -260 -5709999999999 7000 1989 3128313031 3031 - 9999999999999999999999999 120 240 80 240 -130999999999999999 7000 1990 3128313031 313031 - 9999999999999999999999999 120 290 30 -31099999999999999999999 7000 1991 3128313031 313031 - 9999999999999999999999999 780 90 -70 1099999999999999999999 7000 1994 312831303130 313031 - 999999999999999999999999999999 -160 100 -12099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KOTELNYI (KOTELNYI OSTROV) 030475 76 00 N137 52 EK7042002 50 0 0 39 1951 -140 -180 -340 -260 -160 40 -100 90 -140 30 -200 -20 -114 7000 1952 -350 -530 -390 -270 -250 -120 0 -140 60 -110 -160 -210 -205 7000 1953 -320 -180 -260 -340 -260 110 20 170 230 20 100 30 -57 7000 1954 80 100 120 -70 -180 120 170 50 180 -90 110 40 52 7000 1955 30 -280 -300 -80 -220 -220 -130 90 -40 -10 -180 -140 -122 7000 1956 -230 -110 -230 -380 -290 -90 50 -110 -20 -40 -120 -160 -144 7000 1957 40 -240 -300 -120 -210 -50 0 50 -70 -80 -130 -160 -105 7000 1958 -150 -110 -330 -280 -320 -30 -40 90 10 -10 -250 -90 -126 7000 1959 -320 -40 -230 -180 -310 -60 -130 -180 -70 20 160 290 -88 7000 1960 -120 30 -10 50 -100 -40 140 150 140 110 -70 20 25 7000 1961 -180 20 -280 -360 -90 -40 -40 -100 20 160 220 -100 -65 7000 1962 -80 -140 -350 -120 -260 -40 70 -30 -80 40 90 -160 -88 7000 1963 -170 -170 -50 -180 -160 -30 80 -90 120 130 0 220 -24 7000 1964 120 170 0 -200 70 -20 210 30 -70 30 -170 170 29 7000 1965 -120 -270 -130 -60 -180 -130 -120 -80 -80 150 0 -110 -93 7000 1966 -80 -190 -240 -270 -100 100 120 -40 110 -40 30 -40 -53 7000 1967 40 -30 -180 -50 -100 0 130 160 210 170 110 70 45 7000 1968 110 -180 -80 -210 -100 20 20 80 30 230 -10 150 7 7000 1969 -150 -260 -160 -100 -220 40 -40 60 120 120 -140 50 -55 7000 1970 -80 -270 -210 -180 -110 150 40 60 140 -160 130 90 -32 7000 1971 0 -50 -90 -220 -50 60 -120 70 250 140 80 80 13 7000 1972 -40 -140 -220 -110 -140 -20 140 120 40 350 -100 120 1 7000 1973 180 -160 -200 -380 -180 70 280 180 90 180 -10 -110 -3 7000 1974 10 -130 -30 -280 -190 40 150 40 50 40 30 70 -15 7000 1975 70 40 -80 -160 -170 -130 100 180 340 360 150 270 82 7000 1976 -130 -70 -80 -180 -190 130 120 240 260 20 140 -130 10 7000 1977 -250 -210 -230 -30 -60 30 -40 20 250 50 -60 50 -40 7000 1978 110 -170 -120 -400 -80 20 -60 60 10 100 350 170 1 7000 1979 0 -110 -370 -270 -160 -70 -70 -80 -70 -30 0 130 -91 7000 1980 -210 -30 -80 -290 -320 160 -110 10 70 220 -70 -140 -66 7000 1981 130 80 -260 -110 40 60 130 90 130 0 260 170 60 7000 1982 -60 40 -140 -80 -50 100 200 60 220 -30 90 70 34 7000 1983 300 130 -20 0 110 310 310 350 100 10 300 380 191 7000 1984 220 210 -60 -90 110 200 -30 40 100 -10 70 230 82 7000 1985 70 30 280 0 30 60 50 40 50 90 130 -240 49 7000 1986 -200 -100 10 -100 -170 210 -180 -120 -110 20 -100 90 -63 7000 1987 10 -120 10 -170 -10 60 120 100 150 440 90 -70 52 7000 1988 80 -10 -20 -120 -280 50 160 200 270 240 40 280 75 7000 1989 250 130 -10 -60 -180 220 300 220 340 280 140 40 139 7000 1990 10 -20 100 140 150 120 100 110 70 100 50 160 92 7000 1991 30 -40 -160 -100 -90 90 70 290 220 200 90 310 77 7000 1992 10 -80 -110 -280 70 210 70 260 290 310 170 320 104 7000 1993 280 130 210 -120 -270 -100 70 -300 -320 -330 310 190 -22 7000 1994 60 210 390 460 610 340 310 450 390 540 370 200 362 7000 1995 -120 -140 -230 -270 -110 -30 -80 90 280 60 40 70 -36 7000 1996 340 150 100 -160 -10 90 160 10 -120 70 10 -10 53 7000 1997 220 50 -60 70 -240 40 50 240 370 310 270 -50 105 7000 1998 -200 -30 -80 -100 -20 230 130 120 110 70 -50 90 23 7000 1999 10 -160 -210 -110 -20 250 100 130 420 190 320 100 86 7000 2000 312931 - 999999999999999 -110 80 290 160 110 240 200 20 -35099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SANNIKOVA (SANNIKOVA PROLIV) 030480 74 40 N138 54 EK7042002 51 0 0 39 1950 170 140 -20 -220 -210 240 110 120 150 280 50 -150 54 7000 1951 -60 -90 -240 -130 -40 230 50 270 50 200 -110 50 16 7000 1952 -160 -300 -180 -200 -190 -160 220 110 20 -30 200 -80 -62 7000 1953 -200 210 50 0 -230 100 60 140 110 80 210 170 57 7000 1954 170 100 240 30 -140 -70 300 230 260 230 240 310 159 7000 1955 40 -270 -320 -130 -260 20 70 290 210 130 -60 -50 -26 7000 1956 -120 0 -130 -180 -120 50 180 -50 20 70 -10 -120 -34 7000 1957 0 -170 -220 -90 -220 -30 140 10 -70 -40 -100 -220 -84 7000 1958 -220 -200 -260 -170 -260 70 10 80 300 0 -230 -230 -93 7000 1959 -330 -10 -110 -290 -290 -100 120 160 90 190 130 200 -20 7000 1960 -150 -120 -60 -110 -70 50 180 10 -40 -50 -50 20 -32 7000 1961 -170 -50 -360 -390 -110 -10 40 50 90 160 110 -180 -69 7000 1962 -220 -270 -450 -190 -170 160 180 270 -40 110 40 -70 -53 7000 1963 -190 -150 -10 -150 10 30 110 -20 20 110 60 330 14 7000 1964 140 160 70 -60 90 20 140 40 -50 0 80 140 64 7000 1965 -140 -330 -40 -60 -120 -60 -30 -50 -210 150 180 20 -55 7000 1966 10 -290 -200 -260 30 140 60 -30 100 -10 100 10 -27 7000 1967 70 -30 -110 50 50 110 170 90 140 230 210 -20 80 7000 1968 20 -130 -30 -160 -40 80 110 30 70 90 -150 200 9 7000 1969 0 -150 -60 -30 -110 130 60 30 170 160 -130 160 20 7000 1970 -20 -350 -300 -140 -110 200 90 80 130 -40 130 60 -21 7000 1971 -310 -150 -110 -240 -80 70 -40 40 180 130 0 50 -38 7000 1972 0 -240 -200 -130 -90 60 130 60 -40 260 -130 190 -9 7000 1973 170 -60 -170 -310 -150 130 160 170 160 90 -60 -80 5 7000 1974 60 -290 -70 -260 -180 170 130 -40 -50 -50 -20 120 -38 7000 1975 150 70 -70 -140 -90 90 90 130 150 240 260 340 102 7000 1976 170 -50 -60 -90 -150 160 70 180 280 -30 100 -110 39 7000 1977 -210 -180 -200 -40 -50 0 -60 -10 240 -30 -140 -30 -59 7000 1978 -50 -210 -170 -250 -130 50 30 70 -50 -20 200 50 -39 7000 1979 -120 -210 -400 -260 -180 -60 -60 -50 -50 -60 -160 -120 -144 7000 1980 -400 -80 -120 -310 -350 100 -50 70 50 100 -200 -350 -129 7000 1981 -80 -100 -330 -140 0 220 140 90 190 170 170 200 45 7000 1982 -30 70 -70 -110 -110 -20 70 -10 130 -130 -110 -60 -33 7000 1983 -140 -60 -180 -190 -80 320 190 210 120 0 20 80 24 7000 1984 -50 -140 -100 -100 40 160 30 130 130 20 -80 140 16 7000 1985 -120 -30 110 -200 -160 90 0 0 90 90 70 -230 -25 7000 1986 -250 -180 -80 -170 -230 200 110 100 40 190 70 -30 -18 7000 1987 40 -170 190 -220 -90 100 230 200 260 340 90 -80 76 7000 1988 0 -120 -60 -130 -290 0 160 140 300 160 0 200 31 7000 1989 290 80 -50 -30 -160 260 260 160 350 140 40 -30 109 7000 1990 -10 -40 80 80 140 400 170 130 130 110 10 20 102 7000 1991 50 190 -40 90 50 130 30 230 190 150 10 380 121 7000 1992 180 170 100 -50 260 270 130 -100 -230 40 20 100 74 7000 1993 240 30 110 -180 -160 120 220 -60 -130 -140 230 -60 18 7000 1994 -170 -20 -90 -120 -20 280 100 260 310 260 160 350 109 7000 1995 -60 -20 -190 -200 -90 -30 50 120 220 -40 -160 -100 -42 7000 1996 -80 -100 -140 -230 -30 120 200 -50 -80 -20 -20 -60 -40 7000 1997 60 0 -70 140 -90 140 180 380 480 360 200 30 151 7000 1998 -140 -20 -40 -80 -40 -80 0 -10 40 -110 10 20 -38 7000 1999 130 60 20 10 -30 -30 -10 190 250 190 80 20 73 7000 2000 -130 70 -120 -130 -150 -20 -200 -130 30 -110 -110 -310 -111 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KIGILIAH 030485 73 20 N139 52 EK7042002 50 0 0 39 1951 20 -20 -200 -140 -10 190 90 220 90 270 50 240 68 7000 1952 -50 -140 -30 10 0 70 110 -20 20 190 110 0 23 7000 1953 -90 60 70 80 -160 160 50 120 110 120 190 130 69 7000 1954 20 -20 60 10 -100 60 260 340 180 140 240 230 119 7000 1955 100 -190 -150 30 -90 170 130 330 270 310 0 0 78 7000 1956 -80 30 30 -140 -30 100 140 -30 -40 210 0 -150 3 7000 1957 -10 -180 -290 -190 -190 -40 100 220 50 60 20 -50 -41 7000 1958 -100 -180 -200 -120 -200 150 40 20 170 190 -40 -80 -29 7000 1959 -260 150 -40 -130 -70 -10 210 40 -90 130 40 210 15 7000 1960 -150 -120 -90 -150 -50 10 70 -10 -50 -50 -100 -100 -65 7000 1961 -240 -130 -370 -230 50 90 30 -80 250 150 320 -100 -22 7000 1962 -130 -200 -370 -170 -200 20 50 70 -80 60 30 -120 -86 7000 1963 -180 -120 0 -90 -70 110 170 -50 80 150 -60 180 11 7000 1964 100 180 70 -140 -90 -80 170 20 -130 10 -160 110 5 7000 1965 -90 -200 -130 -30 -70 80 -60 -160 -460 200 100 -100 -76 7000 1966 -70 -120 -240 -300 -50 160 50 -150 80 -10 240 60 -29 7000 1967 120 20 0 60 30 290 130 140 180 420 210 10 135 7000 1968 50 -120 -20 -160 -30 70 120 130 20 250 -90 110 29 7000 1969 -70 -190 -90 -50 -130 130 40 70 80 280 -100 90 6 7000 1970 -210 -300 -240 -150 -50 190 -10 10 130 -190 -50 -30 -74 7000 1971 -190 -170 -140 -220 -60 70 -60 10 160 10 -50 70 -47 7000 1972 -10 -150 -190 -110 -40 70 150 190 -40 360 -40 90 25 7000 1973 210 -90 -180 -190 -70 160 170 90 50 120 -240 -230 -16 7000 1974 20 -190 -90 -200 -140 30 180 -10 -100 -50 70 20 -37 7000 1975 50 50 -50 -110 -150 -100 70 140 130 190 310 240 64 7000 1976 -40 -40 -40 -100 -120 150 150 310 180 -40 130 -90 37 7000 1977 -180 -160 -170 -40 -20 70 10 -30 130 -200 -130 -70 -66 7000 1978 -80 -250 -170 -260 -140 10 -10 -80 -240 -120 230 60 -86 7000 1979 -110 -180 -340 -300 -160 20 50 -100 -100 -100 -40 80 -106 7000 1980 -180 -30 -80 -250 -250 120 -90 30 -60 280 -90 -260 -72 7000 1981 0 20 -280 -110 50 170 90 30 150 -130 190 170 28 7000 1982 -80 -10 -110 -50 -20 100 110 80 180 -190 -50 20 -2 7000 1983 50 10 -140 -140 -60 100 190 120 150 -20 -60 -20 15 7000 1984 -60 -200 -130 -130 40 220 60 80 150 -10 -110 100 2 7000 1985 -200 -100 40 -160 -140 20 0 -120 80 100 100 -160 -45 7000 1986 -170 -100 10 -80 -110 250 40 -30 -110 200 -80 -170 -29 7000 1987 -50 -120 -40 -210 -90 110 110 50 140 220 -40 -40 4 7000 1988 0 -80 -100 -110 -280 -80 150 170 290 240 -60 140 24 7000 1989 240 130 -20 -30 -130 210 250 140 310 160 0 40 108 7000 1990 90 30 130 130 200 210 160 60 -40 80 70 30 96 7000 1991 -60 -70 -90 30 -20 60 50 140 140 140 20 370 60 7000 1992 160 130 30 -70 190 180 150 280 20 120 -90 -20 91 7000 1993 160 50 140 -170 -100 130 230 20 -110 0 -10 -160 15 7000 1994 -140 -30 -80 -170 -90 160 90 340 230 280 100 280 82 7000 1995 -70 -30 -180 -210 -110 -100 -150 240 230 60 -100 20 -33 7000 1996 90 120 80 -130 10 100 210 -40 40 100 -30 -20 44 7000 1997 90 -20 -90 80 -140 -20 -10 160 130 170 30 10 33 7000 1998 -130 -30 -30 -80 -50 0 50 120 0 -90 -100 0 -28 7000 1999 3031 - 50 -90 -200 -170 -90 -130 -120 -70 260 50999999999999999 7000 2000 -20 -130 -180 -180 -30 20 0 -170 170 70 -100 -190 -62 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ZEMLIA BUNGE 030510 74 53 N142 07 EK7042002 37 0 0 39 1951 -80 -130 -240 -120 -50 180 60 110 40 150 -100 50 -10 7000 1952 -160 -370 -180 -200 -170 -80 220 60 30 -30 0 -90 -79 7000 1953 -190 -20 40 10 -200 90 70 70 70 60 200 100 25 7000 1954 10 60 40 -60 -170 -50 230 130 150 -70 120 250 53 7000 1955 -100 -350 -390 -180 -300 40 40 130 150 70 -120 -30 -85 7000 1956 -90 20 0 -190 -120 20 170 -60 10 60 -20 -90 -24 7000 1957 20 -50 -190 -100 -230 50 120 30 -50 -20 -80 -200 -59 7000 1958 -260 -230 -220 -160 -230 70 10 20 190 -110 -190 -170 -107 7000 1959 -240 120 -40 -180 -130 170 180 -10 -50 80 180 340 34 7000 1960 20 -50 50 -20 -30 60 110 100 140 -10 -70 -40 22 7000 1961 -240 -140 -360 -510 -170 -100 50 30 40 100 160 -200 -112 7000 1962 -240 -290 -420 -140 -230 60 150 70 -70 50 100 -70 -85 7000 1963 -150 -110 -10 -130 -120 -10 210 -10 10 50 0 220 -3 7000 1964 130 190 40 -140 50 0 170 90 -30 10 -140 20 33 7000 1965 -150 -300 -170 -30 -120 -90 -30 -20 30 90 110 -40 -59 7000 1966 -40 -80 -180 -250 30 170 50 -60 80 -10 110 10 -14 7000 1967 60 -30 -120 30 90 100 220 110 140 280 210 0 92 7000 1968 30 -130 -40 -190 -50 -30 80 60 0 70 -80 130 -11 7000 1969 -40 -180 -50 10 -10 270 90 70 120 170 -100 20 32 7000 1970 -250 -340 -280 -140 -110 240 80 110 100 -10 120 60 -34 7000 1971 -110 -70 -80 -170 -40 90 20 70 190 140 20 100 14 7000 1972 0 -130 -140 -90 -50 70 180 120 0 320 -90 90 25 7000 1973 160 -50 -130 -260 -80 130 170 140 90 30 -190 -60 -3 7000 1974 30 -190 -60 -280 -210 90 210 -20 -40 -10 40 100 -27 7000 1975 220 110 -30 -110 -120 -70 180 190 230 190 210 260 105 7000 1976 -30 -40 -50 -100 -140 120 170 250 260 10 120 -60 42 7000 1977 -160 -130 -130 20 -20 30 -10 70 270 -20 -40 40 -6 7000 1978 0 -160 -100 -190 -60 40 40 80 50 60 230 130 11 7000 1979 -30 -90 -300 -240 -150 -40 50 -40 -60 -50 -30 90 -74 7000 1980 -170 -20 -50 -220 -250 160 -40 110 120 160 -70 -210 -41 7000 1981 40 30 -280 -120 20 100 170 170 110 -70 180 140 41 7000 1982 -30 20 -100 -70 -70 60 160 80 220 -30 0 130 31 7000 1983 120 70 -90 -100 10 310 260 230 170 50 50 40 93 7000 1984 110 10 -70 -130 40 140 80 150 160 70 -30 100 53 7000 1985 -90 0 120 -160 -110 70 20 20 110 120 120 -140 6 7000 1986 -130 -40 60 -40 -90 320 110 80 40 240 160 270 82 7000 1987 190 -60 0 -130 -10 140 200 160 200 300 270 280 130 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. SHALAUROVA (SHALAUROVA MYS) 030516 73 11 N143 14 EK7042002 50 0 0 39 1950 70 20 -100 -180 -160 180 40 60 150 230 50 -150 17 7000 1951 -40 -80 -260 -200 -70 120 40 150 120 200 -10 120 8 7000 1952 -110 -190 -70 -60 -40 -10 120 -10 120 70 30 -40 -15 7000 1953 -170 -100 10 -10 -220 170 80 170 130 100 220 80 38 7000 1954 0 0 10 0 -70 80 230 230 200 -10 170 190 86 7000 1955 60 -170 -140 10 -90 110 80 250 260 160 -80 -10 38 7000 1956 -40 20 10 -120 -40 -10 30 -90 -70 160 70 -80 -13 7000 1957 10 -70 -180 0 -140 70 240 280 30 60 -20 -100 16 7000 1958 -120 -80 -210 -110 -180 130 70 0 220 300 -10 -80 -6 7000 1959 -160 160 10 -70 -100 140 150 -50 -200 180 0 140 16 7000 1960 -180 -120 -90 -140 -150 0 30 -40 -50 -70 -90 -60 -80 7000 1961 -210 -100 -310 -350 -130 30 0 -30 -120 60 270 -50 -79 7000 1962 -30 -140 -310 -100 -190 100 110 70 -20 40 30 -190 -52 7000 1963 -260 -220 -80 -110 -120 70 130 -40 20 100 -80 130 -37 7000 1964 40 120 0 -130 70 20 140 -20 -250 130 60 80 22 7000 1965 -170 -280 -220 -90 -170 -30 90 120 -360 170 120 -90 -74 7000 1966 -90 -110 -250 -320 -70 30 40 -130 70 10 160 30 -52 7000 1967 70 0 -10 120 30 250 260 260 110 470 300 80 163 7000 1968 40 -140 -40 -180 -80 90 160 180 0 140 -90 100 17 7000 1969 -80 -200 -180 -80 -90 150 70 120 50 320 -110 20 1 7000 1970 -170 -270 -250 -100 -80 160 50 80 180 -170 130 20 -34 7000 1971 -150 -120 -110 -180 0 140 0 120 240 160 0 70 15 7000 1972 -30 -150 -180 -120 -30 70 150 270 0 370 -60 40 29 7000 1973 150 -120 -190 -220 -90 110 230 300 70 150 0 -30 32 7000 1974 20 -170 -80 -250 -180 60 110 0 -20 -50 30 -10 -44 7000 1975 30 10 -90 -150 -170 -190 70 140 100 80 230 210 23 7000 1976 -50 -70 -60 -120 -140 60 130 380 190 -100 110 -100 19 7000 1977 -170 -180 -160 -20 -20 40 -20 -30 140 -130 -140 -70 -63 7000 1978 -100 -240 -190 -270 -130 10 -270 -50 -190 -70 240 140 -93 7000 1979 100 40 -100 -10 100 190 110 -60 -80 -50 -50 10 17 7000 1980 -230 -130 -220 -270 -280 30 -10 180 20 350 -80 -270 -76 7000 1981 -20 -10 -210 -60 -40 130 140 40 90 -210 140 130 9 7000 1982 -50 0 -110 -90 -70 40 90 90 140 -200 -80 -30 -23 7000 1983 -50 -20 -180 -180 -70 200 210 100 210 0 0 -10 17 7000 1984 20 -150 -110 -140 0 170 50 90 130 0 -50 -40 -2 7000 1985 -150 -40 60 -200 -150 0 20 -100 110 120 100 -140 -31 7000 1986 -140 -70 30 -100 -120 250 70 70 0 320 20 0 28 7000 1987 40 -160 -100 -220 -100 0 100 70 330 330 30 30 31 7000 1988 50 -60 -60 -80 -240 30 190 150 460 250 0 120 68 7000 1989 240 110 -70 0 -150 260 390 160 290 210 120 10 131 7000 1990 50 -10 70 80 50 60 170 60 120 180 30 -60 67 7000 1992 90 60 -30 -170 90 150 260 330 70 80 10 70 85 7000 1993 190 0 70 -180 -140 110 260 0 -30 -130 180 -160 14 7000 1994 -210 -140 -160 -190 -80 140 20 270 260 90 280 270 47 7000 1995 -10 0 -140 -150 -70 0 70 220 170 -30 -90 30 0 7000 1996 10 -30 -30 -270 -110 0 220 350 40 140 30 -120 20 7000 1997 31 XX -80 -20 -120 0 -220 2099999 130 380 200 170 -20 39 7000 1998 -180 -50 -20 -50 -40 130 60 140 -60 -120 -360 -190 -62 7000 1999 10 -100 30 0 10 90 30 70 70 -80 40 -60 10 7000 2000 2931303130 313031 - 09999999999999999999999999 -60 -200 -3099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. NEMKOVA (NEMKOVA OSTROV) 030521 71 25 N150 45 EK7042002 22 0 0 39 1956 31293130313031 313031 - 99999999999999999999999999999999999 -300 -31099999999999999999999 7000 1957 31283130 30 313031 - 99999999999999999999 14099999 -30 190 -33099999999999999999999 7000 1958 312831303130 313031 - 999999999999999999999999999999 90 -200 -18099999999999999999999 7000 1959 31283130313031 313031 - 99999999999999999999999999999999999 150 -13099999999999999999999 7000 1960 312931303130 313031 - 999999999999999999999999999999 0 -70 -24099999999999999999999 7000 1964 312931303130 313031 - 999999999999999999999999999999 0 -210 -33099999999999999999999 7000 1965 3128313031 313031 - 9999999999999999999999999 580 10 -400 -71099999999999999999999 7000 1966 3128313031 313031 - 9999999999999999999999999 610 -50 -120 -16099999999999999999999 7000 1967 312831303130 313031 - 999999999999999999999999999999 290 160 -24099999999999999999999 7000 1968 312931303130 313031 - 999999999999999999999999999999 70 10 -17099999999999999999999 7000 1969 31283130 313031 - 99999999999999999999 -30 390 90 -100 -21099999999999999999999 7000 1970 3128313031 31 - 9999999999999999999999999 110 -30 -210 -110 -650 -4209999999999 7000 1971 3128313031 3031 - 9999999999999999999999999 410 -150 -180 -160 -300999999999999999 7000 1972 3129313031 3031 - 9999999999999999999999999 320 -110 20 -410 -140999999999999999 7000 1973 3128313031 3031 - 9999999999999999999999999 310 30 -200 -250 -220999999999999999 7000 1974 31283130 3031 - 99999999999999999999 -290 460 100 -40 -350 -600999999999999999 7000 1975 3128313031 3031 - 9999999999999999999999999 480 -30 -90 -110 -420999999999999999 7000 1976 31293130 3031 - 99999999999999999999 -610 280 40 -80 -30 -540999999999999999 7000 1977 31283130 3031 - 99999999999999999999 -300 270 -110 0 -30 -560999999999999999 7000 1978 3128313031 3031 - 9999999999999999999999999 570 140 0 -540 -630999999999999999 7000 1979 31283130 3031 - 99999999999999999999 -520 500 -110 -170 -430 -420999999999999999 7000 1980 3129313031 313031 - 9999999999999999999999999 180 -50 -30 -40099999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. ZHOHOVA (ZHOHOVA OSTROV) 030528 76 09 N152 50 EK7042002 34 0 0 39 1959 -310 130 10 -170 -120 160 200 80 -40 130 150 400 51 7000 1960 100 -30 60 -60 -10 -20 30 20 0 10 -10 10 9 7000 1961 -170 20 -310 -330 30 90 80 -40 -60 0 140 80 -40 7000 1962 10 -110 -230 -130 -170 80 110 10 20 140 130 -110 -21 7000 1963 -140 -100 0 -70 -40 60 130 40 20 130 -20 110 11 7000 1964 40 60 -40 -80 40 20 160 0 -80 60 -60 60 15 7000 1965 -120 -280 -180 120 -90 -70 50 10 -200 -120 130 70 -55 7000 1966 50 -80 -200 -230 0 80 70 -60 40 -60 -20 30 -31 7000 1967 20 -60 -200 -60 0 10 230 170 120 130 200 -40 44 7000 1968 40 -160 0 -200 -60 50 210 70 30 130 -120 90 8 7000 1969 110 -90 -70 -60 -110 90 150 70 120 150 -100 10 24 7000 1970 -210 -290 -280 -150 -100 170 140 130 130 -40 50 40 -33 7000 1971 -60 -50 -140 -200 -40 60 110 100 110 70 40 50 5 7000 1972 -90 -160 -130 -160 -110 10 90 100 0 190 -100 -90 -37 7000 1973 20 -210 -190 -340 -190 -10 180 130 -70 -120 -190 -380 -113 7000 1974 -180 -180 -50 -120 -150 60 130 10 -40 -50 20 50 -41 7000 1975 10 0 -150 -160 -220 -160 150 170 150 70 60 180 9 7000 1976 20 30 -10 -120 -140 -20 0 240 100 -30 -120 -460 -43 7000 1977 -360 -220 -200 -60 -20 30 -30 40 170 -30 -80 20 -61 7000 1978 -50 -180 -130 -240 -120 -60 20 90 -30 -40 150 50 -44 7000 1979 -60 -140 -380 -270 -210 60 -60 -10 -30 70 120 190 -60 7000 1980 0 180 -10 -170 -340 -30 -60 180 90 50 -100 -190 -34 7000 1981 50 20 -270 -140 -30 20 140 110 40 -100 190 230 22 7000 1982 -50 130 -10 -80 -40 50 150 110 170 -80 -60 -40 20 7000 1983 10 -30 -170 -190 -60 280 190 250 160 70 30 10 46 7000 1984 60 -80 -140 -120 50 140 170 220 140 20 -70 170 48 7000 1985 -60 -30 100 -180 -130 380 210 110 130 90 50 -160 43 7000 1986 -160 -30 40 -60 -120 260 270 140 70 210 -30 20 51 7000 1987 60 -110 -90 -160 -40 -50 110 150 190 220 10 -10 25 7000 1988 0 -10 -60 -110 -190 50 180 250 220 120 -30 190 51 7000 1989 350 130 -30 -10 -70 260 330 170 190 40 140 -160 111 7000 1990 -180 -170 -90 40 170 80 90 80 170 100 110 -80 27 7000 1992 10 10 -30 -230 100 20 250 140 150 290 110 250 90 7000 1993 30313031 - -20 70 110 190 210 100 10 2309999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. AMBARCHIK 030535 69 37 N162 18 EK7042002 51 0 0 39 1950 0 -60 -90 -70 -130 390 150 190 170 210 -60 -170 44 7000 1951 -110 -120 -320 -200 -160 250 30 250 50 150 20 140 -1 7000 1952 -50 -70 -100 -60 -10 150 140 -160 -10 0 0 -140 -26 7000 1953 -260 -180 -160 -200 -330 190 80 50 60 -120 300 0 -48 7000 1954 -60 -40 -130 -140 40 220 250 270 160 70 100 200 79 7000 1955 -30 -280 -260 -160 -220 260 -30 150 120 -110 -200 -100 -71 7000 1956 -100 40 -90 -150 -40 280 200 -50 -70 150 60 -40 16 7000 1957 -140 -280 -240 -90 -170 220 180 450 -100 -110 -80 -120 -38 7000 1958 -80 -260 -250 -230 -230 140 110 -30 240 330 50 -110 -26 7000 1959 -130 150 -50 -140 -10 290 180 -190 -200 60 -130 110 -6 7000 1960 -170 -230 -120 -150 -80 190 -100 -230 -190 -130 -170 -40 -118 7000 1961 -200 -190 -300 -390 -150 50 10 -110 -180 -50 160 -120 -122 7000 1962 -160 -190 -340 -270 -220 320 200 20 40 -60 110 -150 -58 7000 1963 -190 -260 -130 -160 -140 240 190 110 -60 120 -50 120 -16 7000 1964 20 30 -70 -150 0 140 280 -120 -60 -30 -200 -140 -25 7000 1965 -230 -280 -260 -180 -150 130 0 -130 -450 40 50 -120 -131 7000 1966 -100 -130 -240 -280 -40 280 30 -210 -80 -120 -300 -110 -108 7000 1967 -140 -190 -200 -170 230 140 280 250 -20 360 60 0 52 7000 1968 -60 -250 -70 -160 -60 220 70 110 160 80 -260 0 -17 7000 1969 -120 -180 -180 -110 -90 210 110 110 0 -600 -110 10 -79 7000 1970 -310 -240 -200 -160 -140 300 130 -10 160 -220 60 30 -50 7000 1971 -210 -120 -220 -230 -170 210 80 -20 0 100 -100 -30 -59 7000 1972 -40 -210 -200 -250 -110 270 -50 190 0 290 -20 20 -8 7000 1973 20 -140 -200 -260 -130 230 290 170 80 0 -90 -150 -14 7000 1974 0 -240 -170 -280 -210 310 160 10 -140 -320 -70 -210 -96 7000 1975 -90 -100 -180 -210 -210 250 200 130 200 60 200 20 23 7000 1976 -90 -100 -90 -150 -190 330 180 270 150 -120 40 -170 5 7000 1977 -170 -170 -210 -150 -110 210 -80 20 160 -40 -150 -60 -62 7000 1978 -50 -300 -240 -280 -190 240 130 -20 -180 -230 -20 -10 -95 7000 1979 -130 -250 -340 -330 -270 160 140 50 20 -100 -20 -100 -97 7000 1980 -170 -90 -80 -220 -230 330 40 160 -110 280 -60 -170 -26 7000 1981 0 -40 -280 -160 30 230 230 100 -20 -210 200 110 16 7000 1982 -190 -130 -140 -130 -40 380 90 80 10 -320 -220 -160 -64 7000 1983 -180 -170 -320 -270 -150 400 170 230 340 20 10 -150 -6 7000 1984 -120 -190 -130 -170 40 230 200 100 100 -10 -70 -100 -9 7000 1985 -30 70 110 -190 -70 320 110 -60 70 70 30 -60 30 7000 1986 -140 -90 -60 -130 -130 380 240 250 90 310 -10 180 75 7000 1987 190 -90 -40 -120 -20 220 80 70 420 320 50 90 99 7000 1988 200 80 20 -90 -80 410 180 360 410 170 -70 10 133 7000 1989 50 80 -170 -40 -20 460 440 320 260 460 100 100 170 7000 1990 150 110 220 230 150 180 -160 -150 200 170 -120 -160 67 7000 1991 20 -10 -30 -40 20 270 120 110 110 230 -10 390 99 7000 1992 50 60 -30 -120 150 370 200 480 140 -80 80 30 111 7000 1993 90 40 20 -70 80 280 320 200 0 -40 110 130 97 7000 1994 190 410 350 -180 -40 710 260 460 240 180 280 490 278 7000 1995 110 -40 -60 -60 140 280 10 180 60 -180 -240 10 18 7000 1996 312931303130 31 - 999999999999999999999999999999 420 -40 50 20 3609999999999 7000 1997 312831303130 3031 - 999999999999999999999999999999 50 60 330 10999999999999999 7000 1998 312831303130 3031 - 999999999999999999999999999999 210 450 60 160999999999999999 7000 1999 312831303130 313031 - 999999999999999999999999999999 180 30 37099999999999999999999 7000 2000 312931303130 3031 - 999999999999999999999999999999 130 -80 280 230999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. CHETYREHSTOLBOVOI 030550 70 38 N162 29 EK7042002 44 0 0 39 1951 80 100 -40 -190 -160 40 100 310 240 320 70 190 89 7000 1952 0 -20 40 10 10 10 200 -70 60 20 40 -120 15 7000 1953 -230 -170 -130 -90 -260 60 200 310 110 -130 300 20 0 7000 1954 -10 40 -50 -70 -60 -40 260 170 120 110 140 230 71 7000 1955 100 -170 -220 -60 -150 80 200 320 160 130 -170 -70 14 7000 1956 -60 120 -50 -100 -100 20 230 30 -10 150 130 70 36 7000 1957 -30 -10 90 30 -280 -40 130 380 -30 -50 -20 -80 8 7000 1958 -70 -170 -170 -120 -80 0 90 10 270 310 70 -50 8 7000 1959 70 20 -30 -130 -80 190 310 -80 -130 180 -40 180 39 7000 1960 -80 -150 -110 -170 -90 -10 20 -160 -90 -50 -170 -50 -92 7000 1961 -190 -160 -350 -420 -190 -60 100 -30 -110 30 180 -100 -108 7000 1962 -80 -150 -320 -200 -210 120 240 120 110 10 170 -40 -19 7000 1963 -20 -120 0 -100 -80 70 190 150 -20 150 -20 150 31 7000 1964 60 60 -50 -100 10 10 300 -30 -40 10 -140 -110 -1 7000 1965 -190 -280 -260 -200 -190 -160 0 -80 -390 70 70 -110 -142 7000 1966 -70 -140 -240 -290 -50 80 110 -140 -30 -130 -230 -50 -98 7000 1967 -20 -120 -150 -110 30 50 260 230 80 360 110 60 67 7000 1968 20 -200 -100 -180 -90 40 80 120 260 200 -250 20 -5 7000 1969 -90 -170 -160 -100 -100 50 180 140 50 440 -110 -40 9 7000 1970 -310 -280 -230 -150 -160 120 240 90 180 -220 -10 -140 -72 7000 1971 -300 -200 -330 -320 -280 -10 70 80 230 170 -140 30 -83 7000 1972 10 -160 -130 -200 -110 50 160 200 0 320 0 -10 12 7000 1973 70 -110 -190 -260 -110 10 270 190 90 -10 -130 -200 -31 7000 1974 -50 -190 -100 -230 -170 80 160 40 -100 -270 0 -30 -71 7000 1975 -50 -100 -180 -200 -210 -100 160 140 220 20 90 40 -14 7000 1976 -30 -60 -80 -130 -160 40 140 310 310 -40 30 -180 12 7000 1977 -170 -110 -150 -120 -80 -60 -30 160 160 -120 -130 -120 -64 7000 1978 -150 -240 -220 -240 -120 -10 60 0 -80 -210 40 20 -95 7000 1979 -80 -230 -350 -290 -290 20 100 60 -10 -100 40 -30 -96 7000 1980 -150 -50 -70 -210 -260 60 30 200 40 180 0 -150 -32 7000 1981 10 30 -220 -90 0 110 240 130 120 -290 70 110 18 7000 1982 -110 -40 -40 -90 -140 40 250 260 220 -160 -110 -50 3 7000 1983 -60 -60 -190 -190 -130 230 160 250 290 40 10 -60 24 7000 1984 -20 -140 -130 -120 0 130 210 150 130 20 10 100 29 7000 1985 30 -40 10 -240 -90 120 100 0 120 180 50 -140 9 7000 1986 -200 -160 -140 -220 -210 40 270 240 80 450 260 460 75 7000 1987 330 140 350 270 600 390 130 80 360 320 20 -110 241 7000 1988 -50 -180 -270 -60 -110 110 130 330 370 190 -190 -170 9 7000 1989 -120 -330 -630 -210 -180 -10 310 330 510 470 160 80 34 7000 1990 220 40 -50 20 90 220 200 100 380 400 220 20 155 7000 1991 -160 -130 -100 170 10 40 80 120 110 130 -50 150 32 7000 1992 -250 -170 -110 -190 -20 -60 30 90 150 -60 110 60 -35 7000 1993 360 210 200 0 -80 50 310 200 80 -70 330 90 140 7000 1994 303130313130313031 - -180 30 -4099999999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. RAU-CHUA 030556 69 30 N166 35 EK7042002 47 0 0 39 1950 110 0 -70 -90 -120 250 80 110 210 210 140 -170 55 7000 1951 -90 -120 -310 -130 -120 120 130 280 170 270 70 130 34 7000 1952 -70 -50 -10 20 50 70 230 -60 90 70 50 -20 31 7000 1953 -170 -100 -40 -70 -210 130 160 70 110 -70 340 90 20 7000 1954 -110 -40 -70 -80 10 120 270 180 230 190 130 340 99 7000 1955 190 -140 -100 0 -70 170 230 260 270 240 -70 10 84 7000 1956 10 90 0 -10 0 140 240 50 90 180 160 0 79 7000 1957 -100 -190 -190 -60 -250 110 340 540 240 0 -60 -110 24 7000 1958 -120 -240 -210 -170 -160 10 170 -70 320 350 140 0 3 7000 1959 -100 120 -50 -170 -110 190 160 -190 -180 120 -60 170 -9 7000 1960 -140 -210 -140 -200 -120 0 -80 -250 -140 -160 -160 -20 -135 7000 1961 -220 -200 -340 -410 -50 20 20 -40 -90 -50 130 -120 -112 7000 1962 -130 -190 -380 -290 -250 120 260 40 90 20 240 -220 -57 7000 1963 -30 -100 0 -70 -50 280 230 120 -60 130 0 140 51 7000 1964 31 - 50 50 -20 -70 40 120 290 -70 16099999 -100 2099999 7000 1965 -130 -170 -130 -50 -60 -40 40 -40 680 110 150 0 30 7000 1966 10 -10 -150 -190 10 150 120 -110 -80 10 -230 -30 -41 7000 1967 10 -80 -130 -110 130 10 320 320 320 410 150 110 124 7000 1968 30 -160 -60 -160 -90 70 40 100 220 110 -230 60 -5 7000 1969 -60 -190 -170 -110 -120 50 60 120 -40 440 -60 150 8 7000 1970 -190 -230 -230 -140 -70 200 200 40 240 -270 -60 0 -42 7000 1971 -190 -90 -210 -200 -160 50 130 50 190 260 40 30 -8 7000 1972 0 -180 -200 -240 -120 110 120 200 100 340 30 0 15 7000 1973 80 -100 -160 -240 -120 60 300 250 170 80 -20 -130 15 7000 1974 0 -210 -120 -230 -160 130 120 70 0 -240 -30 -90 -62 7000 1975 -70 -90 -130 -170 -140 50 210 60 0 160 160 10 5 7000 1976 -100 -110 -90 -130 -160 70 170 300 220 -40 50 -160 2 7000 1977 -160 -160 -160 -150 -100 -10 -100 0 160 -40 -120 100 -61 7000 1978 -30 -300 -200 -220 -180 60 50 -10 -110 -150 -340 40 -114 7000 1979 0 -270 -380 -300 -300 120 70 40 10 -100 -10 0 -92 7000 1980 -170 -90 -50 -190 -250 100 0 40 -140 260 -90 -240 -68 7000 1981 -180 0 -310 -110 -30 130 230 120 50 -190 100 -10 -17 7000 1982 -40 -40 -70 -80 -130 80 170 160 140 -200 -100 -20 -11 7000 1983 -130 -140 -210 -200 -120 280 160 230 390 80 0 20 30 7000 1984 -60 -180 -160 -160 0 230 220 120 260 90 60 0 35 7000 1985 20 -20 40 -140 -60 80 110 80 220 160 110 -60 45 7000 1986 -140 -90 -40 -110 -120 310 280 270 130 360 -10 170 86 7000 1987 150 -150 -110 -200 -80 80 70 80 500 250 10 30 54 7000 1988 40 80 -60 -30 -100 130 140 280 380 200 -130 110 87 7000 1989 240 110 -130 -10 -70 290 370 320 290 440 300 300 205 7000 1994 303131303130 - -220 10 -70 -120 -40999999999999999999999999999999 58099999 7000 1995 3131303130 - 60 -10 -110 -90 -70 -909999999999999999999999999 -32099999 7000 1996 31 3031 - -100 -60 50 -110 0 27099999 -209999999999 -20 -20099999 7000 1997 -170 -110 -170 -120 -280 -90 -100 70 220 50 160 20 -44 7000 1998 -150 -60 -60 0 -50 -10 10 320 -150 130 10 40 3 7000 1999 30 -60 -110 -120 -30 160 80 -80 400 -100 100 -40 19 7000 2000 0 30 -180 -210 20 170 70 -120 250 200 10 -40 16 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. AION 030560 69 56 N167 59 EK7042002 47 0 0 39 1954 -40 20 -90 -110 0 -30 300 350 220 250 270 380 128 7000 1955 220 -100 -70 20 -40 220 270 300 270 230 -120 -20 100 7000 1956 -10 80 0 -40 -20 20 300 80 30 270 190 30 78 7000 1957 -50 -80 -140 0 -190 80 240 540 30 30 -50 -120 25 7000 1958 -100 -220 -210 -160 -150 20 130 0 360 450 100 -60 15 7000 1959 -140 110 -20 -140 -70 210 270 -150 -230 190 -30 200 17 7000 1960 -90 -150 -110 -170 -90 40 -60 -210 -150 -140 -150 -30 -109 7000 1961 -210 -200 -320 -380 -110 -40 40 -30 -30 70 220 -70 -88 7000 1962 -80 -140 -320 -230 -220 130 230 -70 120 30 240 -40 -29 7000 1963 -60 -130 -40 -140 -50 110 160 110 30 160 10 200 32 7000 1964 40 20 -60 -110 0 120 220 -130 30 30 -90 -10 5 7000 1965 -170 -190 -170 -110 -110 -90 40 -60 -230 40 90 -30 -82 7000 1966 -10 -50 -170 -220 30 160 80 -170 -70 -50 -270 -20 -63 7000 1967 30 -80 -110 -80 180 90 300 310 70 440 40 90 109 7000 1968 10 -170 -80 -150 -100 60 50 160 300 260 -240 10 10 7000 1969 -110 -180 -210 -140 -120 60 100 130 -20 420 -120 60 -9 7000 1970 -230 -250 -240 -140 -80 220 180 40 170 -260 -70 -40 -58 7000 1971 -220 -60 -210 -190 -170 20 60 0 30 160 -50 0 -52 7000 1972 -10 -210 -210 -250 -150 50 90 190 -40 320 -10 -40 -21 7000 1973 40 -130 -210 -290 -140 -30 260 210 180 -20 -10 -100 -19 7000 1974 -40 -240 -170 -300 -220 70 150 40 -140 -310 -100 -40 -107 7000 1975 -30 -70 -140 -170 -150 -40 130 100 150 -90 -120 30 -33 7000 1976 -70 -100 -110 -150 -150 60 140 300 190 -40 60 -130 0 7000 1977 -150 -160 -190 -140 -80 -60 -130 -10 160 10 -170 -60 -81 7000 1978 -110 -300 -230 -250 -120 20 30 -10 -50 -130 20 -120 -103 7000 1979 -110 -270 -90 -370 -370 -40 90 20 10 -100 30 20 -97 7000 1980 -110 -20 -30 -180 -230 90 -20 130 -70 290 -30 -120 -25 7000 1981 70 60 -180 -190 -50 120 220 90 10 -220 140 -20 4 7000 1982 -110 -60 -60 -100 -150 90 120 140 90 -220 -170 -30 -38 7000 1983 -50 -180 -240 -220 -190 250 130 250 350 120 60 -50 20 7000 1984 0 -130 -170 -140 30 160 200 190 140 40 20 -90 21 7000 1985 -10 -120 -20 -230 -90 -10 50 -30 110 130 40 -30 -17 7000 1986 -150 -100 -70 -300 -280 170 230 230 100 380 -10 190 34 7000 1987 170 -70 -30 -140 -40 70 60 0 420 370 50 40 76 7000 1988 10 -20 -120 -160 -170 70 80 180 320 210 -130 110 32 7000 1989 280 140 -130 -30 -70 280 350 240 250 320 30 30 141 7000 1990 100 -40 10 30 50 280 90 0 220 160 -50 -80 64 7000 1991 -130 -100 -60 -100 -100 0 40 20 100 190 -30 300 12 7000 1992 -80 -90 -180 -320 -40 260 60 440 210 -30 30 -30 19 7000 1993 80 20 20 -70 70 260 200 60 -180 -10 140 110 59 7000 1994 150 80 -130 -220 -110 390 200 400 240 150 220 440 151 7000 1995 30 XX 50 -120 -170 -140 -11099999 60 130 70 -80 10 130 -14 7000 1996 31 XX 20 -100 0 -23099999 150 250 30 160 -70 40 -160 9 7000 1997 -110 -40 -90 -60 -220 -10 0 90 300 250 240 -70 23 7000 1998 -270 -200 -190 -140 -240 -60 120 410 0 170 40 30 -26 7000 1999 50 -40 -110 -130 -20 180 160 180 310 -150 -50 -100 23 7000 2000 31XX 10 80 -210 -220 0 150 70 -140 200 210 099999 13 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. PEVEK 030567 69 42 N170 15 EK7042002 51 0 0 39 1950 -40 -100 -140 -130 -120 250 30 80 190 190 120 -160 14 7000 1951 -100 -130 -400 -270 -220 -10 100 310 170 280 20 10 -19 7000 1952 -210 -170 -110 -80 -60 -80 220 -100 70 40 40 -110 -46 7000 1953 -290 -170 -160 -150 -290 30 80 60 100 -150 250 30 -55 7000 1954 -90 -30 -140 -170 -60 -90 220 300 220 180 180 310 70 7000 1955 170 -130 -120 -30 -90 170 230 260 210 240 -80 -60 66 7000 1956 -30 60 0 -30 -100 60 230 110 40 210 110 70 61 7000 1957 -70 -110 -120 30 -170 120 280 530 50 20 -50 -110 34 7000 1958 -110 -230 -210 -150 -50 80 120 60 340 390 30 -240 4 7000 1959 -270 -60 -170 -300 -150 260 230 -150 -210 90 -80 170 -53 7000 1960 -130 -190 -160 -220 -110 100 -80 -220 -190 -170 -180 -30 -131 7000 1961 -250 -250 -350 -400 -100 -40 50 -70 -130 -30 120 -150 -133 7000 1962 -120 -180 -380 -260 -200 100 250 10 60 -30 110 -170 -67 7000 1963 -50 -90 30 -180 -220 90 120 160 -10 140 -20 110 8 7000 1964 60 10 -110 -120 20 10 270 -60 10 80 -120 -90 -3 7000 1965 -190 -250 -230 -160 -150 -170 0 -50 -290 90 100 -70 -113 7000 1966 -160 -110 -240 -280 -30 120 90 -160 -100 -70 -310 -70 -110 7000 1967 -20 -90 -120 -140 40 30 280 280 70 420 170 60 84 7000 1968 0 -170 -110 -170 -120 10 0 60 220 200 -210 10 -22 7000 1969 -120 -150 -180 -140 -120 10 130 160 -20 380 -120 80 -6 7000 1970 -230 -240 -250 -130 -60 190 210 90 200 -190 -30 -30 -39 7000 1971 -240 -100 -270 -240 -160 -40 60 80 50 190 -70 30 -59 7000 1972 -50 -250 -210 -230 -130 50 110 210 0 340 30 20 -8 7000 1973 70 -120 -150 -240 -80 0 310 290 160 120 -20 -100 22 7000 1974 60 -180 -80 -200 -130 100 170 30 -60 -290 20 -20 -47 7000 1975 -70 -110 -140 -180 -150 -60 130 120 180 0 120 0 -13 7000 1976 -80 -120 -100 -140 -100 60 140 290 250 0 80 -110 14 7000 1977 -120 -120 -160 -120 -90 -80 -150 20 200 -30 -160 -50 -72 7000 1978 -110 -290 -220 -240 -140 -20 10 -10 -70 -160 90 40 -92 7000 1979 -50 -210 -300 -260 -290 0 130 80 60 -40 100 60 -59 7000 1980 -90 10 10 -130 -180 110 -10 210 -10 310 10 -60 15 7000 1981 80 30 -210 -140 0 120 250 160 40 -170 180 10 29 7000 1982 -60 -50 -40 -100 -80 60 190 180 140 -120 -100 -20 0 7000 1983 -70 -90 -190 -170 -60 270 160 270 370 60 -10 -110 36 7000 1984 -30 -70 -150 -150 20 160 220 150 100 40 20 80 33 7000 1985 20 -50 30 -180 -50 40 40 20 150 190 100 -10 26 7000 1986 -140 -110 -60 -170 -190 160 260 290 140 370 0 190 63 7000 1987 180 -70 -30 -140 -40 50 90 80 410 320 70 90 85 7000 1988 110 -70 -90 -150 -140 120 120 330 350 180 -100 130 67 7000 1989 210 120 -120 50 -10 300 340 210 240 330 40 40 146 7000 1990 80 -60 -10 20 50 280 100 70 280 240 70 -50 90 7000 1991 3130 - -100 -80 -40 -209999999999 80 150 130 260 50 33099999 7000 1992 3130 30 - 50 40 -60 -1809999999999 160 500 250 8099999 11099999 7000 1993 250 40 0 -90 10 90 330 170 130 -20 280 -30 97 7000 1994 3130 - -300 -40 -110 -1709999999999 200 440 290 250 190 35099999 7000 1995 31 XX -40 -20 -120 -11099999 110 90 200 100 0 -190 -10 1 7000 1996 3130 - 100 -20 50 -1809999999999 320 0 -50 -40 -20 -15099999 7000 1997 -80 -40 -110 -60 -180 -40 70 50 230 50 220 0 9 7000 1998 -160 -80 -60 -30 -90 60 140 410 40 150 30 80 42 7000 1999 31303131 3130 - 90 10 -70 -11099999999999999999999 4509999999999 -6099999 7000 2000 3131 3130 - 100 70 -140 -200 30 2509999999999 2809999999999 -4099999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. VALKARKAI 030570 70 05 N170 56 EK7042002 38 0 0 39 1956 -50 80 -10 -50 -70 20 190 60 30 200 160 80 53 7000 1957 -50 -110 -130 30 -180 100 260 480 60 30 -50 -90 30 7000 1958 -140 -270 -220 -160 -110 40 80 30 350 430 160 -130 6 7000 1959 -190 30 -70 -200 -180 100 260 -120 -180 30 -130 80 -48 7000 1960 -130 -220 -200 -190 -80 60 -70 -180 -190 -130 -230 0 -129 7000 1961 -170 -190 -290 -360 -140 -60 110 -10 -60 -60 230 -60 -88 7000 1962 -80 -140 -340 -260 -250 0 210 -70 110 -10 120 -130 -70 7000 1963 -90 -170 -10 -80 -230 70 70 110 -70 70 -30 110 -20 7000 1964 60 40 -60 -90 10 20 230 -100 -40 100 -90 -90 -1 7000 1965 -240 -240 -190 -130 -130 -180 80 -40 -430 10 120 -20 -114 7000 1966 -20 -70 -190 -230 0 90 70 -30 -60 -30 -210 -50 -60 7000 1967 10 -100 -130 -120 90 90 270 250 60 380 150 110 90 7000 1968 -20 -140 -90 -160 -100 80 -40 60 160 220 -180 70 -11 7000 1969 -60 -130 -180 -90 -90 50 100 130 -40 330 -110 80 1 7000 1970 -240 -320 -250 -140 -100 180 200 70 190 -210 -130 0 -61 7000 1971 -160 -10 -190 -170 -150 -20 40 70 70 190 -110 110 -27 7000 1972 30 -180 -160 -230 -170 80 110 190 30 220 -50 20 -8 7000 1973 80 -140 -170 -250 -100 80 250 210 180 110 -30 -110 11 7000 1974 100 -120 -20 -160 -90 150 50 100 200 100 80 -20 32 7000 1975 -20 -80 -180 -210 -190 -50 120 120 140 -10 120 50 -15 7000 1976 -20 -70 -70 -110 -110 100 230 300 230 10 90 -110 39 7000 1977 -110 -120 -160 -70 -10 20 -160 -10 90 -110 -150 0 -66 7000 1978 -80 -290 -250 -260 -160 -80 0 -60 -120 -140 100 30 -108 7000 1979 -100 -320 -420 -390 -420 -80 140 20 20 -70 190 40 -115 7000 1980 -60 10 10 -150 -200 130 -20 110 -50 300 10 -90 0 7000 1981 70 60 -170 -70 70 150 230 200 30 -190 130 -40 39 7000 1982 -110 -40 -30 -80 -130 100 160 140 110 -230 -140 -30 -23 7000 1983 -140 -90 -180 -180 -140 290 160 260 400 80 -120 -10 28 7000 1984 80 -150 -110 -70 100 190 210 160 60 0 -160 -120 17 7000 1985 -110 -120 -40 -260 -100 50 40 -20 90 140 70 -20 -23 7000 1986 -160 -80 -30 -110 -180 200 240 250 150 330 -70 110 55 7000 1987 140 -40 100 -20 -60 -10 50 40 360 320 70 90 88 7000 1988 70 -60 -90 -110 -140 150 120 270 340 190 -110 140 65 7000 1989 290 180 -90 40 -40 410 400 350 340 490 40 50 205 7000 1990 80 -30 20 40 90 120 300 130 540 260 -60 -50 121 7000 1991 31XX -100 -80 -60 -120 -30 120 150 250 280 310 3099999 69 7000 1992 312931303130 - 999999999999999999999999999999 -40 370 250 90 200 9099999 7000 1993 2831303130 3130313031 - 2509999999999999999999999999 220999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. BILLINGA 030578 69 53 N175 46 EK7042002 43 0 0 39 1953 -240 -130 -140 -190 -360 80 140 110 170 -140 350 80 -23 7000 1954 -120 70 -70 -100 -140 -90 200 350 230 180 230 360 92 7000 1955 180 -50 0 0 -70 130 210 230 150 280 -80 -40 80 7000 1956 20 150 -10 -40 -60 70 240 110 30 240 160 160 89 7000 1957 -30 -40 -150 0 -220 50 260 500 120 20 -180 -130 17 7000 1958 -120 -240 -240 -200 -180 -60 30 -40 270 420 330 -120 -12 7000 1959 -300 20 -120 -240 -180 120 260 -200 -140 210 60 180 -28 7000 1960 -120 -130 -150 -210 -100 -30 30 -210 -210 -120 -210 -30 -124 7000 1961 -220 -240 -320 -380 -210 -40 70 -40 -80 -80 200 -70 -117 7000 1962 -80 -130 -350 -240 -220 40 180 -60 80 0 150 -70 -58 7000 1963 -110 -150 -20 -100 -120 60 70 120 -50 70 -20 110 -10 7000 1964 90 50 -80 -120 0 -10 210 -110 120 140 -80 -100 9 7000 1965 -210 -240 -280 -190 -270 -120 110 -40 -220 60 70 -20 -111 7000 1966 -70 -140 -240 -260 -60 40 10 -90 60 110 20 80 -44 7000 1967 0 -120 -150 -50 100 20 200 220 80 370 180 100 81 7000 1968 60 -140 -90 -170 -130 60 0 -20 170 270 -80 60 0 7000 1969 -140 -120 -240 -150 -240 -70 120 160 -50 320 -50 140 -25 7000 1970 -180 -180 -220 -120 -100 180 220 90 190 -190 -20 -20 -29 7000 1971 -220 -70 -270 -240 -220 -80 -10 40 10 250 -50 50 -67 7000 1972 50 -170 -130 -220 -210 40 40 140 -10 390 120 120 15 7000 1973 50 -140 -200 -270 -180 -80 270 240 160 70 -40 -230 -28 7000 1974 -180 -180 -90 -250 -200 40 80 80 20 -140 -60 -100 -81 7000 1975 -180 -100 -160 -200 -190 -30 120 50 190 -20 130 30 -30 7000 1976 -80 0 -80 -150 -160 50 150 290 270 10 80 -110 22 7000 1977 -120 -120 -140 -100 -60 -60 -200 -20 180 90 -230 -40 -68 7000 1978 -130 -320 -250 -250 -180 20 -50 -40 110 -40 70 20 -86 7000 1979 -70 -250 -330 -280 -290 130 150 20 50 -190 -10 70 -83 7000 1980 -150 -90 -100 -210 -240 40 -60 150 10 260 20 -20 -32 7000 1981 140 60 -120 -110 -20 60 260 150 -30 -210 100 -50 19 7000 1982 -140 -60 -70 -120 -170 30 150 160 130 -190 -90 -30 -33 7000 1983 -40 -60 -200 -160 -150 560 210 290 360 130 160 -20 90 7000 1984 70 0 -40 30 180 160 160 180 100 140 -30 -90 72 7000 1985 -10 -100 -10 -270 -110 50 -30 -10 180 70 10 -20 -20 7000 1986 -120 -100 -40 -130 -210 100 200 210 120 330 -70 230 45 7000 1987 210 -80 -80 -150 -70 10 40 0 390 250 70 30 52 7000 1988 40 -60 -80 -140 -120 70 220 460 350 180 -180 270 86 7000 1989 290 130 -10 210 -40 220 370 190 300 340 -30 -30 162 7000 1990 -10 -140 -80 -30 10 370 150 100 410 190 -10 -20 79 7000 1991 -40 -90 -120 -100 -40 100 60 150 260 290 10 280 65 7000 1992 -50 -110 -140 -230 20 180 50 350 250 110 140 120 58 7000 1993 230 50 30 -130 -190 -290 180 230 170 -40 310 140 58 7000 1994 -390 -90 -100 -180 -120 280 110 360 250 240 110 10 40 7000 1995 28 313130 31 - 5099999 -100 -50 -30 30999999999999999 -20 209999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. MYS SHMIDTA 030610 68 54 N179 22 WK7042002 45 0 0 39 1950 -20 -60 -110 -110 -100 250 10 10 190 190 0 20 23 7000 1951 -110 -140 -490 -300 -330 -110 -10 280 110 210 120 10 -63 7000 1952 -230 -160 -120 -140 -150 -230 140 -170 70 80 150 -100 -72 7000 1953 -230 -90 -140 -140 -240 -20 10 100 160 -10 120 20 -39 7000 1954 -60 90 -80 -200 -140 -60 170 320 240 240 160 360 87 7000 1955 190 -80 -90 0 -60 80 130 160 100 320 -130 -190 37 7000 1956 -120 80 -10 -50 -70 20 140 80 0 170 180 150 47 7000 1957 -100 -30 -50 50 -200 60 250 390 70 30 -150 -130 16 7000 1958 -60 -220 -210 -170 -170 -100 0 100 330 430 120 -130 -5 7000 1959 -320 30 -140 -250 -120 130 280 -130 -210 200 -10 220 -26 7000 1960 -120 -190 -70 -100 -90 -30 60 -50 -210 -20 -70 0 -73 7000 1961 -150 -170 -230 -310 -130 -10 110 -20 -40 50 190 -40 -62 7000 1962 -80 -150 -360 -250 -230 20 190 40 140 120 210 -130 -40 7000 1963 -110 -180 -50 -140 -130 80 40 190 0 360 30 140 21 7000 1964 100 40 -170 -170 -10 0 230 -70 180 250 -20 -120 20 7000 1965 -180 -170 -160 -10 -160 -50 90 100 -30 170 20 40 -27 7000 1966 -90 -150 -220 -240 -70 60 10 -100 20 130 -90 40 -58 7000 1967 -50 -150 -170 -60 10 210 390 270 120 340 250 60 103 7000 1968 20 -190 -150 -170 -120 40 -60 -40 230 250 -60 60 -15 7000 1969 -240 -110 -220 -160 -170 -60 100 180 -40 310 -30 80 -29 7000 1970 -240 -170 -220 -160 -180 100 160 60 160 -200 -20 -30 -62 7000 1971 -240 -90 -320 -280 -270 -110 10 80 0 220 -30 10 -85 7000 1972 30 -190 -120 -210 -230 20 0 130 50 390 150 -40 -1 7000 1973 50 -200 -210 -300 -150 -80 210 230 170 90 -60 -120 -29 7000 1974 50 -180 -100 -220 -160 100 0 0 0 -280 -20 -10 -68 7000 1975 -80 -110 -140 -210 -190 -60 50 30 170 10 50 10 -39 7000 1976 -100 -120 -80 -150 -160 0 60 210 290 70 80 -90 1 7000 1977 -90 -90 -130 -140 -100 -80 -250 -70 90 40 -100 -10 -78 7000 1978 -90 -240 -200 -260 -180 0 -80 -20 20 -40 50 110 -76 7000 1979 40 -210 -260 -220 -310 40 150 30 30 0 140 90 -39 7000 1980 -110 -10 -20 -150 -240 80 -100 190 10 270 100 -40 -2 7000 1981 80 40 -180 -150 -10 50 270 220 0 -140 220 -10 32 7000 1982 -110 -50 -60 -130 -200 -10 150 130 180 -60 -80 -50 -24 7000 1983 -60 -70 -190 -160 -140 290 100 270 380 180 130 -60 56 7000 1984 80 -40 -90 -50 80 120 220 150 30 120 30 40 58 7000 1985 50 -70 30 -210 -50 10 -20 -20 210 170 20 30 13 7000 1986 -90 -60 -40 -160 -220 70 190 260 150 340 -20 270 59 7000 1987 240 -50 -50 -100 -50 0 50 -20 400 290 120 90 77 7000 1988 60 -40 -80 -170 -150 80 100 320 360 110 -10 170 63 7000 1989 270 80 -90 70 -60 250 320 190 220 290 40 30 134 7000 1990 60 -50 -70 -30 10 240 80 -10 330 210 -30 -70 56 7000 1991 -50 -30 0 -100 -50 -30 60 150 210 200 -10 370 61 7000 1992 20 -10 -20 -200 70 80 0 430 310 110 100 100 83 7000 1993 290 -30 10 -110 -210 30 160 210 270 50 370 40 90 7000 1994 3130313130313031 - -370 -60 -70 -180999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. VRANGELIA (VRANGELIA OSTROV) 030620 70 59 N178 29 WK7042002 51 0 0 39 1950 100 0 40 10 10 100 80 180 180 -60 -220 -270 13 7000 1951 -310 -250 -450 -270 -190 -30 80 160 130 200 180 110 -52 7000 1952 -60 -130 -70 -60 -10 -150 130 100 180 70 50 -40 2 7000 1953 -130 -90 -10 -40 -210 -10 150 180 180 50 330 70 39 7000 1954 -120 -100 -160 -150 10 -60 120 40 90 100 60 110 -4 7000 1955 120 -90 -70 50 20 250 140 240 220 80 -40 -60 72 7000 1956 -130 -20 -70 -60 -20 60 140 50 -90 -50 30 -20 -15 7000 1957 -30 -100 -100 -20 -140 10 170 190 150 10 240 120 42 7000 1958 90 -250 -280 -260 -260 -70 -20 30 130 -70 -130 50 -85 7000 1959 -250 20 -140 -310 -160 -60 160 -30 -40 -30 10 110 -60 7000 1960 -130 -200 -200 -210 -160 10 20 -80 0 -100 -280 -80 -117 7000 1961 -270 -330 -220 -280 -90 10 80 30 40 70 -40 -50 -86 7000 1962 -70 -130 -230 -160 -110 -30 100 80 60 40 20 -100 -44 7000 1963 -170 -190 -110 -160 -100 30 60 100 -50 130 -110 70 -40 7000 1964 40 -50 -130 -150 -60 70 190 70 40 90 -60 -70 -1 7000 1965 -190 -200 -180 -110 -110 -100 10 0 -60 40 60 -50 -73 7000 1966 -90 -110 -240 -280 -60 60 30 -50 90 -100 -130 -30 -76 7000 1967 -20 -110 -150 -100 10 10 90 80 150 200 90 -30 19 7000 1968 -100 -220 -110 -170 -130 10 0 -10 90 140 150 -70 -35 7000 1969 -130 -120 -170 -180 -150 -90 140 190 140 160 -80 60 -18 7000 1970 -180 -220 -280 -210 -230 120 90 120 220 40 -20 -40 -49 7000 1971 -240 -120 -240 -250 -220 -90 -50 140 140 140 -130 -10 -77 7000 1972 -30 -250 -240 -280 -150 50 -10 100 50 200 -20 -90 -55 7000 1973 60 -160 -210 -290 -160 -30 140 60 10 -90 -90 -70 -68 7000 1974 -10 -190 -150 -220 -140 50 160 50 0 -30 70 0 -33 7000 1975 -50 -80 -160 -220 -210 -110 100 160 190 50 -60 -30 -34 7000 1976 -50 -110 -90 -140 -140 0 70 180 180 10 60 -100 -11 7000 1977 -90 -80 -120 -150 -110 -70 -70 20 140 50 -50 -40 -47 7000 1978 -80 -210 -210 -240 -190 10 -30 90 100 110 120 100 -35 7000 1979 0 -170 -240 -190 -200 40 60 -10 -90 30 0 -20 -65 7000 1980 -140 -60 -90 -170 -240 30 -50 220 120 -30 -30 -210 -55 7000 1981 -10 -90 -280 -190 -30 -10 190 200 110 -50 120 -120 -13 7000 1982 -230 -130 -40 -90 -100 0 110 80 210 0 70 50 -5 7000 1983 -30 -20 -120 -130 -130 180 140 170 90 120 150 -60 30 7000 1984 20 -90 -130 -70 20 120 170 160 140 100 190 80 60 7000 1985 30 -70 10 -190 -20 40 80 80 160 120 10 80 29 7000 1986 -60 -60 -60 -120 -120 120 70 220 70 160 0 190 35 7000 1987 150 -60 -50 -90 10 40 120 130 190 240 120 120 78 7000 1988 70 -20 -80 -120 -110 100 100 290 210 90 80 120 61 7000 1989 140 30 -150 0 -60 190 230 210 320 360 150 60 124 7000 1990 100 -20 10 -20 80 160 200 160 270 130 50 -20 92 7000 1991 -40 -50 -60 -70 -50 80 100 260 170 60 80 230 60 7000 1992 90 -10 -20 -130 100 160 140 290 290 90 110 100 101 7000 1993 200 50 30 -70 -50 60 190 240 180 70 250 -10 95 7000 1994 -180 -40 -70 -140 -30 210 150 230 250 190 110 210 75 7000 1995 -50 -10 -80 -30 50 110 130 310 240 120 110 140 87 7000 1996 130 40 40 -70 20 170 290 180 90 70 70 -30 84 7000 1997 30 XX 20 -10 -80 -10 -9099999 100 280 200 40 200 90 67 7000 1998 31283130313031 - 99999999999999999999999999999999999 170 140 90 140 7099999 7000 1999 90 10 -80 -130 -30 150 130 110 270 110 50 20 58 7000 2000 70 90 -120 -150 50 180 210 110 190 200 190 130 96 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. VANKAREM 030630 67 50 N175 50 WK7042002 51 0 0 39 1950 -90 -130 -130 -160 -130 100 -20 -30 290 290 -20 40 1 7000 1951 -100 -120 -570 -320 -370 -100 -80 190 180 220 60 -110 -94 7000 1952 -290 -210 -200 -180 -190 -270 130 -180 60 110 130 -30 -93 7000 1953 -180 0 -60 -100 -180 -60 10 120 160 10 460 40 17 7000 1954 -210 30 -200 -310 -180 -80 50 220 240 280 180 350 31 7000 1955 160 -200 -140 -90 -130 30 80 80 130 420 -100 -130 11 7000 1956 -160 110 -90 -230 -230 -110 210 190 50 230 310 170 37 7000 1957 -170 -50 -100 -20 -270 50 160 400 130 -10 0 -70 4 7000 1958 -70 -220 -230 -180 -220 -180 -130 -20 300 340 150 -90 -45 7000 1959 -290 40 -130 -260 -220 -110 180 -170 -260 120 -60 190 -81 7000 1960 -150 -220 -210 -200 -120 -60 -110 -210 -250 -60 -160 -60 -150 7000 1961 -120 -190 -210 -470 -330 -60 70 60 -110 60 120 -120 -107 7000 1962 -200 -220 -390 -310 -240 40 180 10 120 100 380 -140 -56 7000 1963 -60 -220 -110 -170 -210 -70 -60 200 20 320 0 100 -20 7000 1964 80 40 -110 -120 -30 60 140 0 0 220 -80 -190 1 7000 1965 -210 -180 -150 -90 -60 0 0 10 -10 220 70 -40 -36 7000 1966 -90 -120 -180 -110 0 150 90 -90 20 180 -80 60 -13 7000 1967 -30 -90 -190 -100 -120 -140 150 290 90 220 320 160 48 7000 1968 -120 -330 -220 -260 -290 -200 -170 -120 340 230 -10 80 -88 7000 1969 -240 -130 -280 -200 -160 -80 110 230 -80 330 0 70 -34 7000 1970 -300 -190 -270 -220 -240 100 140 80 190 -70 -40 -10 -69 7000 1971 -250 -70 -290 -230 -200 -120 -20 90 110 310 -50 40 -56 7000 1972 70 -160 -70 -40 -170 40 -70 80 0 380 -10 -120 -5 7000 1973 70 -240 -200 -310 -170 -150 150 220 260 180 -170 -160 -41 7000 1974 60 -190 -90 -200 -160 80 -20 0 -70 -400 0 20 -80 7000 1975 -90 -40 -160 -230 -210 -80 20 10 180 50 50 70 -36 7000 1976 -80 -150 -120 -330 -230 0 30 170 250 130 110 -30 -20 7000 1977 -60 -90 -140 -150 -100 -130 -270 -110 60 170 -90 -50 -80 7000 1978 -110 -250 -250 -240 -160 -30 -140 -70 140 50 110 100 -70 7000 1979 -70 -260 -260 -240 -350 40 110 50 100 50 90 70 -55 7000 1980 -100 0 -30 -160 -260 30 -110 280 10 280 150 -100 -1 7000 1981 140 70 -140 -140 -40 50 250 250 60 -100 190 -50 45 7000 1982 -120 -20 10 -80 -120 30 160 90 270 -80 -100 -10 2 7000 1983 -30 -40 -150 -120 -160 450 110 300 370 260 300 -50 103 7000 1984 10 -90 -130 -120 0 110 270 170 30 110 20 20 34 7000 1985 90 -80 20 -200 -40 30 -20 40 320 180 -60 50 28 7000 1986 -90 -130 -80 -180 -250 60 190 300 170 250 -10 350 50 7000 1987 320 -10 -30 10 0 90 90 -10 370 290 140 90 113 7000 1988 50 -40 -80 -150 -110 70 40 300 360 120 40 160 64 7000 1989 220 40 -180 -10 -130 180 220 230 140 350 90 140 108 7000 1990 200 50 30 80 110 250 90 20 360 340 100 -30 133 7000 1991 60 110 50 -140 -80 -50 100 110 100 200 -10 340 66 7000 1992 31 31 - 160 110 60 -210 30 150 -110 470 46099999 1409999999999 7000 1993 170 40 -40 -90 -230 40 40 250 320 100 290 90 81 7000 1994 3031 - -260 -30 -20 -160 -110 100 20 230 170 80999999999999999 7000 1995 31283130313031 - 99999999999999999999999999999999999 130 110 180 -50 099999 7000 1996 50 50 70 100 -20 50 200 -20 90 110 50 -30 58 7000 1997 10 -90 -60 -30 -40 60 140 220 270 240 200 80 84 7000 1998 110 110 140 180 120 90 90 330 -40 190 250 40 135 7000 1999 120 110 130 30 20 -40 110 100 80 90 110 80 78 7000 2000 30 XX 150 120 80 0 -30 -20 -50 10 200 21099999 140 73 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. KOLUCHIN 030640 67 29 N174 39 WK7042002 42 0 0 39 1950 -60 -80 -90 -140 -150 140 -10 -20 220 260 -20 100 13 7000 1951 -40 0 -440 -290 -370 -160 -120 130 160 110 80 -60 -84 7000 1952 -280 -180 -130 -110 -250 -340 90 -100 80 100 170 0 -79 7000 1953 -220 -100 -170 -180 -290 -20 0 70 140 -10 410 50 -27 7000 1954 -170 70 -170 -280 -180 -50 50 180 220 280 260 490 58 7000 1955 260 -80 -70 10 -20 110 50 90 80 350 -80 -120 50 7000 1956 -160 130 10 0 30 80 50 100 20 150 410 260 89 7000 1957 -180 20 -20 30 -190 40 100 280 110 -20 -70 -110 -1 7000 1958 -110 -210 -240 -160 -210 -150 -110 -10 320 360 80 -90 -44 7000 1959 -250 70 -30 -300 -260 -20 180 -150 -190 100 100 240 -43 7000 1960 -80 -230 -240 -170 -90 -30 -100 -90 -170 40 0 30 -93 7000 1961 -130 -260 -280 -400 -230 -70 30 30 0 110 180 -70 -90 7000 1962 -250 -250 -380 -330 -290 -10 50 -10 130 -10 200 -210 -113 7000 1963 -170 -210 -80 -180 -240 -70 -10 150 -30 280 0 120 -35 7000 1964 90 30 -200 -150 -110 10 190 -50 100 320 20 -110 12 7000 1965 -170 -160 -110 -50 10 -70 -30 10 -20 280 110 120 -5 7000 1966 0 -40 -120 -130 20 -430 60 -50 20 150 -90 50 -46 7000 1967 10 -40 -290 -90 -70 -70 160 360 100 290 410 270 88 7000 1968 -100 -270 -200 -230 -210 10 -30 -20 290 280 0 30 -37 7000 1969 -230 -70 -190 -150 -120 -60 130 260 -20 370 -70 60 -6 7000 1970 -200 -120 -260 -210 -240 50 120 50 210 -80 20 -30 -58 7000 1971 -260 -20 -250 -220 -180 -150 -50 80 50 230 -70 -20 -72 7000 1972 0 -270 -170 -230 -220 50 50 180 50 330 110 -50 -13 7000 1973 140 -170 -150 -220 -60 -80 100 140 140 130 0 160 13 7000 1974 80 -100 -20 -140 -110 40 -10 30 -20 -260 0 10 -41 7000 1975 -60 -60 -80 -140 -90 -40 -10 50 200 180 10 90 5 7000 1976 -50 -140 -60 -90 -50 30 -10 140 300 170 120 -20 29 7000 1977 -20 -90 -140 -170 -110 -180 -230 -90 -50 0 -120 -20 -101 7000 1978 -90 -210 -160 -130 -60 90 -140 -50 130 40 70 60 -37 7000 1979 20 -170 -110 -80 -180 90 80 20 70 100 240 60 12 7000 1980 100 300 300 180 -250 -40 -150 -440 0 380 230 20 51 7000 1981 90 40 -130 -180 -30 0 200 240 40 -70 280 -30 38 7000 1982 -110 -100 -40 -110 -170 -40 130 90 230 10 30 20 -5 7000 1983 100 80 -130 -110 -150 260 50 240 370 240 180 -90 86 7000 1984 70 -80 -140 -130 -30 140 160 70 20 70 -70 -80 1 7000 1985 60 -70 120 -200 -100 0 -80 0 270 110 -110 50 5 7000 1986 -40 -80 -80 -190 -260 70 130 320 220 330 110 250 66 7000 1987 140 -30 0 -30 30 160 40 -40 460 320 140 90 107 7000 1988 30 40 20 -90 -50 110 10 330 360 120 180 200 105 7000 1989 220 -100 -160 -10 -170 180 230 130 190 260 0 30 68 7000 1990 100 -30 -10 -60 40 340 40 50 370 300 0 -50 91 7000 1991 0 60 30 -20 0 10 140 250 340 380 100 490 150 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. NETTEN 030650 66 58 N171 56 WK7042002 46 0 0 39 1950 -70 -100 -90 -170 -190 140 -30 -60 210 250 -40 100 -4 7000 1951 -80 -70 -470 -260 -320 -60 -50 240 250 340 260 -20 -20 7000 1952 -190 -170 -110 -130 -310 -330 90 -10 120 280 230 60 -39 7000 1953 -190 -60 -170 -150 -240 -70 50 170 230 50 520 -60 6 7000 1954 -310 0 -220 -330 -190 -80 70 290 270 370 180 420 40 7000 1955 130 -140 -120 -100 -100 50 110 190 160 360 -210 -170 15 7000 1956 -240 40 -70 -130 -110 100 140 170 50 180 300 80 42 7000 1957 -240 -40 -100 -80 -240 -60 140 350 240 70 30 -50 2 7000 1958 -70 -130 -270 -170 -210 -180 -70 30 330 410 50 -150 -36 7000 1959 -340 50 0 -210 -100 50 250 -150 -250 150 110 200 -20 7000 1960 -60 -250 -220 -150 -60 -120 -170 -180 -220 -60 20 160 -108 7000 1961 10 -120 -190 -390 -320 -160 30 40 20 110 190 40 -61 7000 1962 -130 -170 -350 -240 -190 30 80 40 110 -70 180 -160 -73 7000 1963 -110 -230 -100 -150 -150 60 10 230 50 370 30 100 11 7000 1964 60 -20 -100 -120 -60 -130 130 -130 20 200 40 -170 -23 7000 1965 -150 -110 40 -20 50 -40 10 60 80 240 10 110 25 7000 1966 -30 -100 -190 -190 -10 150 20 -40 40 170 -90 80 -15 7000 1967 30 -10 -170 -70 -120 -10 190 290 180 410 -120 160 65 7000 1968 -100 -270 -200 -230 -230 -10 -130 -40 340 280 0 110 -39 7000 1969 -210 -100 -170 -150 -140 -70 120 290 -20 450 60 120 17 7000 1970 -280 -120 -260 -210 -240 100 120 70 200 -60 -50 60 -56 7000 1971 -240 20 -250 -220 -220 -220 10 80 50 240 -70 20 -67 7000 1972 50 -310 -180 -250 -310 50 -80 110 80 410 210 -100 -26 7000 1973 20 -190 -170 -290 -150 -70 140 190 180 150 -190 -200 -47 7000 1974 -40 -210 -70 -160 -110 50 -50 -110 -50 -260 30 -80 -88 7000 1975 -110 -100 -180 -250 -100 -110 20 20 240 110 -20 40 -36 7000 1976 -100 -80 30 -160 -140 -30 0 140 370 190 40 -80 15 7000 1977 -30 -80 -150 -200 -110 -170 -290 -160 20 50 -30 110 -87 7000 1978 -90 -170 -190 -250 -180 -70 -200 -70 130 0 140 140 -67 7000 1979 -20 -220 -190 -180 -290 50 60 40 110 130 280 60 -13 7000 1980 -110 0 -10 -110 -190 0 -140 230 70 360 90 -60 11 7000 1981 160 40 -160 -190 -50 40 150 220 40 -90 250 -140 22 7000 1982 20 -150 -40 -120 -190 -30 90 90 260 10 -60 20 -7 7000 1983 0 -10 -120 -100 -150 270 10 280 360 240 190 -160 67 7000 1984 30 -80 -150 -130 -10 90 200 120 40 120 10 10 22 7000 1985 90 -110 0 -140 0 70 -70 40 300 330 -60 90 46 7000 1986 120 -60 -90 -220 -280 50 190 340 220 390 30 400 93 7000 1987 270 -50 -90 -100 -70 -10 80 20 500 370 260 140 111 7000 1988 10 -80 -140 -200 -140 90 60 360 400 140 150 250 75 7000 1989 140 -130 -100 0 -160 170 260 220 250 320 80 90 97 7000 1990 150 -40 -80 -100 -80 160 70 0 310 300 -30 -110 46 7000 1991 313130313031 - -70 -10 -80 -150 -40 -8099999999999999999999999999999999999 7000 1992 20 -110 -130 -300 -80 30 -10 420 430 190 270 170 76 7000 1993 340 10 20 -160 -280 50 90 210 300 160 390 190 110 7000 1994 31XX -320 -100 -70 -220 -130 210 200 280 310 350 24099999 69 7000 1995 3130313130313031 - 20 -40 -180 -60999999999999999999999999999999999999999999999 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. RATMANOVA 030670 66 51 N169 08 WK7042002 f 41 3 0 39 1950 -100 -10 0 -80 -100 50 -40 -20 100 240 -60 80 5 7000 1951 -90 -20 -160 -130 -90 -70 -20 140 80 210 150 -110 -9 7000 1952 -220 -180 -170 -210 -80 -160 50 10 20 100 130 40 -55 7000 1953 -180 -180 -150 -60 -30 10 0 10 150 30 320 40 -3 7000 1954 -160 0 -60 -260 10 -60 90 120 60 120 130 140 11 7000 1955 120 -170 -140 -120 -90 60 30 40 100 190 -100 -140 -17 7000 1956 -240 -10 -80 -100 50 90 40 90 70 40 50 -180 -15 7000 1957 -270 -340 -250 -70 -240 30 30 120 70 -30 -60 -50 -87 7000 1958 -100 -110 -80 50 -140 -40 -10 60 170 230 170 -30 14 7000 1959 -230 80 -90 -220 -120 0 220 20 -10 190 160 40 3 7000 1960 -10 -30 -270 -190 0 10 -10 0 -20 70 110 170 -14 7000 1961 30 -190 -180 -160 -50 -20 70 100 100 100 130 -120 -15 7000 1962 -90 50 -180 -210 -130 -20 40 70 60 -60 30 -110 -47 7000 1963 0 -130 -70 -80 -20 110 30 60 170 180 -10 150 34 7000 1964 140 -70 -110 -70 -40 -20 120 -40 100 210 50 -140 11 7000 1965 -160 -240 -90 -110 -10 -20 30 80 90 170 130 0 -9 7000 1966 90 0 -270 -180 -10 100 0 0 80 110 -60 120 -2 7000 1967 230 170 90 160 80 70 200 260 170 270 130 90 160 7000 1968 70 -160 30 -10 -30 -90 -100 -10 130 170 110 100 18 7000 1969 -100 -30 -130 -50 100 -20 80 180 90 190 -50 150 35 7000 1970 -170 80 -170 -110 -70 100 140 60 110 -40 170 70 13 7000 1971 -190 -70 -120 -130 -30 80 30 120 200 210 20 40 14 7000 1972 80 -310 -100 -100 -50 80 20 120 70 320 240 0 32 7000 1973 180 40 -70 -90 20 50 140 170 130 170 -20 -40 57 7000 1974 20 -270 -90 -120 -30 70 90 10 50 90 140 -20 -3 7000 1975 0 -50 20 -60 -140 -170 90 80 180 70 30 70 11 7000 1976 -60 -110 10 -30 100 80 70 150 250 170 120 -80 56 7000 1977 90 0 -90 -100 90 50 -100 70 60 20 -30 50 9 7000 1978 140 -30 -140 -60 -50 40 -30 70 190 150 290 210 65 7000 1979 180 -150 -60 80 -60 100 90 80 130 150 180 80 68 7000 1980 -100 -30 70 -100 80 40 -250 -70 -180 40 -120 -100 -60 7000 1981 200 0 -50 40 80 0 100 130 40 -40 150 20 56 7000 1982 30 270 210 110 100 -50 -130 -170 -40 -160 -270 -180 -25 7000 1983 -320 -220 -310 -200 -220 70 -20 -10 -60 30 20 -140 -115 7000 1984 -170 -140 -160 -190 -110 -90 -110 -180 -280 -220 -140 -190 -165 7000 1985 0 -420 -330 -390 -120 -120 -330 -230 -110 0 -170 -80 -190 7000 1986 3031 - -290 -240 -300 -360 -370 -190 -200 -110 -190 -110999999999999999 7000 1989 312831303130 - 999999999999999999999999999999 280 300 300 270 70 2099999 7000 1990 370 100 20 -20 100 190 180 100 120 -20 160 150 121 7000 1991 140 120 130 140 150 80 60 140 240 250 200 70 143 7000 1992 80 -10 10 50 110 120 20 250 170 150 190 180 110 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan27 : Suspicious data from 1982 to 1993. Possible new gauge in 1989. Entire record flagged for attention. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. PROVIDENIA 030725 64 25 N173 14 WK7042002309 33 0 0 39 1951 312831303130 - 999999999999999999999999999999 -100 10 0 150 50 -2099999 7000 1952 -50 -40 -50 -50 -130 -170 -120 -180 -90 30 90 120 -53 7000 1953 40 60 -80 -30 -40 -170 -130 -50 -20 -70 290 130 -7 7000 1954 -150 60 -70 -260 -110 -130 -60 -10 -20 190 190 160 -18 7000 1955 220 -110 -100 -60 -10 -90 -110 -50 -40 50 -130 -70 -41 7000 1956 -140 40 -60 -70 -10 -30 -100 -20 -70 -70 120 20 -33 7000 1957 -110 -60 0 10 -130 -120 -70 30 20 10 30 -30 -35 7000 1958 60 0 0 90 -70 -170 -130 -60 80 150 100 50 8 7000 1959 -150 80 -90 -160 -140 -120 20 -160 -150 70 100 170 -45 7000 1960 100 130 -200 -100 -10 -120 -140 -140 -150 -40 30 220 -35 7000 1961 170 10 -60 -120 -100 -110 -70 -60 -80 0 100 -10 -28 7000 1962 -90 70 -110 -170 -170 -110 -40 -20 10 10 200 -60 -41 7000 1963 70 -50 -50 -110 -60 0 -100 10 -30 90 20 150 -4 7000 1964 230 50 -50 0 -170 -110 0 -80 0 30 -70 -70 -20 7000 1965 0 -40 0 -80 -60 -90 -70 -40 -30 80 30 140 -13 7000 1966 170 70 -100 -40 -30 -60 -80 -80 0 -20 -180 120 -19 7000 1967 150 140 -40 -20 -140 -50 10 60 90 140 210 130 56 7000 1968 20 -40 -30 -50 -170 -90 -100 -60 70 100 90 20 -20 7000 1969 -70 120 0 40 130 180 230 260 210 260 110 300 148 7000 1970 -40 240 60 -80 -120 -10 60 0 40 -20 0 60 14 7000 1971 -220 -20 -140 -120 -120 -200 -170 -110 0 70 0 20 -85 7000 1972 70 -200 -70 -150 -120 0 -80 -10 -50 140 180 -10 -24 7000 1973 70 60 0 -50 -10 -80 0 40 20 10 0 90 13 7000 1974 110 -120 -10 -20 -10 -70 -60 -90 -100 -150 130 170 -18 7000 1975 60 40 30 -50 -40 -80 30 10 160 30 50 100 28 7000 1976 130 -80 40 -20 50 -80 -10 20 160 110 170 160 55 7000 1977 220 210 -10 -110 60 -150 -140 -30 0 -10 90 60 15 7000 1978 312831 - 999999999999999 0 50 -110 -170 -100 20 10 180 13099999 7000 1979 31 XX 140 -90 30 -10 -100 -4099999 -60 10 110 170 130 27 7000 1980 31XX 0 180 200 70 60 -90 -90 100 -10 170 15099999 67 7000 1981 320 140 160 50 -10 -10 10 100 0 -50 230 70 84 7000 1982 30 -10 70 -20 -60 -50 50 0 110 -50 120 250 37 7000 1983 120 270 120 130 60 130 50 120 170 180 280 90 142 7000 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Instrumental measurements of the sea level in the Russian Arctic Seas began in the 1920s. Stationary observations began in the Kara Sea (Dickson Island) in 1933, in the Laptev Sea (Tiksi Bay) in 1934, in the Chukchi Sea (Cape Schmidt) in 1935, and in the East- Siberian Sea (Ambarchik Bay) in 1939. There were 53 stations with sea level observational program in the mid 1980s. As a results of economical problems in Russia, many stations were closed in th 1990s, and at present, there are 7,7,5 and 2 stations in the Kara, Laptev, East-Siberian and Chukchi Seas, respectively. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Observations have been conducted according to the Manual for Stations and Gauges of the Hydrometeorological Service (1968). The observations with manual reading have been carried out four times a day with an accuracy of 1 cm. Tide gauge stations have 1-hour frequency of observations, and the same accuracy. Monthly data quality control includes visual data control and statistical control by the Arctic and Antarctic Research Institute (AARI) scientists and administration of RosHydromet. Observations at some stations have had different locations in summer and winter, some of which were interrapted during replacement. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : Therefor a lot of sea level data before 1949-50 in many cases cannot be used because of absence of relible geodetic survey. All stations have one or more geodetic benchmarks installed on stable ground. Periodic (usually annual but for some stations every summer month) geodetic surveys are made to a gauge to determine if any vertical changes in the gauge mount have occurred. The Russian sea level network has a complete geodetic history consisting of Revised Local Reference (RLR) sites. Only 30-40 years ago, the sea level station benchmarks were related to the Baltic System (Kronshtadt gauge) using geodetic methods. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2003Jan23 : The monthly sea level data are calculated using daily data. The mean monthly sea level data based on four measurements per day are very close to the observations with 1-hour interval. It is estimated that the error does not exceed 2 cm with probability of 99.7%. The annual sea level based on 4-hour interval observations coincide with results based on 1- hour observing intervals. VARDO 040001 70 20 N 31 06 E04242008323 44 23 0 0 1947 312831303130313110 5 13 - 9999999999999999999999999999999999999999 3058 3073 2868 279699999 4179 1948 1 1 2 310 2 4 3 5 9 1XX 2878 2852 2934 2812 2701 2794 2735 2812 2933 3042 3084 3124 2890 4179 1949 4 1 8 1 5 1 7 831 7 5XX 3101 3106 2807 2890 2711 2718 2852 2942 294499999 2894 2983 2902 4179 1950 14 1 3 1 2 2 3 4XX 3002 2965 2961 2814 2797 2839 2754 2790 2933 2984 2991 2969 2894 4179 1951 12 1 214313031 1 5 1 - 2955 2806 2849 2752999999999999999 2762 2904 3052 3009 323499999 4179 1952 3 2 303130 8 1 2 1 - 3020 2881 2785999999999999999 2962 2889 3020 2791 2854 282599999 4179 1953 4 6 5 3 4123031 1 - 2947 2762 2894 2734 2731 2668 2755 29589999999999 3073 312699999 4179 1954 1 3130 2 - 3000 2792 2855 27549999999999 2807 2828 2932 3035 2914 300199999 4179 1955 1 4 1 131303131 2 3 1 3 - 3049 2791 2766 282999999999999999999999 2901 3038 2962 289899999 4179 1956 10 1 30 8 9 6 1XX 2867 2617 2854 2689 283399999 2733 2829 2876 2995 2901 2977 2840 4179 1957 7 1 1 2 2 3 6 5 2 4 4XX 3020 2906 2841 2763 2773 2837 2777 2809 2848 3038 3028 3065 2890 4179 1958 1010 2 2 2 1 2 3 2XX 2910 2845 2686 2697 2738 2753 2865 2777 2927 2956 3010 2943 2841 4179 1959 8 93115 8 1 4 9 7 3XX 2858 314599999 2797 2781 2887 2859 2883 2995 2913 2842 2849 2890 4179 1960 2 5 3 11 3 3 2850 2821 2774 2763 2720 2819 2736 2789 2767 2856 2831 2837 2799 4179 1961 5 4 6 5 4 3 531XX 2803 2900 3046 2803 2736 2867 2829 2845 2960 2952 297299999 2880 4179 1962 3 6 1 3 2 3017 2960 2775 2726 2704 2829 2760 2868 2859 3047 2922 2990 2871 4179 1963 1 4 4 1 1 1 7 3303111 4 - 2893 2830 2811 2718 2727 2759 2866 27269999999999 2956 305799999 4179 1964 1 1 930 1 1 2 5 1 1XX f 3112 2875 2794 2712 284599999 2902 2868 2984 2977 3069 3049 2928 4179 1965 1 1 83031 2 1 2 1 - 2893 2864 28589999999999 2835 2859 2781 2817 2983 2903 284899999 4179 1966 431303130313130313031 - 2856 28089999999999999999999999999999999999999999999999999999999 4179 1984 5 1 2 2937 2827 2682 2723 2719 2731 2825 2821 2784 2848 2826 2909 2802 4179 1985 2 2 4 7 214 XX 2791 2741 2718 2764 2648 2745 2743 2759 2847 3050 2912 2959 2801 4179 1986 7 6 2825 2808 2902 2642 2685 2788 2757 2728 2758 2999 2969 2805 2804 4179 1987 31 2 XX 99999 2869 2634 2780 2752 2689 2747 2746 2885 2954 2912 3073 2821 4179 1988 830 XX 2989 2728 2812 2864 2812 2880 2825 2866 2996 311999999 3100 2904 4179 1989 7 14 31 2 2XX 3137 3121 2864 2611 2829 2806 2822 2665 267599999 3039 3162 2885 4179 1990 1 1 2 1 5313130 3 - 2966 3127 3083 2859 2864 2727999999999999999 3008 2962 304499999 4179 1991 1 3 5 2 1 3029 2814 2699 2747 2747 2763 2792 2828 2957 2866 2918 3080 2856 4179 1992 3 1 3 5 3165 3006 2889 2632 2788 2815 2871 2856 2800 2848 2878 3134 2892 4179 1993 2 6 3 2 3265 3012 2898 2707 2662 2758 2716 2739 2779 2845 2821 2889 2841 4179 1994 4 6 2 2 2854 2783 2832 2720 2703 2883 2779 2807 2847 2986 2990 3102 2860 4179 1995 3 3 5 5 1 2980 3066 2812 2794 2691 2714 2884 2897 2818 2984 2917 2934 2877 4179 1996 2942 2799 2732 2726 2703 2791 2815 2748 2778 2978 2972 2846 2819 4179 1997 231 5 4 12XX 3027 2923 2907 2796 2675 271599999 2808 2986 2971 2858 2855 2866 4179 1998 5 7 5 2 2888 2882 2764 2627 2720 2640 2752 2791 2769 2869 2810 3022 2796 4179 1999 2 2874 2887 2700 2773 2696 2757 2851 2828 2904 2934 3032 3044 2856 4179 2000 3080 3044 2940 2731 2774 2792 2714 2807 2847 2841 2783 2948 2858 4179 2002 1 3091 3027 2884 2748 2746 2789 2810 2799 2933 2882 2846 2886 2869 4179 2003 2986 2918 2983 2750 2787 2801 2765 2851 2961 2949 2960 3078 2899 4179 2004 2895 2913 2755 2710 2754 2825 2789 2790 2956 2928 3041 3113 2872 4179 2005 3008 2822 2740 2743 2756 2798 2822 2874 3057 2992 3060 2854 2877 4179 2006 2952 2887 2767 2747 2733 2876 2878 2759 2934 2886 3018 3125 2880 4179 2007 1 3093 2775 2868 2874 2776 2800 2780 2857 2936 3036 2964 3087 2905 4179 2008 2958 3019 2840 2674 2696 2745 2769 2790 2833 3022 2976 2967 2857 4179 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Vardo 040/001 RLR(1964) is 8.9m above BM 03N9 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Vardo 040/001 RLR(1964) is 8.9m above BM 03N9 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-JUL-93 : Value for January 1964 is anomalously low (data checked to be as received from authority). =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1989 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. Values for July and August 2008 suspect due to malfunction a the gauge data to be reviewed and revised if necessary. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset for Vardo now refers to TGBM O3 N18 3.921m above TGZ. A value for RLR 2008 was calculated. VARDO II 040002 70 22 N 31 06 E03249999323 6 0 0 0 1880 31293130 30 - 99999999999999999999 1913 2003 1991 2053 2031 202299999 208999999 99999 1881 28313031 - 208499999999999999999999 2063 2213 2238 2211 2324 2560 249199999 99999 1882 2550 2506 2349 2134 2073 2085 2180 2251 2151 2111 2038 2121 2212 99999 1883 31303131 - 2315 1962 1810 177999999999999999999999 1982 2085 2102 215199999 99999 1884 2213 2112 1961 1862 1876 1958 2021 2022 2157 2228 2226 2150 2065 99999 1885 2107 2076 2049 1894 1934 2068 2064 2025 2122 2048 2202 2335 2077 99999 VADSO 040005 70 04 N 29 45 E04241970 f 19 10 0 0 1969 XX -255 -293 -219 -283 -327 -213 -153 -199 -82 66 28 -152 -173 7209 1970 -161 -210 -334 -337 -323 -199 -165 -194 -139 -68 -107 -20 -188 7209 1971 31 8 XX -63 -231 -275 -290 -262 -23099999 -75 -87 -4 -22 -5 -141 7209 1972 29 4XX XX -19999999 -163 -272 -320 -238 -153 -95 -76 -5 -24 127 -133 7209 1973 -13 -24 -96 -234 -242 -115 -155 -62 -112 -48 42 -84 -96 7209 1974 130 XX -52 -188 -23399999 -284 -167 -22 -108 20 -240 -160 82 -122 7209 1975 6 30 4 XX 2XX 95 89 -42 -246 -22999999 -43 -82 67 -41 27 152 -26 7209 1976 303130 6 - -23 -49 -146999999999999999 -112 -132 -97 -219 -87 -20499999 7209 1977 -234 -246 -229 -279 -340 -179 -269 -287 -155 -232 -147 -189 -232 7209 1978 -213 -426 -339 -343 -357 -273 -292 -280 -222 -117 6 -261 -259 7209 1979 -351 -328 -340 -415 -292 -199 -199 -228 -54 -185 -195 -109 -241 7209 1980 31 XX -301 -168 -335 -267 -297 -221 -26299999 -94 -46 -35 42 -181 7209 1981 14 30 2123031 6 - 39 -173 -308 -199 -30799999 -153 -1489999999999 -29 -18699999 7209 1982 7 XX -209 -109 -267 -202 -299 -294 -188 -188 -54 -208 30 -132 -176 7209 1983 31 XX 99999 -60 -141 -332 -324 -192 -166 -174 -206 48 6 -50 -145 7209 1984 12 -143 -143 -322 -271 -326 -195 -133 -182 -205 -130 -178 -68 -194 7209 1985 3130 - -192 -225 -315 -2419999999999 -249 -144 -56 40 -130 -9199999 7209 1986 631 XX -199 -281 -137 -410 -276 -17899999 -266 -97 47 32 -21 -161 7209 1987 730313130313031 - 2018 1956 1812 1864 18679999999999999999999999999999999999999999 5069 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Vadso 040/005 RLR(1970) is 9.7m below BM AE4N11 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 17-MAR-93 : Possible datum shift in RLR record in the late 1970s. =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Vadso 040/005 RLR(1970) is 9.7m below BM AE4N11 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 10-OCT-94 : 1987 gauge taken out of service BERLEVAG 040011 70 51 N 29 06 E03241943 5 4 0 0 1939 -1555-1423-1669-1659-1780-1613-1672-1638-1582-1558-1479-1524-1594 8500 1940 -1637-1601-1724-1680-1772-1697-1683-1620-1591-1601-1524-1516-1637 8500 1941 30313031 - -1594-1725-1800-1838-1746-1706-1712-17039999999999999999999999999 8500 1943 -1588-1386-1551-1500-1637-1655-1668-1606-1553-1511-1503-1385-1545 8500 1944 3130313031 - -1366-1535-1667-1631-1690-1668-1683999999999999999999999999999999 8500 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Berlevag 040/011 RLR(1943) is 8.5m below FM Berlevag =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Berlevag 040/011 RLR(1943) is 8.5m below FM Berlevag HONNINGSVAG 040015 70 59 N 25 59 E04241972275 38 8 0 0 1970 3128313031 4 2 - 9999999999999999999999999 1355 1392 1376 1434 1527 1494 159999999 5594 1971 1 31303112 1 - 1545 1407 1346 1293 1304 1298 1375999999999999999 1608 160899999 5594 1972 3 1406 1383 1416 1334 1242 1323 1392 1441 1496 1562 1568 1729 1442 5594 1973 13 1 1573 1538 1466 1308 1294 1403 1371 1489 1478 1520 1596 1465 1457 5594 1974 1530 1397 1268 1297 1190 1293 1388 1340 1438 1254 1322 1559 1356 5594 1975 2 1 1 7 1725 1617 1435 1318 1309 1384 1464 1391 1614 1491 1563 1682 1501 5594 1976 4 1538 1505 1363 1360 1244 1326 1344 1400 1428 1338 1495 1390 1394 5594 1977 9 9 2 1355 1318 1364 1284 1210 1305 1274 1268 1421 1420 1591 1463 1353 5594 1978 1481 1239 1329 1212 1218 1283 1257 1294 1370 1497 1662 1376 1352 5594 1979 3 1 5 2 1318 1365 1319 1155 1249 1307 1316 1311 1487 1386 1526 1615 1365 5594 1980 1 3 1407 1419 1236 1319 1256 1431 1375 1412 1514 1545 1527 1546 1416 5594 1981 3 3 1511 1460 1324 1341 1237 1350 1367 1381 1429 1441 1593 1437 1405 5594 1982 3 3 1498 1530 1390 1403 1283 1287 1403 1400 1522 1427 1662 1657 1455 5594 1983 3 1 9 4 1735 1490 1455 1252 1259 1377 1411 1473 1476 1636 1649 1574 1480 5594 1984 3 1523 1438 1248 1297 1275 1330 1365 1347 1347 1427 1386 1464 1372 5594 1986 9 2 1 114 8 4 1 XX 1418 1331 1491 1253 1361 1442 1444 1356 1471 1691 1679 1565 1464 5594 1987 3 3130 - 1448 1431 1244 1328 1285 1258 13459999999999 1534 1456 158499999 5594 1988 52931 3 8 14 2 8 5 - 15219999999999 1340 1218 1369 1376 1383 1504 1548 1674 164899999 5594 1989 9 1 3 6 9313031 - 1776 1765 1536 1311 1464 1422 1486999999999999999 1613 171999999 5594 1990 1597 1756 1675 1463 1415 1340 1382 1439 1437 1600 1534 1656 1523 5594 1991 3015 XX 1634 1399 1301 1351 134099999 1370 1440 1540 1459 1545 1674 1464 5594 1992 1 1 1731 1591 1491 1259 1372 1380 1449 1463 1404 1422 1484 1730 1481 5594 1993 1 4 1858 1611 1460 1299 1255 1327 1328 1348 1362 1413 1426 1511 1434 5594 1994 2 611 1462 1339 1459 1317 1310 1454 1360 1385 1492 1568 1589 1717 1456 5594 1995 1581 1666 1452 1356 1289 1338 1458 1474 1411 1579 1496 1511 1467 5594 1996 1519 1392 1325 1313 1281 1387 1377 1329 1369 1574 1575 1430 1406 5594 1997 1593 1541 1507 1388 1281 1298 1250 1378 1566 1578 1465 1494 1444 5594 1998 1 1516 1535 1383 1236 1317 1264 1386 1386 1359 1477 1448 1638 1412 5594 1999 1511 1512 1314 1352 1295 1364 1473 1435 1521 1545 1679 1641 1470 5594 2000 1698 1648 1511 1309 1358 1385 1310 1396 1429 1438 1393 1557 1452 5594 2001 1564 1436 1382 1353 1363 1338 1391 1433 1406 1555 1604 1503 1444 5594 2002 1675 1658 1477 1351 1328 1373 1397 1383 1534 1449 1435 1457 1459 5594 2003 1569 1504 1551 1327 1369 1383 1369 1418 1534 1549 1565 1660 1483 5594 2004 5 1499 1502 1359 1316 1338 1409 1397 1385 1559 1513 1626 1737 1472 5594 2005 1651 1423 1337 1351 1367 1388 1416 1471 1648 1593 1656 1460 1480 5594 2006 1561 1482 1345 1371 1332 1450 1451 1367 1505 1480 1642 1727 1476 5594 2007 1 1683 1389 1467 1461 1394 1374 1379 1445 1534 1628 1588 1679 1503 5594 2008 5 1562 1615 1442 1262 1284 1333 1349 1371 1414 1626 1599 1569 1453 5594 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Honningsvag 040/015 RLR(1972) is 13.1m below BM FMI =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Honningsvag 040/015 RLR(1972) is 13.1m below BM FMI =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1988 HAMMERFEST 040021 70 40 N 23 40 E04241964 52 24 0 0 1955 31283130313031 - 99999999999999999999999999999999999 1214 1216 1314 1265 127099999 99999 1956 3130313031 - 1195 9799999999999999999999999999 1368 1424 1538 1496 156999999 99999 1957 3 4 1 1 2090 1884 1880 1793 1734 1825 1789 1853 1871 2105 2047 2110 1915 6945 1958 9 2 1934 1898 1725 1751 1756 1784 1890 1824 1931 2001 2060 2008 1878 6945 1959 91413 1 4XX 1951 2171 2073 1777 1793 1897 1900 1874 1979 1985 1925 1929 1930 6945 1960 4 1 7 1872 1826 1738 1759 1739 1813 1793 1817 1821 1823 1856 1872 1811 6945 1961 2 8 31 6 XX 1865 1944 2100 1813 1782 1929 179699999 1976 1999 2072 2087 1938 6945 1962 2831 - 20599999999999 1737 1711 1842 1746 1851 1891 2093 1920 197899999 6945 1963 6 5 9 2 1888 1910 1790 1746 1745 1782 1798 1793 1897 2036 1985 2054 1870 6945 1964 1 1 3 1 7 3 2 2103 1932 1781 1730 1925 1903 1898 1839 1997 1985 2047 2041 1930 6945 1965 1 5 13031 3 - 1872 1797 1813 1754 1673 1779 1848 17629999999999 1934 187599999 6945 1966 102831303114 3 - 191199999999999999999999 1756 1885 1862 2029 1859 1894 191799999 6945 1967 931303130 30313031 - 1839 196299999999999999999999 1899 18709999999999999999999999999 6945 1968 31293130313031 - 99999999999999999999999999999999999 1927 1801 1886 1907 200299999 6945 1969 831303130 1 1 - 1806 183799999999999999999999 1846 1805 1962 2127 2046 186999999 6945 1970 XX -162 -201 -230 -260 -271 -131 -75 -131 -135 -64 -36 57 -136 6945 1971 3113 2 9 1 XX 99999 1774 1789 1748 1782 1760 1861 1943 1941 2039 2039 2061 1895 6945 1972 1 1 1854 1851 1864 1788 1685 1803 1870 1919 1980 2059 2083 2221 1915 6945 1973 30 3 1 2XX 2096 2060 198199999 1807 1925 1900 2004 1923 2000 2060 1984 1977 6945 1974 1 2006 1861 1722 1755 1657 1786 1893 1799 1961 1805 1885 2155 1857 6945 1975 5 2168 2066 1940 1790 1775 1848 1940 1843 2085 1951 2033 2166 1969 6945 1977 1826 1762 1826 1748 1666 1754 1719 1683 1890 1897 1986 1901 1805 6945 1978 6 1921 1689 1784 1672 1679 1757 1694 1755 1850 1960 2129 1832 1811 6945 1979 15 1825 1836 1791 1629 1739 1859 1839 1812 1983 1876 1996 2031 1844 6945 1980 2 1871 1896 1731 1785 1708 1764 1686 1762 1849 1904 1923 2000 1823 6945 1981 31XX 1960 1915 1759 1765 1643 1781 1797 1802 1837 1836 204499999 1830 6945 1983 8 4 2222 1939 1925 1738 1765 1869 1911 1983 1965 2120 2155 2077 1976 6945 1984 4 2 3 2073 1945 1732 1805 1775 1763 1851 1837 1848 1944 1906 1997 1875 6945 1985 9 6 9 1862 1836 1826 1823 1698 1782 1794 1895 2009 2089 1968 1998 1883 6945 1986 1875 1747 1948 1657 1787 1837 1860 1753 1875 2127 2095 1984 1880 6945 1987 1854 1840 1671 1752 1720 1676 1774 1755 1893 1969 1919 2008 1819 6945 1988 8 8 1962 1790 1886 1853 1764 1851 1856 1835 1983 2057 2140 2128 1930 6945 1989 2255 2232 1986 1749 1892 1833 1905 1914 2035 2029 2033 2137 1999 6945 1990 3130 3 - 2035 2176 2080 1857 1791 1715 17769999999999 2065 1991 212699999 6945 1991 1 1 1 2 2097 1845 1764 1812 1788 1818 1852 1892 2000 1926 2010 2139 1911 6945 1992 1 6 2185 2064 1958 1736 1825 1843 1902 1935 1854 1875 1954 2191 1939 6945 1993 3 4 1 3 2322 2064 1923 1751 1699 1759 1785 1799 1818 1852 1891 1979 1889 6945 1994 1 31 1 1XX 1923 1795 1922 176299999 1904 1814 1858 1894 2028 2063 2186 1923 6945 1995 3 3 8 4 2065 2118 1916 1800 1729 1808 1924 1927 1867 2032 1947 1958 1923 6945 1996 1965 1847 1775 1758 1712 1834 1805 1768 1816 2030 2035 1881 1852 6945 1997 2034 2007 1958 1831 1726 1741 1691 1829 2024 2033 1934 1951 1896 6945 1998 1979 2016 1847 1690 1759 1725 1841 1844 1804 1939 1911 2093 1870 6945 1999 1987 1973 1774 1795 1742 1811 1924 1881 1978 1998 2163 2108 1927 6945 2000 2155 2106 1952 1746 1807 1835 1750 1833 1877 1893 1852 2011 1901 6945 2001 2 2021 1894 1835 1806 1815 1785 1837 1882 1856 2010 2082 1966 1899 6945 2002 4 7 2 2137 2140 1937 1810 1767 1810 1862 1896 2043 1927 1925 1943 1936 6945 2003 3111 XX 2061 1997 2034 1809 1863 186799999 1849 1981 2012 2026 2119 1969 6945 2004 1966 1955 1827 1778 1789 1853 1844 1827 2014 1972 2088 2210 1927 6945 2005 1 2130 1877 1787 1806 1819 1833 1862 1921 2108 2048 2119 1926 1937 6945 2006 4 1 1 2022 1930 1778 1812 1779 1892 1901 1807 1946 1931 2109 2185 1926 6945 2007 1 2137 1849 1912 1903 1851 1822 1826 1896 1993 2094 2051 2144 1958 6945 2008 2027 2074 1904 1718 1739 1780 1798 1820 1860 2092 2059 2024 1908 6945 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Hammerfest 040/021 RLR(1964) is 9.8m below BM U3N23 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Hammerfest 040/021 RLR(1964) is 9.8m below BM U3N23 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1990 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 27-Oct-2009 : The Norwegian Mapping Authority have revised their datasets The benchmark reference for Hammerfest is U3 N25 which is 8.655m above TGZ. As a result the value of RLR has changed to 6945. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The PSMSL dataset begins in Jan 1957. Apparently there is earlier data on the Norwegian database but according to the site sheet the data before 1957 should not be used in any analysis. TROMSO 040031 69 39 N 18 58 E04241964 57 8 0 0 1952 31293130 2 - 99999999999999999999 1392 1529 1515 1477 1538 1437 1489 150699999 5484 1953 1602 1435 1492 1411 1400 1361 1437 1474 1496 1628 1771 1739 1521 5484 1954 2 4 1607 1490 1492 1422 1289 1470 1460 1475 1646 1711 1595 1786 1536 5484 1955 11 1729 1448 1464 1409 1406 1420 1438 1459 1525 1600 1547 1614 1509 5484 1956 1 10 1 1502 1282 1398 1312 1421 1404 1368 1413 1429 1614 1528 1590 1439 5484 1957 5 1658 1533 1439 1403 1333 1420 1378 1412 1461 1686 1610 1692 1504 5484 1958 1591 1502 1319 1342 1379 1351 1467 1414 1477 1608 1661 1633 1479 5484 1959 1523 1688 1578 1410 1341 1484 1441 1471 1556 1564 1538 1504 1507 5484 1960 1113 4 1449 1450 1374 1359 1332 1389 1367 1409 1383 1377 1464 1508 1409 5484 1961 7 33010 1 5 XX 1472 1539 1665 1423 137599999 1479 1475 1563 1576 1669 1645 1537 5484 1962 2 3 1656 1539 1342 1325 1317 1428 1353 1434 1456 1639 1538 1572 1466 5484 1963 1 1450 1416 1378 1304 1355 1365 1423 1382 1520 1643 1565 1639 1454 5484 1964 4 1674 1495 1363 1367 1458 1478 1528 1467 1577 1592 1706 1670 1530 5484 1965 1544 1417 1427 1377 1303 1453 1430 1377 1462 1560 1538 1506 1450 5484 1966 1459 1419 1412 1262 1373 1385 1494 1468 1572 1472 1535 1526 1448 5484 1967 1447 1545 1712 1448 1356 1486 1497 1469 1555 1720 1647 1604 1541 5484 1968 1544 1505 1564 1380 1259 1447 1372 1442 1364 1481 1473 1595 1452 5484 1969 1429 1429 1396 1349 1290 1396 1465 1398 1543 1698 1673 1505 1464 5484 1970 1454 1435 1402 1360 1303 1333 1419 1382 1435 1539 1511 1570 1429 5484 1971 1 1585 1464 1361 1360 1368 1411 1439 1507 1477 1591 1600 1651 1484 5484 1972 2 2 2 1423 1406 1433 1367 1285 1398 1425 1474 1519 1603 1654 1737 1477 5484 1973 2 1578 1590 1497 1380 1364 1479 1421 1505 1466 1501 1622 1563 1497 5484 1974 1609 1492 1311 1324 1274 1384 1483 1424 1531 1355 1437 1712 1445 5484 1975 1690 1552 1456 1325 1329 1398 1475 1415 1622 1498 1563 1725 1504 5484 1976 8 1587 1523 1391 1360 1325 1398 1436 1492 1525 1434 1582 1458 1457 5484 1977 10 1 1 1456 1402 1418 1356 1254 1358 1382 1380 1464 1489 1580 1511 1421 5484 1978 3 1509 1274 1389 1234 1280 1411 1306 1270 1335 1427 1625 1350 1369 5508 1979 1 1 1331 1 XX 1337 1372 1352 1163 1289 1320 133499999 1506 1445 1568 1622 1395 5508 1980 2 1423 1422 1359 1452 1375 1354 1259 1320 1421 1485 1494 1560 1410 5508 1981 4 4 1536 1422 1389 1401 1285 1383 1407 1416 1462 1507 1629 1522 1448 5508 1982 1477 1532 1435 1428 1319 1303 1417 1437 1547 1475 1706 1692 1480 5508 1983 1775 1446 1466 1306 1333 1400 1458 1513 1506 1666 1667 1607 1513 5508 1984 3113 XX 1589 1455 1279 1327 1312 136299999 1429 1376 1477 1447 1521 1416 5508 1985 2 1295 1310 1286 1242 1148 1255 1297 1353 1407 1511 1434 1456 1333 5508 1986 313031 - 1374 1233 1447 1193999999999999999 1367 1513 1690 1655 155499999 5508 1987 1 6 2 1439 1516 1314 1352 1311 1308 1365 1354 1475 1544 1476 1735 1430 5508 1988 5 6 1031303131 - 1518 1389 1368 140199999999999999999999 1557 1624 1737 172299999 5508 1989 2 4 3 1864 1826 1609 1371 1516 1463 1466 1510 1612 1614 1613 1701 1596 5508 1990 9 1666 1797 1676 1452 1367 1358 1395 1459 1454 1619 1525 1672 1538 5508 1991 1639 1366 1320 1363 1330 1390 1393 1437 1536 1459 1580 1664 1457 5508 1992 9 14 3 1691 1604 1498 1303 1363 1341 1446 1487 1362 1412 1552 1735 1491 5508 1993 3 6 3 1854 1569 1458 1289 1245 1307 1363 1356 1340 1366 1419 1536 1428 5508 1994 1463 1307 1485 1309 1302 1467 1347 1391 1441 1580 1589 1727 1452 5508 1995 14 1598 1682 1472 1336 1296 1346 1432 1456 1404 1607 1513 1495 1476 5508 1996 2 9 7 1502 1395 1303 1309 1249 1397 1378 1320 1402 1577 1579 1428 1404 5508 1997 6 4 1564 1555 1509 1383 1293 1336 1252 1376 1565 1573 1486 1493 1448 5508 1998 2 4 1544 1613 1411 1248 1319 1310 1417 1411 1369 1518 1490 1643 1439 5508 1999 7 1 1567 1545 1347 1329 1313 1368 1460 1414 1522 1547 1729 1657 1486 5508 2000 1 1685 1643 1481 1274 1362 1402 1306 1382 1421 1452 1430 1576 1451 5508 2001 1553 1436 1374 1343 1354 1340 1372 1417 1395 1560 1642 1480 1439 5508 2002 1667 1700 1470 1355 1346 1379 1399 1387 1522 1435 1431 1418 1458 5508 2003 1557 1457 1496 1298 1378 1397 1372 1394 1511 1553 1563 1645 1469 5508 2004 1 1511 1482 1362 1326 1335 1391 1400 1369 1546 1501 1614 1747 1465 5508 2005 1682 1392 1313 1357 1376 1394 1409 1453 1635 1586 1648 1475 1477 5508 2006 2 1553 1451 1298 1382 1330 1419 1411 1341 1477 1469 1676 1736 1460 5508 2007 1687 1413 1445 1439 1422 1356 1395 1432 1520 1602 1574 1659 1495 5508 2008 1569 1612 1447 1267 1279 1338 1322 1345 1375 1653 1598 1540 1445 5508 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Tromso 040/031 RLR(1964) is 12.8m below BM "Trafokiosk" =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Tromso 040/031 RLR(1964) is 12.8m below BM "Trafokiosk" =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1986 ANDENES 040041 69 19 N 16 09 E04241991322 46 11 0 0 1938 -31 -194 -73 -285 -360 -256 -311 -205 -201 -43 90 -105 -165 7300 1939 -116 -41 -297 -265 -414 -279 -327 -354 -270 -235 -47 -130 -231 7300 1940 -207 -282 -275 -381 -405 -365 -383 -262 -186 -250 -121 -120 -270 7300 1941 -234 -256 -360 -429 -355 -323 -333 -92 -249 -210 -281 -110 -269 7300 1942 28 XX -30999999 -270 -318 -308 -205 -235 -218 -97 -18 -22 65 -188 7300 1943 -351 -204 -359 -289 -462 -491 -491 -404 -253 -77 -113 -125 -302 7300 1944 30 XX 53 -167 -247 -286 -359 -329 -373 -266 -268 -17899999 -106 -218 7300 1945 -227 -105 -224 -229 -359 -325 -465 -295 -265 -116 -156 -119 -240 7300 1946 3031 - -85 -186 -211 -222 -365 -259 -294 -255 -119 -87999999999999999 7300 1947 -262 -326 -258 -177 -403 -291 -257 -277 -83 -60 -134 -159 -224 7300 1948 30 XX -186 -257 -187 -284 -394 -335 -377 -300 -125 -3099999 88 -217 7300 1949 91 81 -312 -221 -332 -400 -372 -283 -206 -49 -108 9 -175 7300 1950 -190 -116 -30 -130 -269 -176 -269 -281 -20 111 62 0 -109 7300 1951 31 XX -9 -150 -172 -183 -359 -327 -20899999 -169 -111 -154 86 -160 7300 1952 -81 -189 -327 -319 -437 -351 -417 -404 -231 -316 -270 -211 -296 7300 1953 -166 -295 -236 -300 -392 -518 -351 -288 -202 -60 43 -45 -234 7300 1954 -178 -259 -252 -395 -553 -349 -441 -419 -215 -125 -177 -53 -285 7300 1955 28 313031 - -23099999 -328 -398 -436 -457 -378 -334 -17799999999999999999999 7300 1974 XX XX -63 -223 -419 -382 -417 -315 -235 -272 -152 -318 -214 43 -247 7300 1975 XXXX XX 25 -133 -235 -363 -382 -309 -249 -314 -75 -149 -72 72 -182 7300 1976 9 -103 -141 -280 -314 -382 -341 -314 -277 -267 -278 -132 -243 -260 7300 1977 XX XX -90 -137 -83 -173 -278 -168 -197 -189 -62 6 92 37 -104 7218 1978 XX 23031 - 27 -206 -85 -261 -247 -170 -194 -165 -88 28999999999999999 7218 1982 XX -42 -19 -82 -144 -236 -256 -101 -95 23 -30 205 139 -55 7218 1983 313130 - 282 -81 -36 -168 -155 -91999999999999999 158 146 13799999 7218 1984 31 31 23130 313031 - 99999 399999 -1609999999999 -106 -116 -12099999999999999999999 7218 1985 3128313031 30313031 - 9999999999999999999999999 -243 -156 -959999999999999999999999999 7218 1986 312831 83031 - 999999999999999 -353 -188 -196 -162 -267 -148 27999999999999999 7218 1991 3128313031303131303112 - 99999999999999999999999999999999999999999999999999 2107 213899999 5218 1992 2151 2080 1977 1804 1844 1853 1915 1976 1913 1908 2056 2223 1975 5218 1993 2340 2039 1947 1798 1735 1795 1858 1863 1846 1856 1920 2066 1922 5218 1994 9 1987 1808 2024 1829 1807 1961 1835 1889 1942 2056 2083 2219 1954 5218 1995 2100 2197 1976 1826 1798 1816 1904 1924 1894 2114 2010 1980 1960 5218 1996 1994 1892 1786 1817 1748 1873 1859 1809 1837 2061 2063 1923 1888 5218 1997 2 2049 2108 2014 1883 1808 1811 1742 1869 2058 2073 1987 2000 1950 5218 1998 14 2039 2152 1926 1758 1821 1804 1920 1925 1882 2054 2021 2128 1945 5218 1999 3 2 2 2086 2064 1868 1847 1821 1855 1950 1902 2018 2059 2229 2166 1991 5218 2000 2163 2146 1970 1757 1860 1872 1786 1875 1917 1961 1973 2104 1948 5218 2001 2059 1950 1891 1855 1849 1839 1871 1915 1915 2083 2153 1980 1947 5218 2002 2175 2219 1980 1866 1850 1879 1924 1907 2010 1945 1949 1927 1968 5218 2003 4 2074 1959 1983 1792 1893 1896 1872 1896 2024 2051 2072 2136 1969 5218 2004 2045 1991 1888 1853 1849 1889 1909 1879 2045 2011 2120 2269 1979 5218 2005 2208 1894 1832 1875 1890 1895 1898 1971 2129 2080 2144 2003 1985 5218 2006 2078 1952 1809 1915 1840 1913 1906 1852 1999 1980 2214 2258 1976 5218 2007 2204 1938 1956 1923 1926 1844 1897 1938 2033 2106 2088 2171 2003 99999 2008 2097 2127 1980 1803 1793 1845 1829 1858 1892 2197 2126 2067 1967 99999 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Andenes 040/041 RLR(1955) is 7.3m below FM AndenesI =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Andenes 040/041 RLR(1955) is 7.3m below FM AndenesI =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1991 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. RISOYHAMN 040051 68 58 N 15 39 E03249999 2 0 0 0 1955 31283130313031 - 99999999999999999999999999999999999-5068-4985-4816-4785-464399999 99999 1956 3031 - -4755-4966-4873-4958-4834-4858-4931-4924-4942-4785999999999999999 99999 HARSTAD 040061 68 48 N 16 33 E04241964 57 8 0 0 1952 3129 4 - 9999999999 1525 1558 1479 1616 1602 1585 1647 1562 1597 162599999 5434 1953 1724 1561 1602 1548 1502 1454 1557 1579 1610 1707 1861 1825 1628 5434 1954 1 1668 1576 1585 1491 1402 1549 1585 1584 1700 1749 1689 1803 1616 5434 1955 1697 1552 1559 1478 1509 1507 1529 1528 1641 1707 1678 1745 1595 5434 1956 1610 1371 1478 1418 1518 1478 1449 1491 1510 1667 1598 1673 1523 5434 1957 1734 1621 1537 1439 1393 1490 1473 1514 1558 1780 1681 1789 1584 5434 1958 1663 1596 1425 1442 1472 1445 1556 1524 1580 1711 1738 1723 1573 5434 1959 1611 1741 1635 1518 1431 1549 1534 1559 1639 1646 1625 1609 1590 5434 1960 1617 1628 1493 1541 1429 1493 1481 1533 1502 1469 1561 1603 1529 5434 1961 1553 1639 1734 1501 1481 1603 1565 1580 1661 1682 1769 1741 1626 5434 1962 1753 1581 1422 1392 1399 1495 1440 1528 1550 1725 1610 1658 1546 5434 1963 1517 1507 1468 1396 1434 1429 1496 1474 1611 1717 1654 1705 1534 5434 1964 1733 1573 1437 1454 1531 1544 1589 1541 1659 1648 1780 1752 1604 5434 1965 7 2 2 1 1612 1508 1495 1429 1384 1514 1507 1467 1540 1646 1625 1608 1529 5434 1966 3128313031303131 7 4 - 9999999999999999999999999999999999999999 1675 1569 1618 165299999 5434 1967 1523 1639 1802 1519 1466 1557 1590 1560 1646 1836 1743 1705 1632 5434 1968 2 3 1645 1578 1661 1474 1366 1518 1447 1489 1442 1552 1535 1660 1531 5434 1969 1533 1509 1479 1435 1370 1465 1542 1478 1630 1769 1767 1590 1547 5434 1970 1522 1493 1440 1399 1368 1427 1548 1516 1565 1649 1622 1657 1518 5434 1971 3 7 1697 1568 1435 1426 1436 1472 1512 1594 1567 1693 1685 1743 1573 5434 1972 413 830 1 1 XX 1505 1475 1498 1408 136999999 1489 1560 1600 1676 1762 1831 1573 5434 1973 10 2 1652 1674 1574 1452 1440 1537 1500 1570 1551 1580 1698 1658 1575 5434 1974 2 1701 1565 1349 1371 1355 1470 1579 1519 1633 1462 1552 1822 1530 5434 1975 312831 - 999999999999999 1407 1396 1465 1530 1473 1690 1616 1675 183499999 5434 1976 7 1 5313031 7 - 1693 1580 1491 1527999999999999999 1472 1495 1500 1619 152099999 5434 1977 1515 1454 1506 1439 1319 1432 1434 1414 1553 1600 1686 1617 1497 5434 1978 2 1603 1369 1488 1330 1337 1443 1379 1363 1440 1512 1691 1389 1445 5445 1979 3 9 111 1 1425 1449 1499 1248 1376 1412 1460 1466 1602 1500 1654 1680 1481 5445 1980 7 831303130313130 30 5 - 1456 147399999999999999999999999999999999999 156599999 167899999 99999 1981 4 3 830 5 5 3 XX 1588 1506 145399999 1349 1422 1456 1462 1519 1577 1668 1568 1511 5445 1982 2 4 1 4 6 1533 1619 1521 1500 1408 1383 1492 1515 1636 1569 1788 1776 1565 5445 1983 2 4 6 6 1 1867 1526 1558 1398 1424 1475 1526 1572 1612 1767 1759 1712 1605 5445 1984 2 3 1663 1523 1338 1411 1385 1426 1451 1444 1455 1567 1531 1588 1481 5445 1985 2 5 4 1456 1445 1439 1406 1320 1403 1453 1527 1556 1662 1583 1613 1490 5445 1986 13 6 510 2 XX 1460 1311 1543 1278 1450 1432 1507 1416 1533 1732 1725 1639 1505 5445 1987 2 1463 1520 1347 1397 1360 1361 1391 1416 1523 1586 1554 1672 1464 5445 1988 3129313031 8 2 - 9999999999999999999999999 1441 1480 1505 1640 1635 1769 176699999 5445 1989 1902 1869 1650 1408 1541 1495 1516 1607 1686 1705 1693 1792 1655 5445 1990 5 4 9303130313130 - 1772 1894 1735999999999999999999999999999999 1690 1595 173099999 5445 1991 1700 1426 1401 1434 1397 1467 1456 1509 1605 1522 1667 1716 1526 5445 1992 1734 1662 1560 1383 1422 1441 1511 1566 1496 1491 1630 1803 1558 5445 1993 1916 1614 1522 1376 1323 1401 1458 1452 1426 1439 1491 1638 1505 5445 1994 1550 1372 1575 1393 1383 1536 1411 1468 1511 1638 1656 1793 1525 5445 1995 1670 1766 1552 1406 1378 1402 1488 1505 1474 1696 1586 1550 1538 5445 1996 3 1557 1464 1364 1394 1332 1460 1453 1396 1415 1635 1633 1496 1466 5445 1997 1622 1680 1585 1459 1379 1403 1346 1441 1631 1639 1553 1556 1523 5445 1998 31 3 8 XX 1611 171699999 1333 1378 1393 1510 1505 1461 1613 1572 1708 1532 5445 1999 1639 1617 1428 1420 1387 1427 1518 1478 1585 1617 1784 1727 1552 5445 2000 1735 1714 1541 1342 1427 1459 1385 1458 1490 1528 1523 1659 1521 5445 2001 1611 1512 1461 1426 1419 1422 1450 1498 1482 1644 1724 1548 1516 5445 2002 1734 1785 1547 1429 1421 1472 1489 1470 1585 1515 1513 1492 1536 5445 2003 1644 1512 1547 1364 1460 1481 1459 1485 1580 1616 1625 1714 1541 5445 2004 1596 1554 1446 1410 1420 1470 1481 1457 1613 1573 1671 1813 1542 5445 2005 1764 1453 1390 1435 1452 1463 1485 1544 1699 1649 1714 1564 1552 5445 2006 1627 1521 1378 1473 1419 1478 1476 1432 1564 1552 1761 1807 1540 5445 2007 1768 1504 1513 1490 1491 1431 1486 1513 1601 1662 1650 1725 1570 5445 2008 1655 1692 1546 1370 1363 1434 1415 1440 1452 1747 1677 1615 1534 5445 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Harstad 040/061 RLR(1964) is 9.8m below BM "Puller" =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Harstad 040/061 RLR(1964) is 9.8m below BM "Puller" =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1988 EVENSKJAER 040071 68 35 N 16 33 E03241964 24 4 0 0 1947 31 XX -2446-2607-2503-2433-2680-256499999-2638-2306-2305-2332-2371-2468 9400 1948 -2392-2482-2331-2465-2507-2438-2434-2405-2300-2218-2221-2108-2358 9400 1949 31XX -2119-2148-2450-2344-2458-2493-2462-2384-2373-2196-226299999-2308 9400 1950 -2386-2231-2317-2380-2516-2370-2441-2423-2210-2189-2264-2298-2335 9400 1951 -2363-2447-2460-2480-2612-2530-2442-2487-2396-2310-2361-2139-2419 9400 1952 -2297-2439-2498-2462-2541-2399-2427-2461-2371-2460-2417-2364-2432 9400 1953 -2207-2447-2390-2435-2488-2556-2439-2414-2382-2267-2114-2151-2364 9400 1954 -2320-2411-2413-2509-2620-2491-2476-2481-2352-2281-2364-2238-2413 9400 1955 -2353-2494-2488-2564-2537-2545-2506-2474-2376-2314-2348-2285-2440 9400 1956 -2345-2668-2513-2616-2485-2517-2544-2514-2480-2324-2402-2327-2478 9400 1957 -2273-2340-2481-2583-2589-2492-2520-2482-2435-2204-2304-2193-2408 9400 1958 -2328-2392-2591-2558-2515-2552-2451-2483-2420-2281-2269-2308-2429 9400 1959 54 144 41 -91 -172 -53 -62 -28 43 49 26 -31 -7 7009 1960 -111 -120 -229 -174 -250 -156 -171 -121 -147 -174 -84 -34 -148 7009 1961 -85 2 96 -127 -147 -17 -61 -59 25 64 235 110 3 7009 1962 31XX 135 -47 -193 -255 -209 -78 -207 -104 -82 139 3599999 -108 7009 1963 3128313031303131 - 9999999999999999999999999999999999999999 148 82 5 5699999 7009 1964 5 76 -98 -241 -224 -160 -155 -92 82 39 37 165 118 -38 7009 1965 -14 -154 -138 -225 -263 -143 -113 -50 -6 11 -7 -28 -94 7009 1966 -110 -139 -107 -258 -171 -149 -28 -42 52 -11 -37 54 -79 7009 1967 -62 43 202 -71 -133 -49 -137 -144 -55 136 50 28 -16 7009 1968 10 2XX -41 -3 -17 -188 -310 -161 -215 -140 -200 -99 -129 -3 -129 7009 1969 31 6 93131 31 - 99999 -235 -188 -248 -293 -2369999999999 32 168 1719999999999 7009 1970 3128313031 1031 - 9999999999999999999999999 -141 30 -83 -16 137 269999999999 7009 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Evenskjaer 040/071 RLR(1964) is 9.4m below BM M9 N23 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Evenskjaer 040/071 RLR(1964) is 9.4m below BM M9 N23 NARVIK 040081 68 26 N 17 25 E04242008 75 19 0 0 1928 31 30 - f 99999-3958-3768-4148-3938-3838-3718-381899999-4088-4148-414899999 10965 1929 f -4368-4328-3944-4149-4109-4031-3963-3933-3851-3704-3650-3517-3962 10965 1930 3128XXXXXXXXXXXXXXXXXXXX - 9999999999-3947-4125-4000-3953-4089-4035-4027-3807-3675-381599999 10965 1931 31283130313031 5 2 - 99999999999999999999999999999999999 1983 2031 2264 2149 223299999 5119 1932 15 4 8 2420 2052 1998 1948 1833 1910 2051 2084 2269 2213 2212 2359 2112 5119 1933 1 3 2276 2080 2017 1970 1846 1878 2035 2066 2012 2144 2059 2136 2043 5119 1934 1 4 2358 2186 1945 1852 2018 1938 1943 1956 2030 2294 2237 2107 2071 5119 1935 2 31 XX 2091 2197 1934 1861 1841 196199999 2038 1971 2137 2092 2046 2015 5119 1936 303111 8313031 - 2044 1982 1911 1865 18209999999999 2092 212199999999999999999999 5119 1937 2164 2053 1815 1840 1884 1988 1979 1976 2082 2166 2195 1989 2010 5119 1938 1 1 3130 - 2248 1988 2150 1992 1930 2060 2001 2097 20929999999999 211399999 5119 1939 3114 XX 2074 2221 1954 197799999 1987 1979 1955 2022 2037 2234 2162 2056 5119 1940 1 303130313130313031 - 2042 1965 194799999999999999999999999999999999999999999999999999 5119 1947 31283130 3131 7 - 99999999999999999999 1739 18769999999999 2169 2137 2036 200699999 5119 1948 1 1963 1919 2030 1925 1863 1954 1921 1937 2058 2165 2200 2319 2021 5119 1949 9 6 4 6 3 3 2 XX 2314 2279 1907 2096 1946 1873 1925 1986 2012 2202 2096 2193 2060 5119 1950 1 3 2064 2155 2099 2038 1896 2054 1917 1922 2176 2228 2158 2093 2065 5119 1951 3 1 11 2026 1955 1978 1952 1790 1882 2006 1960 2106 2193 2100 2341 2020 5119 1952 1 5 3 8 2197 2051 1914 1991 1855 2039 2053 2002 2042 1934 1970 1998 2004 5119 1953 2 2139 1933 2061 1989 1922 1843 1951 1965 2019 2173 2356 2309 2057 5119 1954 2118 2006 2001 1903 1797 1972 1966 1939 2111 2198 2129 2241 2032 5119 1955 2 1 2135 1956 1965 1877 1891 1891 1967 1975 2040 2119 2064 2130 2001 5119 1956 4 1 1965 1742 1875 1803 1948 1952 1884 1878 1918 2094 2028 2119 1934 5119 1957 2164 2042 1964 1857 1823 1925 1882 1913 1944 2218 2133 2246 2009 5119 1958 2104 2037 1822 1860 1889 1855 1985 1922 1993 2151 2176 2119 1993 5119 1959 4 5 1963 2175 2027 1846 1792 1944 1944 1986 2076 2048 1999 1986 1980 5119 1960 62911 2 XX 192399999 1794 1864 1784 1894 1876 1881 1858 1834 1896 1988 1874 5119 1961 1 1958 2061 2130 1903 1857 1989 1968 1955 2063 2097 2166 2116 2022 5119 1962 2160 1986 1832 1783 1799 1917 1819 1903 1942 2175 2040 2090 1954 5119 1963 1942 1959 1879 1804 1857 1848 1918 1871 2066 2183 2087 2146 1964 5119 1964 2224 2026 1859 1863 1960 1975 2062 1986 2111 2100 2224 2189 2048 5119 1965 2031 1893 1922 1848 1762 1883 1886 1806 1907 2076 2033 1996 1921 5119 1966 1918 1878 1893 1715 1801 1847 1997 1960 2054 1981 2059 2055 1930 5119 1967 1 1921 2039 2212 1912 1820 1958 2012 1969 2022 2227 2155 2116 2030 5119 1968 2019 1974 2065 1866 1712 1903 1828 1906 1806 1901 1917 2081 1915 5119 1969 1 1939 1870 1863 1823 1720 1840 1966 1842 2015 2195 2181 1976 1936 5119 1970 1907 1862 1815 1751 1719 1819 1944 1899 1963 2086 2005 2058 1903 5119 1971 1 2099 1961 1812 1811 1822 1851 1925 2014 2011 2134 2118 2181 1979 5119 1972 1876 1853 1898 1831 1721 1860 1919 1999 2033 2134 2160 2267 1963 5119 1973 1 1 2067 2089 2000 1845 1811 1943 1912 2029 1940 1992 2119 2075 1984 5119 1974 2128 1953 1746 1770 1736 1859 1980 1942 2046 1849 1924 2225 1930 5119 1975 2 2224 2038 1953 1807 1795 1893 1946 1875 2139 2048 2090 2261 2006 5119 1976 4 2078 2014 1862 1830 1732 1782 1831 1884 1877 1881 2120 2008 1905 5119 1977 3 1 1880 1786 1867 1772 1649 1783 1746 1718 1926 1972 2077 1999 1849 5119 1978 5 1991 1748 1853 1668 1677 1800 1762 1749 1838 1955 2185 1857 1842 5119 1979 1871 1872 1867 1646 1789 1839 1875 1825 2002 1884 2020 2062 1879 5119 1980 1834 1829 1722 1803 1719 1800 1737 1746 1868 1933 1929 2032 1829 5119 1981 2006 1919 1815 1764 1717 1786 1842 1849 1921 1966 2049 1939 1881 5119 1982 1 1953 2028 1910 1907 1783 1742 1876 1898 2061 1969 2200 2166 1956 5119 1983 2290 1920 1952 1772 1784 1888 1972 2037 2006 2194 2197 2110 2011 5119 1984 2057 1931 1692 1782 1757 1802 1845 1830 1809 1909 1906 1969 1857 5119 1985 2 1793 1789 1804 1751 1648 1739 1794 1861 1960 2118 1990 2001 1853 5119 1986 1852 1685 1951 1662 1820 1853 1915 1756 1891 2157 2133 2023 1893 5119 1987 1787 1859 1674 1721 1667 1700 1776 1739 1900 2003 1954 2043 1818 5119 1988 31XX 2033 1874 1800 1792 1710 1780 1785 1836 2060 2091 219799999 1905 5119 1989 312831303130313130 4 - 999999999999999999999999999999999999999999999 2119 2089 218399999 5119 1990 1 2163 2328 2163 1916 1796 1778 1813 1895 1907 2093 1970 2143 1995 5119 1991 2100 1804 1755 1804 1759 1811 1832 1875 2010 1916 2060 2158 1908 5119 1992 2163 2102 1967 1735 1790 1826 1905 1943 1845 1860 1972 2218 1944 5119 1993 2372 2046 1946 1726 1668 1722 1779 1779 1764 1805 1880 2015 1875 5119 1994 4 1 313 5 1949 1728 1975 1685 1732 1909 1788 1828 1850 2022 2066 2196 1900 5119 1995 4 4 2098 2154 1938 1791 1715 1765 1871 1915 1830 2112 1971 1930 1926 5119 1996 9 8 1917 1838 1729 1751 1657 1820 1822 1758 1792 2042 2017 1866 1839 5119 1997 3 1 2018 2096 1986 1824 1734 1735 1669 1789 2037 2013 1890 1920 1892 5119 1998 5 3 1976 2102 1865 1671 1737 1723 1828 1858 1799 1985 1931 2119 1882 5119 1999 2008 2001 1778 1765 1725 1776 1894 1839 1948 1984 2187 2087 1915 5119 2000 2115 2102 1899 1692 1786 1835 1733 1784 1847 1898 1856 2008 1879 5119 2001 1955 1845 1794 1755 1769 1755 1795 1844 1822 1979 2115 1914 1862 5119 2002 2121 2149 1914 1791 1770 1828 1859 1787 1945 1844 1832 1821 1887 5119 2003 1974 1881 1929 1708 1784 1823 1785 1812 1952 1980 1990 2096 1893 5119 2004 1950 1908 1796 1744 1748 1798 1806 1767 1948 1930 2049 2219 1889 5119 2005 2140 1824 1735 1789 1779 1814 1846 1873 2104 2062 2097 1931 1916 5119 2006 2002 1867 1722 1800 1736 1830 1840 1763 1877 1870 2132 2188 1885 5119 2007 1 2130 1840 1862 1857 1837 1766 1779 1828 1964 2057 2017 2124 1923 5119 2008 2008 2063 1878 1685 1678 1754 1725 1733 1775 2152 2037 1963 1870 5119 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Narvik 040/081 RLR(1964) is 13.5m below BMN9N27 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Narvik 040/081 RLR(1964) is 13.5m below BMN9N27 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-JUL-93 : Values from November 1928 - February 1929 anomalously low (checked to be correct as received from authority). =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1989 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : Whole dataset for Narvik now refers to TGBM N9 N28 8.881m above TGZ. A value for RLR 2008 was calculated. KABELVAG 040091 68 13 N 14 29 E04HL1964 67 6 0 0 1880 312931303130 31 31 - 999999999999999999999999999999 1919 1884 202399999 22409999999999 99999 1881 312831 - 999999999999999 2056 2011 1905 2001 2111 1920 1934 2143 224799999 99999 1882 2294 2179 2087 1724 1951 2057 2268 2347 2180 2220 2240 2130 2140 99999 1883 313031 - 2325 2195 1976 2027999999999999999 1995 1922 2079 2153 214099999 99999 1884 2072 1896 1761 1789 1978 1989 2033 1998 2092 2252 2169 2359 2032 99999 1885 2178 2397 2214 2108 2148 2034 1980 1955 2128 2027 2103 2260 2128 99999 1948 1822 1764 1851 1761 1671 1742 1804 1808 1874 1975 2000 2101 1847 5100 1949 2099 2093 1801 1925 1799 1728 1728 1826 1828 1992 1931 2074 1900 5100 1950 1906 1993 1918 1826 1665 1804 1724 1764 2011 2057 2022 1928 1884 5100 1951 1901 1867 1856 1843 1774 1821 1852 1845 1912 1962 1952 2135 1894 5100 1952 2019 1892 1770 1779 1702 1831 1834 1852 1846 1776 1801 1860 1830 5100 1953 1919 2025 1856 1829 1721 1656 1757 1790 1791 1939 2101 2041 1859 5100 1954 1866 1772 1770 1750 1602 1755 1770 1738 1884 2010 1955 2059 1828 5100 1955 1905 1740 1766 1674 1722 1688 1681 1724 1909 1954 1944 2037 1806 5100 1956 1861 1570 1682 1629 1733 1673 1672 1730 1699 1877 1798 1909 1740 5100 1957 1927 1822 1766 1646 1606 1695 1659 1735 1782 2017 1900 2048 1803 5100 1958 1874 1829 1594 1593 1669 1611 1693 1710 1764 1975 1987 1970 1776 5100 1959 1752 1823 1720 1715 1546 1626 1638 1636 1703 1778 1773 1748 1704 5100 1960 1642 1668 1516 1552 1453 1602 1578 1612 1630 1537 1660 1808 1601 5100 1961 1795 1837 1839 1596 1588 1674 1692 1733 1750 1832 1942 1868 1762 5100 1962 2 1935 1751 1578 1515 1517 1645 1534 1646 1713 1950 1813 1868 1705 5100 1963 1794 1725 1663 1577 1593 1565 1693 1675 1853 2001 1892 1935 1741 5100 1964 4 1983 1915 1688 1687 1731 1754 1902 1778 1926 1929 2118 2074 1873 5100 1965 1910 1753 1793 1641 1546 1690 1675 1643 1707 1930 1957 1879 1761 5100 1966 10 1784 1615 1763 1577 1567 1552 1730 1745 1879 1820 1895 1915 1741 5100 1967 9 7 31114 1 1824 1910 2110 1880 1729 1815 1839 1481 1858 2106 2047 1980 1896 5100 1968 1915 1838 1880 1646 1589 1739 1639 1684 1738 1774 1764 1888 1758 5100 1969 10 1 5 3 1783 1829 1743 1637 1619 1696 1778 1736 1888 2036 2010 1765 1789 5100 1970 1706 1679 1701 1671 1923 1667 1803 1749 1832 1991 1917 1921 1798 5100 1971 7 31 1 1 XX 1941 177099999 1725 1731 1668 1725 1720 1831 1980 1990 2027 1828 5100 1972 1 1 1 1653 1523 1796 1726 1608 1714 1660 1810 1842 1933 1985 1998 1771 5100 1973 13 1943 1924 1835 1682 1688 1725 1724 1730 1810 1804 1995 1879 1814 5100 1974 312831 3 1 - 999999999999999 1638 1619 1718 1800 1775 1913 1758 1831 212699999 5100 1975 1 2089 1907 1768 1691 1652 1712 1771 1730 1976 1910 1959 2125 1857 5100 1976 1985 1905 1772 1728 1650 1694 1721 1737 1749 1760 1900 1799 1783 5100 1977 2 4 1 1807 1715 1792 1704 1563 1661 1676 1662 1808 1880 1999 1892 1766 5100 1978 1 1887 1638 1761 1575 1572 1681 1665 1672 1757 1837 2067 1740 1739 5100 1979 2 1767 1785 1796 1575 1681 1697 1773 1746 1906 1805 1957 1976 1790 5100 1980 1 1 3 1754 1767 1637 1711 1628 1671 1638 1659 1748 1824 1836 1932 1732 5100 1981 1 3 1 1891 1836 1714 1651 1613 1660 1697 1703 1802 1879 1924 1846 1765 5100 1982 4 2 2 2 4 8 4 1861 1925 1815 1773 1686 1610 1722 1790 1936 1878 2105 2091 1848 5100 1983 7 2 2 2 2152 1777 1842 1679 1678 1715 1798 1846 1887 2037 2064 2012 1871 5100 1984 1966 1807 1630 1684 1657 1669 1676 1698 1720 1865 1831 1895 1758 5100 1985 2 2 2 1743 1736 1723 1689 1591 1673 1667 1763 1833 1966 1909 1898 1766 5100 1986 1 7 15 1770 1582 1865 1581 1734 1689 1792 1688 1829 2062 2038 1972 1795 5100 1987 31 XX 99999 1821 1641 1672 1623 1653 1675 1666 1791 1874 1871 1961 1749 5100 1988 312931303130313114 - 9999999999999999999999999999999999999999 1886 1889 2006 200199999 5100 1989 31 3130 5 1 - 2169 2149 1894 161599999 1703 17119999999999 1992 1925 200999999 5100 1990 2040 2168 2002 1749 1599 1631 1657 1719 1762 1932 1819 1969 1836 5100 1991 1946 1670 1630 1661 1596 1677 1633 1700 1842 1761 1922 1964 1751 5100 1992 1 2 1 1969 1929 1810 1617 1624 1633 1717 1786 1711 1716 1870 2058 1787 5100 1993 1 12 2217 1842 1784 1597 1526 1586 1645 1646 1634 1648 1731 1898 1733 5100 1994 5 1 1805 1589 1850 1608 1586 1744 1609 1663 1699 1844 1876 2042 1743 5100 1995 1961 2035 1805 1629 1601 1588 1678 1706 1684 1960 1823 1779 1770 5100 1996 1765 1698 1576 1610 1535 1647 1655 1589 1617 1868 1868 1732 1680 5100 1997 1849 1967 1840 1679 1593 1596 1524 1604 1854 1871 1771 1794 1744 5100 1998 1855 1995 1743 1556 1594 1602 1702 1708 1683 1861 1826 1980 1758 5100 1999 1897 1888 1666 1637 1599 1619 1710 1669 1794 1855 2038 1970 1778 5100 2000 1969 1967 1755 1567 1635 1660 1596 1625 1684 1771 1769 1897 1741 5100 2001 1 1828 1730 1684 1638 1621 1622 1640 1691 1698 1860 1967 1784 1730 5100 2002 1984 2033 1792 1668 1644 1692 1705 1644 1783 1734 1732 1709 1758 5100 2003 1871 1750 1776 1589 1669 1681 1650 1683 1792 1840 1869 1959 1761 5100 2004 1 2 1854 1784 1692 1645 1630 1663 1661 1645 1807 1808 1914 2086 1766 5100 2005 2030 1700 1625 1668 1660 1673 1703 1734 1918 1906 1967 1818 1784 5100 2006 1878 1739 1601 1689 1621 1667 1672 1655 1751 1761 2026 2073 1761 5100 2007 2019 1745 1743 1704 1708 1628 1682 1690 1830 1898 1882 1988 1794 5100 2008 1912 1944 1786 1598 1613 1648 1603 1628 1642 2050 1931 1849 1767 5100 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Kabelvag 040/091 RLR(1964) is 8.3m below BM +3,2-51 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Kabelvag 040/091 RLR(1964) is 8.3m below BM +3,2-51 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1988 BODO 040101 67 17 N 14 23 E04242008 58 22 0 0 1949 312831303130313114 5 212 - 9999999999999999999999999999999999999999 1916 2136 2052 215199999 5149 1950 91414 5 4 4 1 8 5 3 8XX 1974 2077 2043 1958 1807 1984 1900 1964 2271 2192 2149 2074 2025 5149 1951 28313031303131 1313015 - 197399999999999999999999999999999999999 19719999999999 235399999 5149 1952 5 5123011 210313012 - 2087 1948 188299999 1832 1972 1965 1924 20039999999999 199399999 5149 1953 312831 30313130313031 - 999999999999999 1911 18509999999999999999999999999999999999999999 5149 1954 31283130313015 310 1 - 999999999999999999999999999999 1851 1831 1994 2089 2046 214099999 5149 1955 2 630143015 2 3 - 2014 1871 188099999 192099999 1889 1837 1967 2041 2011 207999999 5149 1956 313013 2 - 1938 16829999999999 1849 1817 1783 1786 1799 2000 1938 202699999 5149 1957 2 1 4 2075 1965 1867 1756 1722 1809 1786 1807 1897 2144 2034 2153 1919 5149 1958 4 2 3 1994 1975 1794 1816 1844 1766 1860 1860 1919 2090 2098 2051 1924 5149 1959 1 5 4 1925 2028 1916 1775 1677 1820 1798 1820 1909 1957 1928 1923 1870 5149 1960 4 1 2 1842 1856 1711 1783 1703 1794 1771 1817 1810 1783 1878 1908 1804 5149 1961 1 2 1 2 1 1879 1976 2056 1832 1787 1893 1867 1876 1971 2032 2112 2056 1945 5149 1962 5 5 2107 1890 1733 1679 1681 1771 1696 1795 1843 2106 2002 2055 1860 5149 1963 4 1 3 2 3 10 5 1890 1891 1862 1746 1786 1775 1795 1804 1880 2038 1925 1968 1861 5149 1964 2 1 1 2 2 4 1 1 10 4 2134 1922 1749 1766 1835 1861 1922 1866 1983 1978 2192 2079 1934 5149 1965 312831 1 410313130 7 3 - 999999999999999 1766 1688 1789999999999999999 1976 2029 192699999 5149 1966 828 3113 7 8 7 - 180599999 1823 166099999 1769 1902 1888 2009 1905 1961 208099999 5149 1967 31283130 1 1 211 112 - 99999999999999999999 1729 1797 1851 1853 1919 2155 2074 202599999 5149 1968 6 511 6 1 2 1XX 1934 1837 1933 1717 1611 1764 1708 1775 1728 1845 1857 2024 1805 5149 1969 6 6 53130123115 5 - 1828 1744 1716 16849999999999 188399999 1975 2073 2073 189599999 5149 1970 14 2 15 23130 2 1 2 - 1818 1782 1746 1744 0 1737 18679999999999 1977 1928 193999999 5149 1972 3110 1 2 230313130313031 - 99999 1698 1741 1732 16379999999999999999999999999999999999999999 5149 1973 31 313031303131 5 1 2 - 9999999999999999999999999999999999999999 1828 1799 1921 189399999 5149 1974 3 6 1 2 1937 1773 1635 1614 1646 1732 1845 1786 1935 1738 1873 2151 1808 5149 1975 5 1 1 1 4 1 2135 1932 1818 1712 1625 1736 1805 1753 2029 1947 1974 2146 1883 5149 1976 1989 1924 1785 1743 1681 1725 1767 1777 1776 1786 1921 1826 1808 5149 1977 1821 1746 1820 1741 1595 1709 1707 1694 1853 1923 2026 1931 1797 5149 1978 1914 1655 1787 1585 1581 1706 1681 1669 1769 1889 2086 1762 1758 5149 1979 1430 XX 1780 1784 1784 1573 168099999 1837 1804 1948 1854 1982 2010 1828 5149 1980 5 4 1766 1776 1679 1744 1657 1735 1695 1699 1799 1881 1874 1970 1775 5149 1981 1923 1849 1749 1661 1653 1703 1748 1779 1865 1961 2028 1916 1819 5149 1982 8 1 1887 1964 1862 1855 1785 1705 1835 1901 2021 1958 2191 2139 1924 5149 1983 2262 1843 1907 1758 1765 1802 1874 1916 1948 2116 2100 2071 1948 5149 1984 6 2013 1849 1664 1694 1664 1681 1725 1731 1744 1885 1851 1888 1784 5149 1985 2 4 1740 1762 1753 1716 1617 1704 1722 1800 1888 1983 1926 1935 1793 5149 1986 112831 - 18159999999999 1645 1808 1796 1855 1704 1849 2063 2036 190599999 5149 1987 1739 1804 1622 1650 1603 1627 1687 1658 1797 1910 1891 1988 1748 5149 1989 1 7 2233 2191 1926 1656 1794 1768 1807 1891 1993 2001 2002 2104 1946 5149 1990 93130 - 2112 2256 2095 1849 1702 1739 18059999999999 2047 1932 207399999 5149 1991 1 2030 1756 1726 1757 1703 1785 1758 1815 1954 1869 2040 2070 1856 5149 1992 2064 2021 1904 1709 1736 1755 1836 1901 1821 1820 1970 2155 1891 5149 1993 1 2336 1965 1887 1692 1632 1690 1761 1761 1746 1761 1843 2006 1839 5149 1994 3 1 3 2 1 8 2 1915 1679 1943 1718 1671 1862 1727 1775 1799 1952 1969 2144 1845 5149 1995 8 2032 2114 1885 1718 1695 1699 1791 1821 1779 2062 1960 1871 1866 5149 1996 1 1 5 10 1859 1789 1653 1701 1621 1729 1758 1696 1717 1970 1950 1828 1769 5149 1997 4 530 4XX 1951 2069 1939 1779 1692 1698 1629 1721 1993 197499999 1912 1844 5149 1998 1948 2073 1836 1653 1707 1703 1807 1823 1798 1976 1923 2069 1859 5149 1999 1980 1976 1754 1734 1699 1729 1829 1768 1900 1958 2136 2039 1874 5149 2000 2033 2041 1832 1653 1735 1776 1684 1728 1791 1877 1865 2008 1835 5149 2001 5 3 1929 1817 1779 1745 1710 1722 1739 1807 1794 1964 2070 1856 1830 5149 2002 1 2 2069 2119 1873 1751 1730 1796 1818 1722 1890 1827 1817 1779 1848 5149 2003 1 1940 1812 1846 1663 1754 1776 1734 1774 1895 1938 1948 2027 1843 5149 2004 1919 1856 1771 1726 1722 1753 1755 1727 1908 1910 1999 2161 1851 5149 2005 2098 1764 1691 1743 1743 1767 1793 1821 2016 1977 2045 1886 1862 5149 2006 1936 1799 1665 1767 1699 1760 1768 1730 1838 1863 2116 2151 1841 5149 2007 2090 1809 1812 1780 1796 1702 1754 1780 1929 1984 1954 2041 1870 5149 2008 1958 1999 1859 1672 1649 1729 1690 1712 1751 2159 2005 1918 1841 5149 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Bodo 040/101 RLR(1964) is 10.6m below BM K13 N31 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Bodo 040/101 RLR(1964) is 10.6m below BM K13 N31 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1989 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : To try and resolve the outstanding datum query on consulting the Norwegian web site datum values where found. It appears the Norwegians have revised the datasets. RLR was recalculated at Bodo giving a 2008 value this was them applied to the whole dataset. Data now looks OK although confirmation required from the Norwegian Mapping Authority. NESNA 040106 66 12 N 13 01 E03249999 2 0 0 0 1970 312831303130313130 2 - 999999999999999999999999999999999999999999999-4224-4290-426499999 99999 1971 6 XX 6 313031 - -4181-4342-4498-4487-4455-4440-4421-4335-434199999999999999999999 99999 MO I RANA 040111 66 19 N 13 37 E03249999 3 0 0 0 1951 3128 - 9999999999 -251 -208 -339 -141 20 -33 87 139 13 27599999 99999 1952 95 -52 -156 -98 -150 57 47 -9 45 -104 -57 -38 -35 99999 1953 31 XX 86 -234 -85 -9199999 -109 -116 -49 44 91 222 231 8 99999 SANDNESSJOEN 040117 66 01 N 12 38 E04 C1965 10 4 0 0 1965 3 -439 -633 -559 -641 -697 -544 -577 -512 -395 -235 -295 -324 -485 7483 1966 -451 -454 -420 -601 -522 -503 -395 -427 -298 -347 -329 -264 -417 7483 1967 -429 -304 -136 -463 -503 -408 -349 -366 -328 -80 -169 -277 -318 7483 1968 2 -310 -425 -316 -511 -630 -507 -607 -566 -602 -456 -456 -273 -472 7483 1969 -443 -557 -596 -606 -667 -577 -460 -553 -414 -264 -246 -476 -488 7483 1970 -488 -512 -551 -601 -633 -576 -431 -511 -424 -341 -403 -392 -488 7483 1971 4 8 3 -329 -463 -612 -632 -575 -565 -541 -429 -469 -320 -303 -287 -461 7483 1972 31 1 1 7 - 99999 -547 -510 -542 -622 -498 -499 -436 -395 -335 -230 -16599999 7483 1973 6 30313031 - -367 -330 -446 -529 -566 -452 -517 -4429999999999999999999999999 7483 1974 312831 9 2 8 - 999999999999999 -665 -645 -528 -422 -487 -323 -533 -448 -13099999 7483 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Sandnessjoen 040/117 RLR(1965) is 11.6m below"Topp messingbolt" =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Sandnessjoen 040/117 RLR(1965) is 11.6m below"Topp messingbolt" MOSJOEN 040121 65 51 N 13 12 E03241963 9 4 0 0 1955 31283130313031 - 99999999999999999999999999999999999-3192-3049-2998-3027-299899999 10200 1956 -3125-3401-3288-3294-3132-3115-3199-3220-3208-2981-3102-3023-3174 10200 1957 -2952-3071-3204-3282-3278-3144-3181-3247-3186-2904-3031-2881-3113 10200 1958 28 XX -311199999-3395-3318-3242-3239-3123-3171-3115-2946-2955-3027-3149 10200 1959 -121 74 -54 -151 -207 -62 -105 -90 20 -50 -86 -116 -79 7137 1960 -179 -126 -274 -185 -220 -106 -182 -135 -156 -209 -116 -49 -161 7137 1961 -82 71 213 -97 -99 15 -31 -27 57 75 181 96 31 7137 1962 31 XX 127 -7999999 -294 -206 -69 -166 -105 -58 212 -40 55 -60 7137 1963 3031 - -163 -180 -201 -265 -170 -198 -126 -179 31 111999999999999999 7137 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Mosjoen 040/121 RLR(1963) is 10.2m below BM J17 N6 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Mosjoen 040/121 RLR(1963) is 10.2m below BM J17 N6 BRONNOYSUND 040131 65 29 N 12 13 E04 C1964 12 4 0 0 1956 31293130313031 - 99999999999999999999999999999999999 1081 1097 1304 1247 132799999 5805 1957 31 XX 1337 1262 1183 1104 1056 1088 103999999 1186 1401 1284 1441 1224 5805 1958 1246 1213 984 1026 1093 1013 1105 1104 1163 1332 1293 1290 1155 5805 1959 1146 1211 1139 1085 961 1091 1063 1088 1193 1165 1168 1140 1120 5805 1960 31 XX 1055 1083 931 1003 934 1007 100299999 1044 995 1087 1153 1026 5805 1961 31 XX 1139 1236 1267 1070 1039 1121 108999999 1150 1210 1306 1195 1166 5805 1962 4 5 1174 1141 911 926 994 1095 998 1108 1197 1363 1222 1281 1117 5805 1963 4 1077 1107 1084 1009 1060 1020 1055 1080 1242 1355 1275 1235 1130 5805 1964 1301 1205 1043 1085 1156 1162 1227 1188 1282 1249 1391 1362 1221 5805 1965 11 1246 1059 1143 1061 1028 1153 1111 1072 1219 1342 1290 1284 1164 5805 1966 1135 1156 1117 1000 1062 1077 1188 1146 1291 1215 1228 1316 1166 5805 1967 1123 1288 1423 1129 1085 1150 1225 1228 1265 1536 1416 1355 1269 5805 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Bronnoysund 040/131 RLR(1964) is 9.8m below BM Kai =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Bronnoysund 040/131 RLR(1964) is 9.8m below BM Kai RORVIK 040136 64 52 N 11 15 E04241972234 40 6 0 0 1969 3128313031303131 2 - 9999999999999999999999999999999999999999 1309 1450 1471 124499999 99999 1970 5 3 4 1238 1206 1185 1144 1137 1168 1303 1242 1362 1404 1336 1343 1256 99999 1971 1 2 1415 1317 1218 1155 1209 1194 1191 1271 1266 1428 1458 1487 1302 99999 1972 5 1 1 2 4 1223 1203 1232 1203 1111 1221 1226 1278 1294 1350 1477 1476 1273 5690 1973 1350 1388 1307 1178 1170 1251 1184 1253 1275 1278 1410 1391 1285 5690 1974 10 1 1440 1275 1198 1038 1071 1170 1270 1234 1403 1191 1297 1553 1264 5690 1975 1542 1282 1213 1114 1082 1131 1193 1151 1429 1357 1385 1500 1282 5690 1976 3 3 1399 1278 1185 1127 1102 1139 1155 1142 1140 1189 1303 1240 1200 5690 1977 2 30 7 XX 1233 1170 1217 1174 1002 1119 1104 108799999 1352 1462 1350 1203 5690 1978 2 6 1 1 8 1334 1085 1209 1027 1024 1169 1147 1128 1277 1354 1528 1234 1211 5720 1979 9 2 1136 1177 1250 1059 1185 1186 1256 1219 1396 1288 1399 1403 1249 5720 1980 2 3 1 2 1170 1167 1100 1181 1113 1181 1108 1155 1300 1367 1295 1396 1212 5720 1981 11 3 1341 1207 1196 1092 1116 1153 1174 1227 1273 1400 1433 1310 1241 5720 1982 4 1263 1317 1258 1247 1169 1087 1185 1279 1433 1332 1565 1496 1303 5720 1983 6 1614 1166 1278 1151 1170 1175 1265 1265 1316 1536 1491 1463 1327 5720 1984 3 1387 1200 1038 1118 1124 1124 1150 1155 1213 1363 1329 1350 1213 5720 1985 4 3 2 5 1156 1178 1204 1163 1058 1103 1164 1255 1343 1397 1324 1326 1221 5720 1986 2 11 4 3 6 1 9XX 1212 997 1257 1014 1216 1151 1212 1119 1302 1511 1491 1407 1235 5720 1987 3110 5 5 2 1 1 XX 99999 1229 1133 1146 1104 1110 1147 1135 1311 1393 1342 1445 1230 5720 1988 4 1 3 231301331 5 6 - 1393 1291 1193 11199999999999 114799999 1496 1385 1410 145999999 5720 1989 3 1 1 1605 1593 1366 1101 1233 1186 1185 1298 1378 1431 1367 1453 1348 5720 1990 1497 1628 1457 1233 1073 1127 1168 1235 1288 1417 1296 1410 1317 5720 1991 1381 1117 1106 1151 1073 1179 1115 1196 1350 1257 1415 1411 1230 5720 1992 1409 1386 1270 1086 1108 1129 1207 1295 1240 1195 1367 1480 1264 5720 1993 3 1655 1264 1228 1081 1018 1075 1175 1185 1146 1155 1230 1399 1218 5720 1994 10 6 3 1316 1077 1322 1110 1083 1259 1113 1157 1195 1324 1341 1500 1237 5720 1995 10 1404 1499 1278 1108 1098 1076 1164 1175 1156 1451 1313 1241 1245 5720 1996 2 3 1216 1133 1020 1072 1028 1136 1144 1086 1083 1336 1327 1228 1151 5720 1997 1318 1483 1308 1162 1092 1093 1017 1119 1388 1347 1265 1254 1235 5720 1998 2 2 1317 1439 1233 1066 1106 1097 1215 1256 1191 1377 1300 1454 1253 5720 1999 1370 1379 1159 1133 1101 1133 1214 1139 1301 1334 1479 1396 1261 5720 2000 2 1371 1413 1199 1063 1137 1148 1076 1119 1197 1306 1288 1421 1228 5720 2001 5 1317 1206 1188 1137 1102 1128 1114 1227 1187 1415 1429 1233 1221 5720 2002 1432 1498 1252 1150 1137 1224 1197 1113 1271 1212 1204 1142 1234 5720 2003 1328 1167 1213 1084 1165 1188 1138 1201 1284 1303 1331 1383 1233 5720 2004 1318 1242 1174 1136 1132 1147 1145 1134 1328 1318 1365 1521 1247 5720 2005 1481 1135 1077 1140 1147 1157 1182 1204 1375 1339 1433 1286 1247 5720 2006 1278 1186 1053 1162 1101 1139 1139 1134 1255 1291 1495 1509 1229 5720 2007 6 6 1476 1213 1195 1147 1201 1098 1162 1193 1332 1298 1297 1377 1248 5720 2008 1354 1376 1284 1084 1060 1139 1106 1156 1184 1525 1384 1271 1243 5720 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Rorvik 040/136 RLR(1972) is 9.2m below BM FM5 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Rorvik 040/136 RLR(1972) is 9.2m below BM FM5 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1988 TRONDHEIM 040141 63 26 N 10 26 E04HL1964 50 14 0 0 1872 312931 - 999999999999999 2133 2196 2220 2225 2174 2216 2385 2335 243499999 99999 1873 31313031 - 2455 2118 2032 2060 2269 219999999999999999999999 2459 249599999 99999 1874 3031 - 2647 2389 2318 2255 2355 2357 2259 2330 2440 2613999999999999999 99999 1877 3128 - 9999999999 2164 2065 2098 2192 2235 2161 2144 2390 2497 232999999 99999 1878 31 3031 - 2295 2342 2210 2093 2239 230599999 2153 2232 2379999999999999999 99999 1880 31 303130 - 99999 2330 2153999999999999999 2155 1956 2265 2190 2448 231599999 99999 1881 3128 30 - 9999999999 2180 2066 2047 2190 2218 2298 2130 224799999 237799999 99999 1945 312831303130 - 999999999999999999999999999999 755 738 726 883 823 89899999 6055 1946 313130313031 - 938 842 739 876 738 94199999999999999999999999999999999999 6055 1949 1079 1033 739 909 861 811 743 811 819 1011 939 1049 900 6055 1950 845 926 797 819 661 844 766 828 1042 1038 952 880 865 6055 1951 811 731 703 717 605 691 782 798 890 872 867 1112 798 6055 1952 964 821 756 764 728 876 845 805 857 786 786 837 819 6055 1953 873 762 794 829 753 757 800 868 868 929 1048 977 855 6055 1954 831 685 709 642 608 725 764 751 919 990 918 988 794 6055 1955 980 812 745 717 784 786 779 737 867 894 982 1053 844 6055 1956 902 652 713 723 829 831 799 796 790 977 919 1002 835 6055 1957 987 936 739 664 713 793 741 729 870 1091 969 1130 853 6055 1958 911 887 665 864 942 936 946 951 976 1039 990 902 913 6055 1959 805 838 735 789 696 799 751 751 850 817 798 796 785 6055 1960 720 772 641 760 766 859 842 991 883 818 810 987 821 6055 1961 909 974 1062 833 847 923 856 898 968 1014 1079 1032 950 6055 1962 5 5 1091 888 747 699 792 865 802 876 934 1074 916 995 889 6055 1963 9 1 930 783 772 712 814 756 778 783 953 1016 964 962 850 6055 1964 1 2 1 936 871 728 763 888 893 923 871 954 895 1052 1027 900 6055 1965 3 3 6 5 2 898 759 815 767 730 705 818 819 921 1028 976 944 852 6055 1966 2 1 813 848 869 713 795 808 884 820 959 933 913 1007 864 6055 1967 2 834 939 1093 840 801 878 917 909 936 1135 1052 1035 948 6055 1968 938 846 949 807 736 858 769 757 730 896 866 937 841 6055 1969 2 838 759 732 764 720 735 795 778 866 996 1038 813 820 6055 1970 8 1 3 824 804 778 734 677 764 851 793 895 978 906 932 831 6055 1971 4 1 8 4 612 7 f 999 889 691 704 748 777 549 486 562 863 932 980 765 6055 1972 2 2 671 683 689 704 676 785 762 718 731 791 929 832 748 6055 1973 3 2 785 839 745 669 623 725 701 785 861 861 1018 939 795 6055 1974 3 3 2 1 2 929 841 595 612 645 797 869 828 969 776 840 1090 819 6055 1975 1 3 5 7 7 31 5 2XX 1100 833 790 677 718 739 835 744 96499999 979 1099 863 6055 1976 8 7 3 9 1 949 868 813 1082 726 826 803 728 734 740 851 795 817 6055 1977 5 1 817 759 789 739 610 699 716 676 796 899 1007 881 782 6055 1978 3 828 630 768 592 596 759 733 727 866 920 1103 765 774 6055 1979 2 729 715 764 584 686 716 789 744 909 828 925 945 778 6055 1980 2 1230 8XX 729 741 663 714 665 741 697 739 863 102599999 930 760 6055 1981 4 2 5 800 764 832 696 733 846 834 854 904 1035 1081 951 861 6055 1982 3 4 2 893 967 925 899 856 804 847 959 1088 1020 1238 1200 975 6055 1983 5 6 4 1312 808 934 811 833 807 850 875 954 1236 1232 1158 987 6055 1984 2 1079 886 746 709 691 699 704 678 730 893 888 901 800 6055 1985 2 3 4 1 666 698 687 662 573 653 674 747 848 999 877 803 740 6055 1986 695 467 750 522 704 648 710 613 739 921 954 855 717 6055 1987 2 628 741 605 614 609 630 628 639 801 862 828 931 708 6055 1988 1031 2 XX 955 791 719 649 633 66699999 814 971 908 1020 1007 835 6055 1989 3 3 1 7 4 3 4 1119 1115 934 683 800 771 794 921 924 1014 971 1103 923 6055 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Trondheim 040/141 RLR(1964) is 10.4m below BM"Sodemannsgt" =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Trondheim 040/141 RLR(1964) is 10.4m below BM"Sodemannsgt" =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUL-94 : Anomalously low values July-September 1971 correct as received from authority. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 10-OCT-94 : new gauge established in December 1989 but treated as separate station (040/142) as no connection between old and new bench marks =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=hl =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1989 TRONDHEIM 2 040142 63 26 N 10 26 E04241995 20 9 0 0 1989 8 0 0 0 0 0 0 0 0 0 0 0 984 63 99999 1990 1 965 1069 914 700 597 634 657 705 747 856 763 857 787 6242 1991 31411 1 829 577 575 611 557 676 625 669 809 733 878 877 707 6242 1992 5 876 859 744 580 590 614 688 766 733 674 846 914 742 6242 1993 1 5 1 3 3 1091 714 678 564 567 607 674 665 626 616 669 854 697 6242 1994 1 784 530 767 575 569 722 599 638 640 779 802 945 698 6242 1995 851 949 737 588 592 590 663 647 619 881 764 693 713 6242 1996 653 613 495 552 537 632 645 562 572 781 784 694 627 6242 1997 6 778 948 777 675 607 620 561 618 858 838 750 716 728 6242 1998 784 921 716 559 591 623 712 749 677 838 767 896 735 6242 1999 4 839 844 639 615 591 636 705 623 769 788 905 865 733 6242 2000 1 840 891 682 559 632 641 567 578 652 779 766 883 706 6242 2001 775 678 680 608 577 613 609 707 676 848 881 712 697 6242 2002 899 962 735 633 632 725 688 617 720 674 677 597 711 6242 2003 800 629 660 561 644 688 637 689 743 775 804 852 707 6242 2004 792 719 643 606 628 657 632 628 811 789 835 987 727 6242 2005 969 622 570 617 631 648 673 691 836 807 895 753 727 6242 2006 729 650 538 642 591 621 620 629 724 767 948 964 702 6242 2007 965 721 684 626 713 634 673 690 817 812 817 837 750 6242 2008 837 858 782 571 563 653 614 667 667 970 856 735 731 6242 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 10-OCT-94 : gauge established in December 1989 but problems of subsidence reported, records for 1991-93 are corrected for the known subsidence =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2000Apr25 : Trondheim 2 040/142 RLR(1995) is 13.9m below BM G24 N144 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 26-Oct-2009 : The gauge at Trondheim is sinking at a rate of 1-2mm per year. They will look at new levelling data before deciding what to do. See letter of 24th March 2009. HEIMSJO 040151 63 26 N 09 07 E04241967 81 23 0 0 1928 3 531 4 2 1 1XX 2200 206399999 1919 1822 1948 2057 1959 2023 2115 2152 2149 2036 6966 1929 2 1 4 1893 1901 1931 1865 1863 1931 1921 1989 2142 2177 2213 2288 2008 6966 1930 1 2 3 7 4 3 5 2277 1900 1993 1837 1875 1937 1988 1940 1966 2212 2247 2109 2025 6966 1931 3031 1 - 2051 2005 18669999999999 1958 2019 1902 1903 2147 2102 214899999 6966 1932 3130 1 2 - 2300 19329999999999 1830 1843 1956 1998 2196 2156 2133 222699999 6966 1933 3130 3 - 2176 20769999999999 1808 1837 1946 2044 1957 2081 1945 200499999 6966 1934 3128313031303115 - 99999999999999999999999999999999999 1980 2107 2280 2105 208699999 6966 1935 2 2008 2197 1847 1866 1757 1926 1956 1956 2033 2255 2135 2106 2002 6966 1936 2046 2052 1820 1930 1735 1895 1939 2021 1981 2108 2076 2328 1994 6966 1937 3 2110 2077 1827 1857 1875 1988 1989 1908 2133 2089 2104 1947 1990 6966 1938 3128 6 2 2 6 31 - 9999999999 2130 1907 1909 1998 1902 1996 1964 2266 23199999999999 6966 1939 3 2 2064 2125 1830 1959 1785 1945 1957 1951 1968 1964 2176 2053 1979 6966 1940 2 1 30 1XX 1982 1907 1945 1859 1829 1876 1892 1951 2073 201699999 2094 1947 6966 1941 1 1936 1992 1851 1759 1777 1880 1903 1992 1961 1999 1952 2149 1929 6966 1942 5 231 4 3 6 7 631 - 1919 185999999 1863 1879 1908 1913 1941 2139 2272 21199999999999 6966 1943 31283130 3 3 1 - 99999999999999999999 1962 1935 1932 1986 2098 2193 2106 212799999 6966 1944 1 4 3 8 615 1 XX 2252 1987 1949 1916 1840 1942 1877 1955 1963 2200 2128 2141 2009 6966 1945 8 1 4 3 1 2 1 2013 2112 1987 2010 1905 1970 1931 1918 1935 2058 2063 2171 2006 6966 1946 7 2 5 2 6 2140 2067 1934 2022 1862 2026 1998 2104 2224 2048 2136 2018 2049 6966 1947 2001 1847 1962 2043 1766 1894 1974 1904 2099 2067 2179 2163 1992 6966 1948 1 2058 1903 1975 1932 1869 1915 1930 1937 2128 2222 2196 2259 2027 6966 1949 2228 2177 1909 2059 1929 1899 1869 1992 2035 2277 2234 2390 2083 6966 1950 2176 2289 2079 2119 1829 1991 1937 2061 2279 2200 2140 2061 2095 6966 1951 714 2029 1979 1940 1955 1842 1935 2031 1979 2109 2142 2094 2301 2022 6966 1952 8 610 2145 2033 1952 1953 1876 2042 2027 1921 2022 1918 1924 2041 1990 6966 1953 2 2 7 4 5 3 9 XX 2040 1985 1984 1981 1894 1853 1934 2054 2072 2166 2256 2146 2039 6966 1954 3 3 2 2040 1909 1923 1814 1789 1876 1938 1933 2131 2192 2133 2189 1991 6966 1955 4 5 2085 1935 1924 1863 1921 1864 1878 1863 2062 2105 2136 2183 1987 6966 1956 1 2 1 1 2035 1775 1853 1856 1941 1898 1875 1881 1908 2167 2091 2144 1954 6966 1957 2149 2079 1968 1839 1815 1853 1855 1866 2028 2218 2109 2228 2000 6966 1958 1 2 31 6 6 4 1XX f 2066 2009 1803 186299999 1840 1903 1959 2026 2155 2101 2116 1984 6966 1959 31410 2 3130313031 - 1988 2116 1946 1954 1789 1956 1903999999999999999999999999999999 6966 1960 4 1957 1997 1898 1917 1809 1842 1856 1927 1905 1890 2074 2089 1930 6966 1961 1995 2096 2118 1911 1891 1950 1919 1980 2106 2148 2157 2136 2033 6966 1962 2192 1961 1834 1794 1897 1905 1828 2025 2062 2201 2002 2095 1984 6966 1963 6 6 1848 1898 1902 1842 1858 1806 1832 1903 2056 2204 2104 2069 1947 6966 1964 8 7 2072 1952 1817 1856 1901 1928 2023 1937 2052 2049 2181 2156 1991 6966 1965 1 3130 4 - 2064 1850 1923 1855 1779 1984 1889 1869 20569999999999 204599999 6966 1966 2 3 2 1927 1978 1989 1789 1864 1867 1977 1914 2111 2097 2042 2166 1975 6966 1967 12 31 XX 1954 2077 2223 1904 1892 1959 2005 1999 205299999 2140 2118 2022 6966 1968 2049 1957 2011 1833 1764 1910 1806 1790 1826 2087 1996 2067 1925 6966 1969 31 1 4 XX 99999 1882 1853 1851 1787 1839 1937 1856 1935 2061 2162 1938 1919 6966 1970 1922 1864 1835 1787 1759 1710 1905 1871 2016 2077 2025 2008 1899 6966 1971 2062 1985 1848 1891 1911 1895 2080 1915 1865 2145 2078 2073 1979 6966 1972 1 3 1839 1891 1884 1837 1850 1965 1849 2000 1964 1998 2116 2191 1949 6966 1973 31 31 1 1 2 - 99999 2053 1950 183699999 1859 1837 1914 1951 1965 2094 205799999 6966 1974 5 2125 1920 1663 1628 1714 1854 1945 1920 2104 1875 2013 2246 1917 6966 1975 2248 1939 1888 1783 1760 1809 1843 1806 2089 2019 2055 2166 1951 6966 1976 2063 1944 1876 1804 1800 1838 1853 1816 1799 1902 2038 1961 1891 6966 1977 4 7 1951 1901 1914 1872 1701 1790 1780 1749 1901 2070 2135 2021 1896 6966 1978 2014 1775 1923 1714 1708 1854 1806 1810 1976 2020 2181 1904 1891 6966 1979 1901 1882 1942 1738 1849 1863 1917 1887 2072 1970 2075 2076 1931 6966 1980 1852 1868 1782 1817 1727 1805 1740 1797 1982 2026 1956 2069 1868 6966 1981 1992 1930 1898 1733 1781 1830 1830 1875 1946 2097 2139 1991 1920 6966 1982 1938 2005 1956 1882 1834 1733 1823 1946 2095 2024 2224 2168 1969 6966 1983 2275 1826 1963 1840 1854 1847 1904 1902 1965 2219 2160 2139 1993 6966 1984 2047 1868 1704 1785 1774 1769 1784 1778 1843 2063 2060 2047 1877 6966 1985 1860 1911 1904 1831 1729 1799 1853 1959 2001 2071 1958 2020 1908 6966 1986 1927 1668 1984 1702 1913 1826 1891 1810 1953 2153 2180 2106 1928 6966 1987 1838 1938 1804 1802 1770 1781 1806 1798 2017 2101 2020 2108 1898 6966 1988 2137 1978 1881 1804 1756 1770 1843 1986 2129 2038 2106 2104 1961 6966 1989 2230 2227 2047 1781 1891 1837 1839 1978 2048 2079 2055 2139 2012 6966 1990 3031 1 - 2194 2300 2127 1912 1741 1797 1851 19179999999999 1982 206199999 6966 1991 2041 1804 1799 1831 1740 1853 1774 1892 2017 1942 2099 2070 1906 6966 1992 1 2056 2039 1931 1775 1779 1821 1873 1972 1966 1874 2092 2137 1943 6966 1993 2309 1904 1885 1769 1703 1757 1853 1865 1830 1838 1913 2091 1894 6966 1994 3 6 2034 1775 2012 1800 1756 1932 1787 1855 1877 1989 2040 2173 1924 6966 1995 5 212 8 8 XX 2101 2158 1971 1778 1780 1738 1836 1832 1827 2130 1977 1902 1920 6966 1996 1887 1830 1706 1760 1727 1818 1821 1775 1784 2019 2004 1915 1837 6966 1997 1976 2159 1970 1837 1768 1760 1711 1840 2082 2023 1963 1942 1917 6966 1998 2008 2142 1917 1757 1759 1780 1903 1960 1880 2063 2000 2102 1939 6966 1999 312 1 2060 2050 1876 1823 1799 1824 1901 1783 2005 1989 2078 2053 1930 6966 2000 10 2 2011 2082 1863 1744 1791 1842 1752 1794 1891 2030 2030 2117 1909 6966 2001 2005 1891 1889 1823 1772 1782 1774 1934 1875 2094 2083 1920 1904 6966 2002 31 2 XX 2111 2173 1937 1846 1828 196999999 1832 1925 1911 1939 1846 1937 6966 2003 6 2022 1859 1884 1768 1848 1881 1830 1901 1958 1975 2037 2032 1915 6966 2004 2 2021 1925 1854 1817 1813 1822 1816 1837 2049 2020 2041 2180 1932 6966 2005 9 2 2258 1810 1777 1817 1817 1825 1848 1876 2048 2022 2113 1973 1926 6966 2006 1961 1852 1745 1857 1791 1810 1829 1834 1977 2008 2189 2184 1920 6966 2007 2153 1920 1893 1810 1892 1794 1859 1921 2018 2021 1994 2044 1944 6966 2008 2065 2079 1991 1788 1745 1842 1813 1898 1934 2200 2063 1959 1948 6966 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Heimsjo 040/151 RLR(1967) is 9.9m below BM E24N1 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Heimsjo 040/151 RLR(1967) is 9.9m below BM E24N1 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-JUL-93 : Anomalously low value for June 1958 - checked correct as received from authority. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1990 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : The Norwegian Mapping Authority have revised their datasets TGBM for Heimsjo is now E24 N1 throughout the dataset this is 4.934m above TGZ. As a result RLR has been recalculated to 6966. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : KRISTIANSUND N 040161 63 07 N 07 44 E04242008 57 16 0 0 1952 31293130 - 99999999999999999999 1967 2136 2108 2074 2116 2120 2106 214699999 4981 1953 5 5 1 5 6 2153 2058 2072 2108 1978 1907 2019 2165 2207 2281 2382 2264 2132 4981 1954 2 1 4 3 2 13031 - 2114 2022 2006 1929 1872 1978 2059 2090 2232 2285999999999999999 4981 1955 11 4 5 5 2 2 4 3 3XX 2275 2065 1981 1926 1997 1940 1973 1964 2181 2188 2189 2275 2074 4981 1956 4 4 4 1 1 1 2145 1836 1951 1939 2023 1968 1951 1992 2026 2263 2189 2262 2049 4981 1957 3 6 4 3 2 5 2248 2227 2089 1942 1909 1942 1950 1976 2145 2310 2206 2228 2091 4981 1958 5 7 4 7 2137 2080 1912 1945 2000 1908 1992 2061 2120 2260 2190 2196 2061 4981 1959 3 2069 2067 2030 2033 1878 2038 1993 2023 2037 2104 2136 2151 2047 4981 1960 3 2014 2059 1925 1974 1881 1940 1955 2031 2055 2007 2183 2201 2018 4981 1961 3 1 3 2 4 1 6 2114 2200 2205 2001 1986 2046 2020 2083 2187 2254 2272 2250 2132 4981 1962 5 2 4 2295 2050 1936 1898 1917 1981 1916 2087 2153 2259 2111 2164 2060 4981 1963 1920 1976 1995 1925 1969 1908 1933 2015 2174 2250 2184 2163 2035 4981 1964 9 2 7 2115 2041 1936 1981 2060 2073 2150 2044 2052 2135 2245 2217 2093 4981 1965 2 1 2 2159 1931 2026 1985 1917 2045 1990 1987 2186 2251 2172 2188 2070 4981 1966 2051 2098 2107 1900 1952 1966 2064 2002 2180 2140 2129 2270 2072 4981 1967 1 4 2042 2172 2292 1973 1961 2013 2090 2079 2159 2374 2226 2182 2131 4981 1968 1 9 2123 2011 2129 1945 1861 1994 1907 1886 1934 2176 2096 2129 2013 4981 1969 2 4 2 2 2067 1967 1924 1929 1868 1899 2009 1945 2053 2185 2233 2029 2009 4981 1970 2035 1985 1925 1885 1866 1855 2015 1975 2120 2182 2158 2128 2011 4981 1971 8 411 2 2234 2159 2047 1986 2034 1990 1986 2065 2016 2163 2168 2211 2089 4981 1972 1982 1934 1951 1948 1872 2006 1983 2017 1995 2059 2223 2259 2019 4981 1973 2 2 2086 2122 2022 1918 1916 1981 1943 1995 2036 2045 2177 2143 2031 4981 1974 3 10 2222 2041 1819 1787 1842 1942 2021 2004 2191 1972 2114 2337 2016 4981 1975 6 2 12 2317 2027 1963 1874 1841 1883 1931 1907 2179 2099 2128 2277 2023 4981 1976 11 5 2140 2032 1973 1884 1891 1924 1959 1885 1863 2013 2122 2062 1978 4981 1977 5 71530 XX 1949 1873 1885 1849 1766 1861 1885 183899999 2126 2207 2101 1948 4981 1978 2 4 2090 1892 2024 1816 1807 1914 1882 1890 2052 2097 2252 2004 1978 4981 1979 1990 1964 2035 1836 1929 1937 1973 1976 2140 2063 2166 2173 2016 4981 1980 1972 1967 1880 1889 1808 1893 1834 1904 2078 2110 2033 2151 1960 4981 1981 15 3 2068 2054 2088 1915 1977 2021 1991 2025 2048 2190 2201 2088 2054 4981 1982 2036 2107 2048 1961 1931 1826 1916 2051 2193 2128 2315 2265 2064 4981 1983 3 2370 1918 2067 1943 1968 1945 1992 1982 2068 2316 2258 2236 2089 4981 1984 4 2160 1969 1798 1892 1867 1880 1884 1881 1952 2177 2171 2133 1979 4981 1985 4 3 1979 2037 2011 1923 1820 1888 1956 2083 2085 2137 2052 2127 2008 4981 1986 731 1 531 - 2043 1790 2092 179999999 1894 1925 1849 1975 2181 21909999999999 4981 1987 3128 1 9999999999 1870 1846 1867 1872 1922 1937 2158 2233 2134 2199 1819 4981 1988 1 2251 2095 1996 1917 1870 1891 1999 2111 2238 2151 2214 2237 2081 4981 1989 1 6 2 2359 2372 2179 1937 2021 1971 1968 2112 2170 2199 2180 2251 2142 4981 1990 31XX 2324 2433 2238 2021 1844 1925 1961 2042 2119 2210 209299999 2108 4981 1991 11 3 1 2050 1932 1924 1949 1846 1962 1863 1989 2100 2033 2193 2156 1999 4981 1992 2 2089 2126 2015 1871 1872 1919 1965 2063 2077 1966 2200 2229 2032 4981 1993 6 1 2409 1991 1978 1867 1788 1841 1936 1967 1924 1931 2019 2188 1988 4981 1994 2134 1870 2110 1896 1842 2012 1881 1950 1976 2071 2138 2267 2013 4981 1995 2182 2246 2049 1859 1867 1811 1920 1912 1937 2235 2071 1987 2005 4981 1996 1990 1926 1804 1864 1820 1909 1910 1882 1887 2121 2095 2007 1935 4981 1997 2056 2264 2060 1908 1850 1845 1807 1952 2158 2105 2075 2055 2009 4981 1998 2114 2233 2002 1863 1851 1874 2008 2062 1988 2169 2117 2202 2040 4981 1999 2174 2141 1992 1923 1908 1930 2001 1874 2126 2126 2217 2152 2046 4981 2000 8 130 XX 2120 2192 1961 1842 1888 1948 1861 189799999 2159 2167 2230 2028 4981 2001 2111 1992 1984 1915 1854 1866 1875 2041 1972 2210 2155 2014 1999 4981 2002 2207 2268 2035 1948 1936 2082 1989 1941 2028 2033 2065 1955 2039 4981 2003 2131 1977 1991 1875 1953 1995 1947 2009 2059 2074 2163 2145 2027 4981 2004 2137 2024 1963 1928 1921 1922 1920 1953 2164 2130 2130 2281 2040 4981 2005 2241 1910 1885 1924 1915 1927 1951 1984 2157 2143 2226 2077 2029 4981 2006 2072 1949 1865 1974 1901 1909 1933 1940 2092 2119 2303 2285 2029 4981 2007 2252 2027 1999 1896 1986 1890 1969 2038 2105 2126 2078 2148 2044 4981 2008 2187 2183 2096 1895 1842 1945 1932 2022 2053 2297 2164 2068 2057 4981 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Kristiansund 040/161 RLR(1964) is 9.0m below BM"Kai" =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Kristiansund 040/161 RLR(1964) is 9.0m below BM"Kai" =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1986 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset for Kristiansund now refers to benchmark D25 N40 which is 11.519m above TGZ. A 2008 value for RLR has been calculated. MOLDE 040171 62 44 N 07 10 E03249999 1 0 0 0 1954 3128313031 - 9999999999999999999999999-2629-2582-2562-2398-2286-2376-235199999 99999 BORGUND 040181 62 27 N 06 18 E03249999 1 0 0 0 1957 -3334-3338-3455-3578-3606-3583-3556-3519-3373-3229-3423-3283-3440 99999 ALESUND 040191 62 28 N 06 09 E04242008 60 22 0 0 1945 31 XX 99999 -216 -342 -312 -369 -298 -294 -347 -275 -202 -164 -86 -264 7211 1946 2831303130313130313031 - -130999999999999999999999999999999999999999999999999999999999999 7211 1951 -207 -274 -326 -393 -374 -448 -355 -247 -144 -158 -132 63 -249 7211 1952 -97 -250 -277 -275 -340 -173 -230 -265 -229 -175 -235 -167 -226 7211 1953 -179 -294 -314 -247 -329 -383 -287 -183 -172 -109 3 -92 -215 7211 1954 -282 -333 -345 -418 -474 -379 -311 -288 -95 -52 -103 -66 -262 7211 1955 -198 -304 -397 -408 -355 -426 -389 -411 -180 -164 -170 -94 -291 7211 1956 -272 -537 -436 -445 -359 -404 -431 -396 -332 -144 -218 -150 -343 7211 1957 -192 -206 -330 -461 -497 -480 -412 -396 -212 -89 -199 -102 -293 7211 1958 -258 -311 -488 -467 -409 -513 -459 -348 -290 -127 -212 -202 -341 7211 1959 -314 -335 -331 -327 -506 -368 -277 -357 -357 -270 -243 -188 -323 7211 1960 -350 -327 -461 -474 -552 -492 -490 -377 -415 -437 -292 -279 -413 7211 1961 8 9 2 1279 1379 1357 1219 1187 1247 1190 1279 1403 1435 1434 1393 1317 5650 1962 1 2 2 3013 XX 1512 1215 1118 1085 1109 1237 1144 134399999 1404 1306 1348 1252 5650 1963 5 7 5 1092 1158 1204 1135 1172 1095 1135 1257 1377 1451 1429 1381 1243 5650 1964 1334 1279 1139 1191 1264 1270 1328 1264 1343 1349 1432 1417 1301 5650 1965 6 5 2 1355 1096 1174 1177 1122 1245 1166 1189 1393 1455 1373 1400 1258 5650 1966 4 1 3 1280 1325 1307 1118 1181 1177 1286 1231 1404 1395 1379 1521 1302 5650 1967 2 12 1281 1418 1552 1231 1248 1289 1369 1378 1412 1686 1525 1461 1405 5650 1968 31 11 8 XX 1407 1301 1386 1214 1122 1288 118199999 1170 1383 1273 1367 1278 5650 1969 3 7 1 1308 1202 1154 1168 1131 1153 1271 1250 1319 1473 1525 1301 1272 5650 1970 411 1311 1281 1221 1207 1183 1152 1289 1240 1331 1353 1391 1295 1268 5650 1971 4 2 4 1 2 1409 1295 1192 1179 1207 1159 1126 1296 1304 1423 1422 1487 1290 5650 1972 4 3 1 2 314 1 1 4 XX 1259 1203 1206 1224 1142 1309 1296 1284 1260 1335 1484 1566 1297 5650 1973 15 2 11 1352 1390 1282 1192 1173 1247 1229 1306 1369 1367 1500 1452 1328 5650 1974 1411 7 11 6XX 1562 1350 1243 1157 1197 1306 1354 1360 1453 1235 1375 1570 1335 5650 1975 4 6 1 1608 1278 1236 1074 1056 1111 1165 1154 1430 1280 1458 1500 1281 5650 1976 4 5 4 1294 1166 1121 1033 1061 1104 1083 1094 1102 1335 1407 1344 1180 5650 1977 1331 1285 1294 1224 1060 1127 1131 1137 1275 1442 1517 1401 1268 5650 1978 3 3 1 5 1387 1184 1314 1114 1113 1233 1180 1188 1315 1366 1533 1309 1270 5650 1979 1272 1210 1317 1122 1204 1214 1245 1259 1400 1338 1439 1451 1290 5650 1980 3 1224 1240 1172 1174 1088 1180 1130 1228 1395 1413 1336 1441 1252 5650 1981 128 3031 61231 6 - 133399999 1248 1050 11199999999999 1194 129399999 1497 134599999 5650 1982 9 13031 5 3 7 - 1288 1386 13229999999999 1100 1173 1325 1448 1434 1566 150199999 5650 1983 5 3 3131 5 - 1642 1200 1359 1208 1250 11829999999999 1318 1586 1461 144699999 5650 1984 1435 1215 1080 1176 1131 1106 1127 1115 1216 1458 1523 1475 1255 5650 1985 3 131 8 3 4 3XX 1348 1396 1313 1200 1101 1170 125999999 1311 1405 1239 1390 1282 5650 1986 52831 6 1 - 13469999999999 1083 1337 1170 1247 1189 1291 1525 1554 152299999 5650 1987 1210 1293 1191 1177 1143 1119 1170 1176 1422 1482 1359 1406 1262 5650 1988 9 1520 1345 1257 1172 1133 1143 1279 1368 1484 1435 1475 1457 1341 5650 1989 1593 1613 1442 1197 1260 1200 1202 1363 1412 1440 1426 1472 1384 5650 1990 1 1601 1712 1507 1290 1112 1198 1239 1324 1397 1491 1354 1429 1386 5650 1991 5 1422 1194 1191 1216 1094 1210 1129 1282 1376 1315 1482 1433 1281 5650 1992 1 1377 1398 1302 1168 1167 1212 1233 1355 1385 1247 1501 1508 1321 5650 1993 1688 1264 1258 1166 1085 1126 1213 1255 1214 1221 1320 1483 1275 5650 1994 2 315 1431 1163 1397 1195 1130 1291 1216 1237 1278 1357 1437 1567 1315 5650 1995 5 4 5 1478 1527 1353 1122 1160 1101 1227 1195 1237 1538 1355 1255 1297 5650 1996 3 1281 1188 1094 1160 1109 1193 1180 1186 1174 1412 1379 1287 1221 5650 1997 1319 1549 1333 1184 1132 1136 1112 1260 1415 1380 1368 1350 1293 5650 1998 2 1403 1506 1287 1160 1145 1155 1302 1349 1287 1452 1418 1482 1328 5650 1999 1474 1414 1289 1216 1212 1227 1283 1156 1441 1413 1489 1452 1338 5650 2000 431 XX 1398 1486 1248 1138 1190 1246 111499999 1324 1480 1501 1543 1336 5650 2001 1403 1281 1299 1218 1143 1158 1191 1347 1253 1518 1410 1302 1294 5650 2002 1485 1548 1322 1252 1251 1389 1271 1262 1298 1334 1369 1239 1333 5650 2003 1416 1277 1275 1174 1252 1300 1248 1294 1328 1351 1464 1415 1316 5650 2004 1435 1301 1250 1220 1211 1206 1212 1266 1458 1424 1398 1564 1329 5650 2005 1524 1202 1181 1226 1212 1209 1235 1258 1449 1448 1514 1357 1319 5650 2006 1350 1232 1169 1275 1205 1191 1228 1238 1393 1430 1611 1574 1325 5650 2007 1546 1325 1296 1182 1282 1187 1272 1351 1378 1415 1349 1446 1337 5650 2008 1499 1475 1396 1199 1140 1230 1246 1339 1350 1574 1437 1354 1353 5650 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Alesund 040/191 RLR(1964) is 10.9m below BM No129 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Alesund 040/191 RLR(1964) is 10.9m below BM No129 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1986 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : A search was made on the Norwegian website to see if the datum issue could be resolved. From looking at the datasets it became obvious that they had been totally revised. Datum figures were found on the web and applied to the data. RLR was recalculated for 2008. There is still a query on the very early data which still needs confirming with the authority. KJOLSDAL 040201 61 55 N 05 38 E04241964 50 8 0 0 1935 -2082-1916-2171-2169-2281-2114-2013-2060-1935-1803-1878-1956-2032 9139 1936 -1962-2034-2152-2203-2292-2186-2033-1993-2073-2005-1949-1793-2056 9139 1937 -1913-2002-2200-2150-2160-2058-2032-2078-1925-1986-1993-2093-2049 9139 1938 -1867-2124-1917-2182-2167-2005-2022-2027-2088-1756-1711-1930-1983 9139 1939 3128 - 9999999999-2145-2130-2236-2196-2079-2062-2067-2128-1901-205999999 9139 1940 -2159-2168-2140-2203-2204-2158-2119-2106-1984-2015-1888-2022-2098 9139 1941 31 31 - 99999-2082-2238-2280-2238-2161-2092-2011-214099999-2103-190099999 9139 1943 28 3031 - -194199999-1992-1904-2031-2035-2108-2021-1898-1762999999999999999 9139 1945 -2120-1964-2087-2078-2105-2017-2042-2132-2008-2010-1991-1941-2041 9139 1946 -1922-2060-2106-2009-2162-1944-1943-1873-1773-2024-1936-1974-1977 9139 1947 -2038-2258-2052-2023-2228-2055-2003-2111-1939-1955-1844-2100-2051 9139 1948 -1963-2330-2102-2071-2152-2076-2081-2048-1847-1813-1905-1783-2014 9139 1949 -1897-1904-2243-2149-2079-2069-2151-2042-1918-1668-1709-1779-1967 9139 1950 -2030-1951-2075-2015-2255-2064-2023-1907-1761-1809-1923-2040-1988 9139 1951 -2035-2075-2145-2097-2243-2175-2092-2001-1885-1948-1914-1726-2028 9139 1952 -1896-2053-2064-2129-2155-2016-2023-2009-2026-1968-2049-2004-2033 9139 1953 -2022-2056-2056-1982-2095-2133-1916-1847-1869-1848-1764-1934-1960 9139 1954 -2088-2138-2140-2192-2244-2114-2055-2018-1870-1817-1862-1819-2030 9139 1955 31 3131 - 99999-2152-2147-2248-2158-21839999999999-1895-1880-1920-181099999 9139 1956 3130 - -1822-2284-2110-21509999999999-2045-2007-1968-1798-1893-179699999 9139 1957 313031 - -1844-1963-2064-2114-2150-2151-2065-2048-184599999999999999999999 9139 1958 303130313130 - -2002-2062-2239999999999999999999999999999999-2104-1959-193799999 9139 1959 22 -42 -13 21 -110 -9 30 -37 -89 45 47 69 -6 7126 1960 -9 58 -127 -58 -150 -37 -65 62 37 -11 152 36 -9 7126 1961 35 159 155 32 -5 98 25 46 127 185 166 106 94 7126 1962 213 -44 -137 -187 -253 -108 -221 11 16 68 -32 -23 -59 7126 1963 3130 - -278 -172 -131 -230 -113 -196 -171 -58 709999999999 21299999 7126 1965 31283130313031 - 99999999999999999999999999999999999 43 121 133 56 5599999 7126 1966 31 XX -88 -16 -64 -263 -126 -6499999 -84 153 39 13 132 -34 7126 1968 6 XX -37 -134 -45 -189 -217 -29 -143 -169 -58 97 22 -27 -78 7126 1969 XX XX 15 5 -26 -134 -180 -203 -188 -129 -21 -57 -53 100 235 135 -43 7126 1970 XX 310 4 -14 -31 -80 -96 -107 -162 -16 -56 84 115 71 -12 -25 7126 1971 4 XX30 5 XX XX 121 -29 -14299999 -106 -137 -165 -42 -60 64 141 133 -21 7126 1972 31 XX 1 31 - 99999 -177 -170 -112 -177 0 -78 -68 -131 -46 1599999999999 7126 1973 11 -10 61 -53 -166 -164 -57 -109 -90 -7 -46 118 29 -43 7126 1974 6 115 -40 -214 -284 -186 -125 -70 -19 173 -63 60 268 -32 7126 1975 9XX 253 -65 -99 -203 -207 -184 -102 -94 155 78 53 44 -32 7126 1976 3129313014 - 99999999999999999999 -155 -98 -105 -213 -226 7 56 2899999 7126 1977 -34 -78 -78 -134 -262 -204 -198 -182 -60 102 177 24 -78 7126 1978 -19 -183 -26 -232 -234 -116 -150 -94 -34 26 208 -68 -76 7126 1979 -104 -157 -49 -210 -133 -87 -80 -62 72 -6 85 108 -51 7126 1980 XX 5 XX -136 -147 -208 -216 -280 -143 -188 -93 56 71 -50 62 -107 7126 1981 XX 5 XX -54 -72 -76 -282 -197 -83 -115 -87 -15 165 164 23 -52 7126 1982 -23 14 -21 -137 -141 -210 -161 -8 153 104 236 193 0 7126 1983 XX 4 1 11 7XX XX 300 -194 -47 -131 -37 -104 -100 -117 -5 299 160 101 8 7126 1984 3031303131303130 - 19 -188 -3549999999999999999999999999999999999999999 9999999 7126 1985 312814 - 9999999999 -74 -127 -213 -142 -80 77 22 78 -28 4899999 7126 1986 11 8 15 -234 16 -259 18 -118 -80 -107 -49 -178 219 194 -46 7126 1987 858 929 771 817 826 812 886 878 1126 1157 1056 1097 934 6126 1988 8 313031 - 1141 970 895 831 839 835 1026 1122 117199999999999999999999 6126 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Kjolsdal 040/201 RLR(1964) is 8.7m below BM B29N16 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Kjolsdal 040/201 RLR(1964) is 8.7m below BM B29N16 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 10-OCT-94 : 1988 gauge taken out of service MALOY 040211 61 56 N 05 07 E04242008235 66 18 0 0 1943 312831303130 1 - 999999999999999999999999999999 1078 1161 1293 1372 1261 124899999 5785 1944 1 2 2 231XX 1340 1098 1065 1063 992 1089 1071 1103 1147 1289 132499999 1143 5785 1945 312810 11 1 - 9999999999 1091 1095 1059 1093 1075 1006 1091 1156 1213 126299999 5785 1946 2 61231 6 811 XX 1263 1166 1063 1128 975 117999999 1254 1371 1157 1221 1162 1177 5785 1947 11 1089 918 1047 1110 866 991 1058 941 1139 1111 1244 1092 1057 5785 1948 1 1184 1003 1062 1052 952 1051 1041 1040 1236 1256 1205 1287 1115 5785 1949 528 4 110 2 XX 123299999 931 1101 982 903 883 1016 1135 1277 1283 1318 1103 5785 1950 5 6 1048 1148 1057 1093 892 1053 1047 1206 1373 1297 1237 1129 1132 5785 1951 1411 1 1 1150 1097 1048 1110 882 920 990 1137 1215 1167 1222 1366 1115 5785 1952 10303130 1 1 915 - 1229 1065 1045999999999999999 1025 1048 1052 1136 1062 111599999 5785 1953 3 1 1127 1076 1015 1085 1020 992 1120 1211 1225 1257 1373 1284 1150 5785 1954 5 1099 1049 1045 957 928 1030 1106 1150 1317 1338 1297 1313 1139 5785 1955 1209 1095 997 990 1041 975 1005 969 1224 1240 1212 1300 1105 5785 1956 2 1150 900 995 986 1054 1029 1006 1052 1118 1265 1195 1276 1087 5785 1957 1237 1227 1139 973 946 960 1016 1060 1223 1325 1225 1307 1136 5785 1958 6 3 2 7 21331XX 1227 1155 988 1006 1060 983 1036 1172 1188 1309 125099999 1117 5785 1959 -387 -425 -401 -376 -578 -473 -440 -438 -462 -371 -335 -316 -417 5785 1960 -496 -527 -571 -585 -614 -568 -528 -432 -479 -481 -327 -328 -495 5785 1961 31 2 2 XX 99999 1193 1157 1053 1024 1081 1048 1144 1259 1307 1293 1249 1165 5785 1962 31 XX 99999 1065 985 945 970 1008 960 1178 1198 1240 1144 1169 1079 5785 1963 3 934 1013 1044 976 1024 956 986 1112 1217 1280 1268 1180 1084 5785 1964 1121 1080 945 1004 1085 1087 1139 1086 1158 1161 1239 1225 1111 5785 1965 6 711 1185 930 1003 1007 963 1078 1013 1064 1233 1258 1211 1209 1088 5785 1966 1210 2 1047 1178 1118 957 1013 1057 1089 1044 1218 1236 1180 1317 1121 5785 1967 3 1079 1206 1301 1023 1047 1058 1159 1169 1246 1454 1282 1229 1189 5785 1968 1179 1076 1142 994 943 1079 959 937 1071 1292 1201 1166 1087 5785 1969 31 XX 1128 105399999 1013 1005 1012 1108 1087 1127 1277 1347 1120 1117 5785 1970 6 4 1151 1119 1073 1056 1034 1007 1143 1092 1236 1265 1261 1149 1134 5785 1971 21412 1260 1155 1060 1033 1080 1014 1071 1130 1113 1249 1273 1290 1153 5785 1972 3 1 1105 1042 1042 1046 1014 1178 1089 1100 1058 1125 1312 1351 1123 5785 1973 1 3 1174 1210 1101 1009 1025 1090 1077 1076 1164 1135 1262 1211 1127 5785 1974 13 3 4 2 1315 1172 967 918 962 1043 1097 1139 1317 1122 1254 1436 1155 5785 1975 2 5 1 931 7 XX 1425 1102 987 933 914 916 982 1000 129499999 1154 1169 1073 5785 1976 4 5 6 7 4 1167 1063 1038 957 991 1026 1020 927 925 1175 1166 1123 1046 5785 1977 10 3 6 9 6 XX 1128 1089 1081 1022 887 932 936 960 1071 1245 1314 1180 1072 5785 1978 283130 411 4 - 1156999999999999999 911 1012 987 1026 1109 1175 1328 113299999 5785 1979 4 1031 23131 - 1096 1041 1155 91299999 10669999999999 1166 1116 1209 123999999 5785 1980 312910 630 1 - 9999999999 885 943 915 1036 985 109699999 1249 1174 125699999 5785 1981 12 2 1162 1124 1118 915 992 1053 1025 1064 1166 1333 1327 1206 1123 5785 1982 1135 1204 1153 1019 1023 949 1013 1168 1305 1279 1417 1362 1169 5785 1983 31XX 1420 982 1141 1046 1120 1018 1046 1023 1164 1398 130299999 1153 5785 1984 31 XX 99999 1034 914 1009 971 966 958 960 1082 1302 1304 1229 1066 5785 1985 28 4 XX 112699999 1073 1031 944 995 1078 1224 1181 1195 1128 1240 1111 5785 1986 30 2 2 30 2 - 1181 882 116299999 1164 1029 1098 1079 1141 133999999 135499999 5785 1987 3 3 1 1022 1091 997 1005 968 960 1014 1041 1289 1324 1235 1254 1099 5785 1988 3 9 2 1327 1179 1080 988 970 986 1132 1171 1317 1272 1211 1238 1156 5785 1989 1 8 1 110 1362 1400 1252 1029 1067 1000 1000 1169 1218 1301 1239 1282 1194 5785 1990 631 8 3 2XX 1402 1510 1291 1102 943 103199999 1147 1201 1299 1162 1226 1214 5785 1991 1216 1003 1006 1019 894 1018 969 1106 1175 1144 1303 1230 1091 5785 1992 8 1 1 2 4 1083 1199 1118 1010 1003 1048 1058 1193 1227 1084 1335 1301 1136 5785 1993 1 2 2 4 3 2 1457 1073 1074 1025 945 965 1041 1103 1065 1068 1157 1316 1111 5785 1994 4 2 5 410 1 1256 989 1203 1025 983 1103 1032 1076 1069 1175 1253 1384 1135 5785 1995 12 1281 1333 1145 972 993 946 1073 1000 1084 1359 1183 1075 1119 5785 1996 2 1098 1026 914 983 945 1019 1004 1034 1019 1254 1223 1121 1054 5785 1997 1128 1356 1135 1000 977 995 978 1104 1223 1199 1197 1178 1121 5785 1998 5 1234 1309 1105 1011 980 1005 1135 1180 1125 1280 1244 1287 1158 5785 1999 1304 1219 1114 1048 1054 1070 1115 1005 1293 1246 1283 1294 1170 5785 2000 1212 1296 1062 977 1035 1083 965 1022 1168 1331 1347 1372 1155 5785 2001 1226 1094 1126 1040 960 979 1056 1190 1095 1364 1217 1125 1123 5785 2002 1 1300 1363 1139 1090 1113 1229 1098 1116 1127 1171 1201 1066 1166 5785 2003 1229 1107 1098 1013 1093 1145 1099 1124 1134 1181 1291 1224 1145 5785 2004 1261 1118 1075 1055 1044 1047 1058 1130 1289 1267 1214 1368 1161 5785 2005 1328 1016 1016 1061 1049 1042 1080 1086 1277 1286 1349 1179 1148 5785 2006 1146 1058 1011 1113 1048 1015 1067 1103 1232 1294 1445 1393 1161 5785 2007 3 1376 1164 1125 1005 1120 1054 1139 1190 1189 1230 1165 1270 1170 5785 2008 1338 1293 1228 1040 982 1063 1120 1200 1191 1394 1265 1184 1192 5785 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Maloy 040/211 RLR(1964) is 10.1m below BM No7 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Maloy 040/211 RLR(1964) is 10.1m below BM No7 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : prior to 1978 fcode=C =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1986 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset for Maloy now refers to TGBM A29 N26 6.615m above TGZ. A RLR value for 2008 was calculated. BERGEN 040221 60 24 N 05 18 E04241964 99 8 0 0 1883 -76 -122 -270 -248 -160 1 148 196 188 251 321 195 35 6989 1884 290 160 -57 -34 23 -16 37 78 152 150 69 168 85 6989 1885 29 149 -11 -7 69 78 18 72 202 194 175 209 98 6989 1886 138 -85 24 57 54 111 149 216 224 202 242 263 133 6989 1887 303130 - 206 117 11999999999999999 -15 69 109 113 110 16899999 6989 1888 30 XX -7 -145 -92 -125 -29 -7 58 3499999 70 230 202 17 6989 1889 80 18 13 -27 37 58 24 94 108 160 161 184 76 6989 1915 4283130 3 - -28999999999999999 -115 -100 -34 -2 -74 -101 -68 -899999 99999 1916 1 1 1 2 1 1 4 228 33 -108 -111 -91 -15 -71 -94 -67 72 232 186 15 99999 1917 1 2 1 2 4 -11 11 -71 -95 -161 -72 -95 3 166 184 203 46 7 99999 1918 810 3 4 1 1 4XX 47 57 -88 -144 -125 -109 -150 -99 21 32 98 123 -28 99999 1919 1 5 6 3 310 6 912 5XX -62 -140 -106 -59 -169 -121 -162 -42 16 -18 81 -13 -74 99999 1920 2 1413 530 7 4 XX 242 200 141 107 121 -35 20 -1299999 -46 67 73 92 99999 1921 8 4 1 912 5 3 1XX 221 -127 110 -192 -59 -108 -172 21 -21 68 60 184 4 99999 1922 813 2 1 3 1 1 1 1XX 60 46 27 -47 6 -69 -59 80 40 -21 108 120 23 99999 1923 2 31 1 6XX 85 87 -148 47 -12 -3799999 57 182 276 174 117 74 99999 1924 4 4 1 3 3 47 -27 -94 -65 -29 -11 91 117 201 159 91 229 61 99999 1925 4 2 4 13 7 2 3 XX 240 146 -96 -68 -44 24 -43 -10 95 110 52 192 52 99999 1926 4 4 3 3 2 610 1 8XX 45 17 31 -14 -47 47 -54 62 95 107 211 65 46 99999 1927 4 6 1 3 812 6 4 6 XX 203 -10 13 42 -72 0 28 128 200 196 141 -33 69 99999 1928 4 11 5 8 4 6 5 5 6 XX 130 23 -70 -25 -95 30 78 96 60 183 204 105 66 6989 1929 6 1 -128 -106 -100 -95 -93 -17 -20 72 137 241 213 294 36 6989 1930 215 -137 -17 -84 -20 1 27 81 72 242 208 89 58 6989 1931 4 5 1 1 1 6 2 92 26 -50 -58 -36 19 174 74 -25 67 177 153 55 6989 1932 264 -81 -20 19 27 -63 56 17 138 218 148 200 78 6989 1933 30 XX 100 29 -11 -50 -67 -12 -14 8 8 5599999 -37 1 6989 1934 108 -6 -67 -183 -20 -58 5 79 193 277 116 143 50 6989 1935 1 -48 148 -125 -62 -188 13 -14 -81 150 267 178 77 25 6989 1936 110 9 6 6 514 12 8XX 127 132 -46 -51 -142 -72 49 -21 -33 86 118 219 25 6989 1937 7 115 6 6 12 4 312 4XX 81 108 -100 -87 -43 1 29 -34 79 33 101 25 18 6989 1938 4 6 6 7 4 2 207 -5 21 -108 -84 -12 2 -12 -9 249 292 100 47 6989 1939 3 6 101315 4 4 6 5 8XX 80 157 -59 -27 -189 -6 34 15 22 -52 115 -6 11 6989 1940 -93 -86 -54 -146 -103 -87 -60 -20 98 97 193 25 -20 6989 1941 3128 4 23031 - 9999999999 72 -178 -161 -47 -32 57 -72 61999999999999999 99999 1944 13 155 -92 -90 -86 -95 21 9 -1 87 128 181 72 20 6989 1945 2831303130313130 - -319999999999999999999999999999999999999999 77 94 14899999 99999 1946 2 131 117 -1 40 -78 113 73 149 205 41 153 116 87 6989 1947 3 9 610 4 4 3 XX 24 -141 -29 -18 -211 -102 26 -107 88 21 174 54 -13 6989 1948 1 12 610 231XX 127 -59 -10 -1 -52 42 20 54 145 253 15799999 54 6989 1949 145 82 -158 9 -97 -49 -102 -33 45 141 197 214 32 6989 1950 30 XX 54 102 -4099999 -123 -8 26 91 210 128 -49 -62 29 6989 1951 631 731 9 5 - -62 4499999 -3799999 -99 -35 55 132 72 200 31199999 6989 1952 3 147 14 -37 -33 2 46 -4 55 50 107 28 53 36 6989 1953 5 1 2 1 -29 -68 -136 -60 -65 -40 34 111 139 127 220 170 36 6989 1954 -17 -117 -42 -120 -110 4 56 84 166 216 172 185 41 6989 1955 2 79 14 -107 -103 -25 -53 -38 -73 123 174 142 209 29 6989 1956 312931303130 - 999999999999999999999999999999 -15 58 50 134 75 13299999 6989 1957 4 3 1 1 50 119 15 -142 -133 -84 -39 -9 100 146 76 152 19 6989 1958 2 1 1 2 1 56 38 -136 -142 -72 -62 -6 89 101 181 47 138 20 6989 1959 2 2 44 -69 -21 21 -89 -45 -14 -31 -70 49 72 94 -4 6990 1960 529 5 1 3 3 4 1 XX -2099999 -144 -137 -152 -91 -52 53 18 45 157 127 -16 6990 1961 4 1 1 1 1 1 -18 33 38 -59 -28 -2 -13 53 108 190 182 101 50 6990 1962 1 1 1 166 -50 -114 -146 -79 -54 -49 100 83 86 48 44 3 6990 1963 7 712 9 5XX -144 -93 -74 -114 -76 -68 -85 -12 78 109 166 14 -38 6990 1964 3 131 3 1 2 4 XX -10 -2499999 -108 2 17 6 -4 89 43 111 95 21 6990 1965 3 4 3 6 4 4 4 1 83 -144 -116 -118 -75 12 -40 -22 111 128 67 106 -1 6990 1966 4 230 5 2XX -49 26 -3399999 -108 -31 -41 -32 86 81 80 160 10 6990 1967 5 7 6 3 3 4 -31 57 180 -127 -50 -30 31 71 104 337 167 123 69 6990 1968 8 67 -43 18 -101 -116 -14 -96 -133 22 169 94 15 -11 6990 1969 2 1 25 -74 -138 -137 -99 -83 -50 -15 -23 121 211 -48 -26 6990 1970 12 3011 2 XX -39 -24 -65 -110 -12399999 24 23 93 107 133 -12 1 6990 1971 1 3 3 13130 3 - 108 -8 -105 -105 -75 -44 -90 -6 -539999999999 6499999 6990 1972 2 530 6 XX -89 -106 -12299999 -70 26 -68 -109 -142 -33 148 138 -37 6990 1973 11 2 -9 42 -86 -117 -96 -75 -10 -68 11 -28 121 72 -19 6990 1974 108 5 -180 -242 -126 -76 -23 -13 161 19 111 253 0 6990 1975 2 2 XX 234 -61 -73 -150 -137 -141 -60 -36 91 43 18 59 -17 6990 1976 83 -81 -100 -150 -108 -79 -76 -189 -139 61 84 45 -54 6990 1977 1 3 -1 -39 -70 -71 -170 -140 -140 -110 -39 120 221 57 -32 6990 1978 8 31 -73 20 -172 -174 -40 -45 -41 19 45 174 22 -18 6990 1979 -38 -59 23 -120 -86 -44 -50 15 48 9 93 148 -5 6990 1980 -78 -92 -145 -154 -175 -57 -76 14 96 177 88 184 -18 6990 1981 45 24 -19 -177 -81 -22 -25 -54 48 209 201 123 23 6990 1982 15 40 -11 -93 -93 -59 -68 30 168 135 241 200 42 6990 1983 282 -127 -4 -64 14 -80 -81 -134 57 259 179 155 40 6990 1984 120 -119 -171 -145 -132 -92 -140 -157 -11 190 186 94 -31 6990 1985 40 -20 -107 -103 -169 -107 -67 52 15 -2 -14 86 -33 6990 1986 31 -256 -29 -188 -13 -78 -25 -35 1 158 220 221 3 6990 1987 -71 5 -114 -58 -61 -12 -77 -22 128 182 118 132 12 6990 1988 3131 6 1 1 - 191 101 16 -81 -65 -289999999999 88 114 118 12899999 6990 1989 1 513 13 3 XX 192 233 98 -67 -68 -8 -88 51 75 96 147 170 74 6990 1990 1 228 333 133 -29 -124 -22 -6 20 84 169 70 95 78 6990 1991 2 3 78 -108 -108 -94 -175 -41 -79 -22 34 47 161 84 -18 6990 1992 1 19 46 -11 -74 -102 -46 -49 87 94 10 200 140 25 6990 1993 2 3 4 4 278 -80 -85 -109 -108 -70 -53 -11 -12 -24 -2 179 -11 6990 1994 3 2 3 2 3 1 1 131 -130 64 -96 -53 -5 -67 -14 57 47 142 238 28 6990 1995 5 2 4 210 2 122 195 23 -133 -90 -89 -43 -114 3 185 79 -29 11 6990 1996 -25 -95 -191 -135 -108 -82 -96 -72 -82 110 135 10 -52 6990 1997 -15 188 -15 -94 -93 -51 -86 -33 70 86 76 69 7 6990 1998 122 161 -51 -50 -111 -54 53 61 33 160 94 132 45 6990 1999 2 147 72 -31 -54 -36 -32 -9 -31 153 116 110 192 50 6990 2000 30 XX 73 145 -47 -105 -4099999 -53 -41 76 199 233 237 61 6990 2001 103 -22 -1 -85 -140 -105 -32 49 22 235 92 15 12 6990 2002 154 224 9 -46 17 80 -2 16 7 70 82 -63 44 6990 2003 100 -41 -57 -104 -19 43 7 17 9 65 121 84 19 6990 2004 87 -5 -68 -78 -43 -28 -19 41 136 132 80 189 36 6990 2005 177 -122 -101 -56 -56 -44 -6 -8 97 124 206 49 22 6990 2006 -44 -61 -95 -26 -53 -108 -73 8 79 179 295 226 28 6990 2007 234 36 -6 -113 8 6 63 53 39 56 51 121 46 6990 2008 1 181 131 99 -58 -85 -17 43 89 45 220 131 31 68 6990 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Bergen 040/221 RLR(1964) is 9.7m below BM B33 N90 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Bergen 040/221 RLR(1964) is 9.7m below BM B33 N90 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1988 HAUGESUND 040251 59 25 N 05 11 E03249999 1 0 0 0 1958 31XX -1255-1257-1429-1442-1411-1405-1344-1217-1217-1154-127699999-1310 99999 STAVANGER 040261 58 58 N 05 44 E04242008 89 18 0 0 1881 3128313031 - 9999999999999999999999999 524 635 640 606 678 871 72799999 99999 1882 31 XX 584 557 545 48499999 531 604 669 675 682 738 545 601 99999 1883 30 XX 675 625 469 538 60499999 529 690 595 653 702 523 600 99999 1884 3129 30 31 - 9999999999 501 665 658 582 692 66699999 661 5799999999999 99999 1885 31 31 - 554 746 505 42899999 486 481 535 644 629 6149999999999 99999 1919 9 5 6 3 2 11 2 6XX 889 934 863 785 731 800 840 912 973 920 940 1061 885 6003 1920 31 10 4 1331 4 1 - 99999 958 920 930 863 855 94699999 917 912 1002 94099999 6003 1921 5 9 1123 924 978 765 846 813 812 940 940 977 835 1047 919 6003 1922 9 6 3131 2 - 849 762 807 0 880 8729999999999 932 877 948 102599999 6003 1923 31 6 XX 980 859 737 849 866 86299999 982 999 1151 1055 937 934 6003 1924 1 1 1 14 897 833 765 777 897 871 966 1009 1055 1042 927 1080 921 6003 1925 6 4 6 8 1 6 13XX 1039 1027 778 828 951 914 891 1020 1013 1006 973 1126 959 6003 1926 415 915 9 1510 7 410 9XX 960 954 805 920 913 965 876 924 1000 1045 1107 960 956 6003 1927 81013 312 811 8 113 5 9XX 1053 889 997 935 806 950 1092 1065 1070 1058 1086 917 998 6003 1928 1315 7 41330 23114 931 - 1024 926 797 880 79999999 97599999 963 1081 10809999999999 6003 1929 115 51314 9 5 8XX 797 802 740 826 858 871 903 979 990 1149 1109 1249 952 6003 1930 6 8 4 1 330 XX 1166 770 872 863 881 868 952 103699999 1126 1109 978 969 6003 1931 9 1 15 1004 863 860 832 924 862 933 922 845 1027 1061 1058 928 6003 1932 5 6 1103 788 883 956 943 869 994 944 1035 1112 1025 1137 980 6003 1933 3 6 2 30 4XX 1070 994 904 842 874 937 898 1026 945 099999 848 842 6003 1934 1 1030 866 868 810 872 848 907 1088 1066 1120 960 1043 958 6003 1935 4 4 315 7 XX 899 1007 805 788 730 872 868 898 1081 1147 1085 1054 947 6003 1936 5 10 7 7 1066 918 816 870 776 798 997 940 861 986 1004 1171 930 6003 1937 1 1 5 8 8 949 1064 883 884 875 899 931 938 967 907 966 898 930 6003 1938 5 1 8 1009 813 964 805 842 947 913 933 958 1160 1170 951 957 6003 1939 8 1 1 1014 983 830 837 769 806 909 921 924 859 1018 900 898 6003 1946 3115 30 1 - 99999 930 888 886 852 1020 987 104399999 950 1054 99199999 6003 1947 8 8 3 113 1 9XX 822 764 900 902 762 886 900 789 954 847 968 997 873 6003 1948 4 1 5 3 4 6 6 5 3 XX 1085 943 893 934 868 956 966 1022 1125 1117 1052 1068 1001 6003 1949 2 1 3 2 4 5 1 1051 975 751 946 847 871 839 945 1036 1060 1008 1031 946 6003 1950 1 6 7 1 2 6 1 1 8 2 1 8XX 840 955 778 838 726 800 880 934 1044 980 947 858 880 6003 1951 2 2 5 4 2 2 2 3 8XX 971 952 949 871 779 845 877 1016 1041 966 1104 1155 956 6003 1952 7 2 1 2 2 4 2 1 4 1 3 1020 910 843 876 878 921 875 948 939 1008 947 985 927 6003 1953 3 5 4 3 5 1 5 961 873 775 887 891 924 964 1027 1048 1028 1111 1063 965 6003 1954 1 4 2 4 7 890 773 933 809 831 923 1009 1042 1118 1153 1075 1124 972 6003 1955 3 4 5 4 2 2 4 1 989 891 788 785 834 842 862 869 1014 1033 1020 1087 917 6003 1956 7 1 1 1 3 2 936 727 871 807 863 843 876 976 959 1023 958 1013 906 6003 1957 328 4 5 1 5 2XX 98699999 978 762 806 831 876 935 1045 1080 997 1085 944 6003 1958 4 4 3 978 980 805 804 831 854 906 1006 1000 1055 943 1052 937 6003 1959 8 7 1 1 992 852 891 990 788 817 907 905 827 985 953 1012 911 6003 1960 7 1 3 5 963 903 793 774 749 832 939 970 949 1018 1105 1035 919 6003 1961 8 7 1 5 830 8XX 932 992 950 890 891 916 960 1014 1070 109999999 974 967 6003 1962 4 4 8 2 9 511 4 XX 1108 865 844 814 892 855 923 1029 1033 992 990 954 942 6003 1963 6 2 2 5 3 1 784 801 820 803 842 859 860 974 987 1055 1130 991 912 6003 1964 1 1 893 880 799 829 905 905 948 933 983 988 1045 1042 929 6003 1965 3 15 2 113 3 XX 1034 795 829 892 815 865 937 940 1051 989 1012 1058 942 6003 1966 1 1 2 7 922 1042 917 809 864 888 900 960 958 1050 1033 1083 952 6003 1967 6 2 1 896 997 1079 827 921 876 941 1003 1058 1223 1062 1049 994 6003 1968 4 5 969 852 923 830 854 912 848 825 1031 1087 1019 977 927 6003 1969 14 1 1 3 1 4 8 3 3XX 977 909 781 821 858 890 851 1012 866 1033 1153 856 914 6003 1970 XX 6 930313031 - -51 8 -111 -101 -174 -179 -22 -449999999999999999999999999 6003 1971 31283130 2 2 1 7 2 6 - 99999999999999999999 852 841 791 928 869 991 1018 99699999 6003 1972 1 1 1031 2 2XX 815 888 837 895 878 941 88199999 841 903 1102 1107 916 6003 1973 976 963 841 819 852 867 911 858 954 907 1075 1024 920 6003 1974 313031 5 5 - 1063 988 838 745 860 887 943999999999999999 1066 116799999 6003 1975 1153 899 920 844 797 811 875 922 1021 976 978 993 933 6003 1976 3 1 990 841 853 762 842 816 842 762 839 1030 1032 973 881 6003 1977 5 2 1 920 910 900 867 751 776 788 859 925 1060 1153 962 906 6003 1978 947 841 971 785 777 854 893 899 959 955 1070 931 907 6003 1979 5 1310 936 904 937 818 831 869 849 972 1020 951 1064 1060 931 6003 1980 859 879 821 773 758 910 893 958 1001 1048 973 1045 910 6003 1981 6 913 882 985 747 853 896 915 863 1032 1122 1092 1044 943 6003 1982 3 952 1004 939 824 821 868 852 968 1049 1045 1170 1119 965 6003 1983 1186 791 934 941 988 858 849 807 1024 1150 1065 1060 973 6003 1984 8 1012 856 787 829 844 874 829 827 963 1089 1081 1051 918 6003 1985 2 6 1 3 993 905 860 877 832 842 932 1043 970 962 997 1065 942 6003 1986 2 9 4 1005 737 960 858 940 860 902 954 952 1086 1112 1121 962 6003 1987 30 13XX 840 885 832 893 810 875 928 99199999 1107 1072 1040 930 6003 1988 8 1 1 1102 1043 938 823 864 867 1010 1044 1052 1021 1032 1041 990 6003 1989 1 1090 1141 1030 885 839 864 835 999 976 1021 1069 1094 986 6003 1990 1 1162 1261 1027 897 803 915 922 965 993 1077 1027 991 1002 6003 1991 998 832 845 854 769 905 884 918 955 1001 1083 1001 921 6003 1992 929 957 897 873 827 880 852 1024 1003 943 1102 1036 943 6003 1993 1 1169 836 844 839 853 823 880 946 950 890 963 1105 926 6003 1994 1050 778 987 870 901 867 863 923 995 957 1040 1150 950 6003 1995 1019 1096 951 811 845 856 874 819 981 1113 996 874 935 6003 1996 5 925 825 743 812 841 836 855 892 891 1019 1068 937 886 6003 1997 902 1083 900 810 860 915 871 912 986 1012 996 1037 939 6003 1998 1076 1056 860 924 825 913 1004 989 1016 1086 1016 1063 985 6003 1999 1088 993 924 890 891 904 904 958 1101 1047 1036 1123 988 6003 2000 1 996 1056 875 873 899 915 911 909 1015 1168 1142 1175 994 6003 2001 1064 900 970 885 791 834 944 988 993 1172 1028 952 961 6003 2002 1 1104 1172 958 953 1003 1001 949 1011 948 1006 1038 883 1001 6003 2003 1066 921 910 859 932 973 987 956 987 1014 1085 1029 977 6003 2004 1041 950 888 907 903 916 958 1014 1081 1090 1019 1107 990 6003 2005 1 1 1 1097 819 861 914 872 886 927 990 1034 1081 1151 971 968 6003 2006 1 1 1 904 938 874 914 900 844 901 996 1052 1128 1224 1161 986 6003 2007 1 1 1 1164 968 991 812 949 946 1025 989 974 1002 1016 1078 994 6003 2008 1 1141 1065 1051 933 863 921 1010 1035 988 1142 1067 964 1015 6003 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Stavanger 040/261 RLR(1964) is 9.9m below BM B38N16 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Stavanger 040/261 RLR(1964) is 9.9m below BM B38N16 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1987 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset for Stavanger now refers to TGBM B38 N37 9.697m above TGZ. A value for RLR 2008 was calculated. ARENDAL 040271 58 27 N 08 47 E03249999 4 0 0 0 1886 28 313031 - 98799999 924 928 875 988 1045 1071 105699999999999999999999 99999 1887 31 XX 977 90299999 871 915 967 986 1050 1054 1056 1000 1093 989 99999 1888 31 XX 99999 760 829 805 937 940 1031 1016 968 1055 1058 1073 952 99999 1889 967 949 909 859 936 963 1043 1083 1062 1035 1084 1007 991 99999 JOSSINGFORD 040281 58 20 N 06 22 E03249999 1 0 0 0 1956 312931 - 999999999999999-3399-3377-3363-3338-3232-3304-3240-3277-318999999 99999 HORTEN 040291 59 25 N 10 29 E04249999 1 0 0 0 1934 1201 1130 987 934 1124 1073 1083 1230 1236 1363 1114 1103 1131 99999 TREGDE 040301 58 00 N 07 34 E04242008321 82 21 0 0 1927 31283130313031313011 1 2 - 999999999999999999999999999999999999999999999 1120 1062 99099999 5984 1928 8 2 6 1 2 130 4 XX 1041 1028 889 978 919 990 1038 106399999 1121 1156 1029 1023 5984 1929 1 3 6 883 826 872 919 926 970 992 1031 1042 1150 1143 1160 990 5984 1930 1144 854 947 924 949 908 1029 1045 1043 1136 1169 1015 1015 5984 1931 1 3 1086 949 918 921 991 958 1086 1091 988 1103 1096 1117 1026 5984 1932 6 9 3 1122 884 931 970 981 967 1041 1014 1110 1170 1007 1078 1025 5984 1933 1 9 1031 990 924 906 950 1010 967 1046 1006 1037 1008 932 983 5984 1934 8 1 3 1049 952 958 905 948 979 979 1059 1066 1278 1154 1213 1044 5984 1935 2 1 1000 1109 874 972 865 964 1021 1011 1146 1201 1133 1113 1032 5984 1936 1 1150 1000 878 972 903 945 1058 1025 995 1098 1074 1159 1021 5984 1937 3 949 1134 932 973 941 986 1013 1003 1071 992 1079 941 999 5984 1938 2 1 2 1109 931 1055 915 945 1025 1026 1052 949 1147 1168 1063 1032 5984 1939 1 1 1094 1027 914 945 903 922 1035 1015 1026 967 1049 969 988 5984 1940 2 5 884 847 926 866 901 924 970 1019 1095 994 1159 1093 971 5984 1941 31 2 30 3 1 - 99999 0 872 804 85399999 0 1088 971 1072 882 110599999 5984 1942 312831 3 2 - 999999999999999 888 933 955 989 1011 1079 1124 1071 113999999 5984 1943 1 1043 1072 933 1037 929 991 1040 1080 1083 1120 1097 1012 1036 5984 1944 5303114 313031 2 - 1104 905 9609999999999 1011 1060999999999999999 1121 106899999 5984 1945 1 989 1017 941 974 1006 1018 1041 1053 1047 1080 1036 1114 1027 5984 1946 2 2 2 1051 1071 912 955 983 1057 1035 1090 1136 1021 1095 1002 1033 5984 1947 11 938 794 1015 959 844 939 992 935 1026 959 1124 1012 961 5984 1948 1045 931 926 957 929 1044 1045 1093 1135 1118 1070 1098 1033 5984 1949 1105 1045 848 1002 942 988 967 1044 1059 1137 1131 1174 1037 5984 1950 2 982 1108 944 1099 930 984 1043 1076 1155 1127 1129 1055 1052 5984 1951 1082 1001 995 940 910 953 979 1050 1083 979 1144 1237 1030 5984 1952 1 1 6 2 6 1080 1009 935 925 955 1005 977 1053 1054 1094 1076 1039 1015 5984 1953 977 907 839 936 962 982 1013 1077 1099 1054 1109 1076 1003 5984 1954 8 935 807 958 850 886 949 1049 1045 1113 1125 1082 1140 998 5984 1955 2 8 5 982 951 863 849 951 930 957 955 1040 1076 1051 1136 977 5984 1956 3 1 15303131303130 - 983 797 902 906 928999999999999999999999999999999 108899999 5984 1957 31 8 XX 1049 1103 944 840 862 91499999 1070 1123 1190 1108 1164 1031 5984 1958 3 5 3 5 1077 1053 898 865 926 943 1031 1100 1091 1103 969 1083 1015 5984 1959 12 8 9 13111 8 XX 1095 879 922 994 862 93699999 989 984 1071 1046 1068 991 5984 1960 2 1009 973 845 873 873 927 1017 1026 1021 1065 1129 1041 983 5984 1961 5 992 1066 1022 980 1046 1012 1081 1089 1089 1161 1127 1051 1060 5984 1962 2 1 1 1223 1023 991 967 1008 1011 1074 1139 1120 1096 1079 1086 1069 5984 1963 7 5 5 912 944 939 931 938 991 984 1081 1007 1150 1239 1078 1018 5984 1964 8 4 3 1007 947 911 948 975 1031 1010 1055 1066 1040 1097 1068 1014 5984 1965 1 1115 907 926 1030 972 1010 1080 1057 1125 1099 1102 1205 1053 5984 1966 3 1 7 937 1103 967 917 939 978 967 986 1032 1019 972 971 981 5984 1967 1 837 1006 1092 908 1013 991 1022 1045 1113 1314 1159 1155 1055 5984 1968 1109 947 1065 925 933 987 1001 1013 1090 1146 1067 1062 1029 5984 1969 3 4 2 2 1030 955 863 959 953 989 943 997 1009 1102 1209 922 994 5984 1970 28 7 9 XX 106599999 946 963 909 951 1089 1004 1045 1092 1132 970 1018 5984 1971 8 2 1070 978 844 904 924 953 941 1014 973 1052 1101 1052 987 5984 1972 6 876 935 902 992 949 1013 986 971 963 983 1141 1119 983 5984 1973 31 3 XX 99999 1032 908 926 932 952 1034 958 1032 1003 1156 1083 1001 5984 1974 1 1093 1004 871 854 911 1001 1063 1024 1151 1066 1093 1229 1030 5984 1975 15 1222 968 988 914 914 938 998 1007 1124 1053 1062 1106 1021 5984 1976 1083 931 932 890 957 921 981 939 973 1106 1135 1067 993 5984 1977 1002 1037 1002 975 893 979 1010 988 1032 1127 1239 1061 1028 5984 1978 1 1045 948 1068 896 925 971 1010 1027 1103 1044 1141 1030 1018 5984 1979 8 1012 1028 989 897 896 947 1010 1053 1061 1005 1135 1105 1011 5984 1980 8 945 936 869 905 884 1009 1006 1046 1034 1124 1040 1095 993 5984 1981 987 954 1039 865 950 992 1004 1000 1078 1169 1199 1129 1031 5984 1982 1019 1011 999 945 949 1018 978 1052 1110 1118 1199 1173 1048 5984 1983 1247 879 1055 1022 1070 959 982 1062 1186 1263 1140 1089 1081 5984 1984 1083 912 882 910 956 948 925 936 1054 1124 1062 1133 994 5984 1985 1017 918 893 911 839 967 965 1028 1055 1009 1049 1109 980 5984 1986 1047 763 953 890 938 939 978 1024 1009 1115 1125 1124 994 5984 1987 4 4 10 854 917 862 874 897 933 991 1033 1083 1083 1096 1153 979 5984 1988 10 3 314 XX 1148 1104 1019 913 929 1018 1025 1112 1090 989 1102 1102 1048 5984 1989 1 9 1 1 1098 1131 1051 950 891 936 955 1077 1025 1087 1122 1165 1039 5984 1990 2 2 6 1 1174 1266 1069 953 893 998 1018 1023 1070 1107 1104 1050 1058 5984 1991 101530 8XX 1043 880 910 922 848 1014 955 99799999 1053 1119 1087 983 5984 1992 14 4 6 2 5 XX 900 998 970 943 910 935 947 1088 1028 1042 1161 1072 1004 5984 1993 5 8 7 1 1158 920 908 913 932 944 994 1030 1027 991 1008 1158 1000 5984 1994 3131 5 2 - 1105 841 1049 925 1013 9549999999999 1074 1056 1123 119299999 5984 1995 9 2 1104 1157 1023 929 946 987 968 985 1053 1126 1039 953 1020 5984 1996 951 889 820 863 945 935 967 965 979 1063 1122 993 958 5984 1997 3 951 1115 945 905 944 1015 942 983 1060 1099 1027 1096 1006 5984 1998 3 4 1085 1086 923 1015 922 988 1099 1073 1074 1134 1072 1095 1046 5984 1999 5 1113 1067 962 963 959 980 978 1071 1123 1084 1084 1170 1046 5984 2000 2 3 1 1052 1099 950 969 961 994 1056 1003 1046 1179 1157 1206 1055 5984 2001 11 4 1089 958 991 962 880 952 990 1042 1079 1193 1104 1034 1017 5984 2002 1128 1207 1005 1004 1038 1011 1021 1045 1039 1041 1052 928 1042 5984 2003 1119 938 947 937 986 1042 1036 1042 1047 1075 1107 1077 1030 5984 2004 1077 1013 954 959 985 1013 1039 1084 1142 1115 1092 1141 1051 5984 2005 1 4 1147 888 902 953 960 993 1039 1089 1073 1087 1140 1052 1027 5984 2006 931 990 929 989 974 953 970 1071 1094 1168 1272 1172 1043 5984 2007 1210 1035 1042 901 1033 1041 1101 1061 1092 1058 1104 1127 1068 5984 2008 1173 1090 1112 994 955 975 1053 1086 1019 1190 1124 1018 1066 5984 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Tregde 040/301 RLR(1964) is 8.7m below BM D40N53 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Tregde 040/301 RLR(1964) is 8.7m below BM D40N53 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1987 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 27-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset is now referred to TGBM D40 N53 which is 2.716m above TGZ. As a result RLR has been re-calculated to be 5984. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : RLR value for Tregde now RLR 2008. HELGEROA 040310 58 59 N 09 52 E04241966 33 20 0 0 1965 312831301515 414 5 131 - 99999999999999999999 821 1082 1025 941 1010 1011 7349999999999 6988 1966 31283130 4 1 5 2 6 6 - 99999999999999999999 947 973 1048 1035 1108 1024 996 103299999 6988 1967 28 2 2 2 5 2 1 2XX 86099999 1134 900 969 1031 1025 1088 1063 1293 1110 1112 1052 6988 1968 1 21030313130 2 2 - 1017 882 1041 944 97099999999999999999999 1106 944 97399999 6988 1969 3 1 4301431 810 1 2 - 909 797 716 834 85999999 98099999 1038 1103 1172 84799999 6988 1981 5 5 3031 - 992 919 990 772 835 969 998 976 1022 1137999999999999999 6988 1982 312831 - 999999999999999 870 902 899 919 1009 1067 982 1143 111899999 6988 1983 8 6 3130 6 - 1243 749 945 878 924 905 9249999999999 1250 1042 103299999 6988 1984 980 774 707 761 785 877 897 864 946 1115 996 974 890 6988 1985 13 3 4 831 799 784 772 776 909 971 1047 1050 998 938 1012 913 6988 1986 42831 14 - 9769999999999 699 866 888 989 947 965 1074 1102 106199999 6988 1987 4 8 8 8 3XX 719 827 776 775 794 920 912 940 1032 1095 1021 1030 899 6988 1988 3 3 1 6 1531 XX 1010 1019 865 790 793 905 1012 1076 105399999 1029 1038 959 6988 1989 11 1 1106 1134 1019 858 867 904 897 1041 971 1022 1034 1041 995 6988 1990 1 1154 1263 1074 907 822 911 964 974 977 1000 971 955 996 6988 1991 3 977 725 757 795 752 935 890 940 997 934 1072 1016 900 6988 1992 4 4 3 938 946 890 841 853 834 916 1016 956 860 1063 1000 925 6988 1993 1201 848 825 781 805 894 959 970 834 841 819 1045 903 6988 1994 310 1000 663 1033 817 850 943 860 912 945 923 1006 1119 924 6988 1995 11 975 1107 960 811 838 906 898 889 906 1069 869 789 919 6988 1996 737 728 632 713 782 863 917 833 811 990 1025 856 824 6988 1997 7 851 1064 895 810 838 868 817 886 1024 996 857 920 903 6988 1998 962 1031 826 834 801 912 1031 1015 922 1063 928 1001 944 6988 1999 1 1009 984 824 847 849 910 934 935 994 976 1007 1091 946 6988 2000 6 1 3 967 1044 864 815 883 923 941 945 913 1069 1060 1087 960 6988 2001 4 934 810 820 804 788 894 921 971 914 1157 1035 886 909 6988 2002 1048 1144 925 874 883 941 947 899 914 864 834 709 914 6988 2003 1013 784 812 765 901 958 923 959 951 947 946 982 913 6988 2004 928 900 819 797 869 930 945 965 1089 973 995 1075 940 6988 2005 1 1083 728 738 817 871 888 940 1009 1004 961 1094 894 920 6988 2006 790 783 722 876 850 851 874 927 983 1058 1199 1145 922 6988 2007 1169 854 914 798 943 913 1047 977 1002 946 980 1032 966 6988 2008 3 1075 1040 988 848 792 923 942 1000 872 1123 1001 860 954 6988 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Helgeroa 040/310 RLR(1966) is 8.3m below BM F38 N29 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-DEC-92 : UP TO 1986 ACODE=03 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Helgeroa 040/310 RLR(1966) is 8.3m below BM F38 N29 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1987 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 27-Oct-2009 : The Norwegian Mapping Authority have revised their datasets. Whole dataset is now referred to TGBM F38 N29 which is 2.312m above TGZ. As a result RLR has been re-calculated to 6988. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Oct-2009 : NEVLUNGHAVN 040311 58 58 N 09 53 E03241964 30 4 0 0 1935 -2785-2650-2911-2850-2932-2759-2685-2738-2595-2544-2654-2720-2735 9800 1936 -2699-2893-2976-2875-2967-2840-2706-2726-2853-2722-2429-2564-2771 9800 1937 -2896-2741-2964-2923-2877-2774-2758-2820-2708-2820-2773-2952-2834 9800 1938 -2683-2889-2674-2863-2846-2722-2749-2738-2762-2547-2520-2773-2730 9800 1939 -2791-2730-2932-2868-2914-2822-2704-2782-2815-2955-2710-2803-2819 9800 1940 31 XX 99999-2961-2921-2999-2932-2892-2766-2732-2634-2804-2609-2821-2825 9800 1941 2831 - -29269999999999-3028-2966-2825-2805-2664-2854-2782-2916-268399999 9800 1943 -2786-2643-2842-2695-2827-2767-2725-2679-2680-2662-2706-2784-2733 9800 1944 -2650-2902-2863-2869-2876-2742-2721-2733-2671-2735-2721-2735-2768 9800 1945 -2880-2788-2822-2805-2794-2694-2720-2759-2735-2709-2810-2723-2769 9800 1946 -2764-2728-2894-2786-2861-2669-2726-2664-2612-2801-2728-2808-2753 9800 1947 -2917-3104-2897-2815-2974-2820-2759-2857-2719-2837-2714-2837-2854 9800 1948 31 XX -2788-2904-2838-2860-2887-2769-2739-2636-265599999-2720-2706-2773 9800 1949 -2666-2779-2985-2793-2857-2821-2819-2724-2781-2659-2737-2598-2768 9800 1950 -2875-2727-2863-2793-2895-2760-2751-2744-2599-2683-2765-2810-2772 9800 1951 -2834-2889-2918-2884-2962-2848-2792-2748-2746-2871-2731-2551-2815 9800 1952 31XX -2757-2828-2955-2897-2887-2763-2811-2744-2727-2812-280599999-2817 9800 1953 -2816-2951-2927-2869-2852-2847-2733-2683-2700-2759-2642-2734-2793 9800 1954 -2910-3029-2914-2967-2989-2812-2725-2726-2628-2649-2734-2629-2809 9800 1955 -2827-2918-2971-2980-2826-2841-2822-2848-2731-2718-2761-2685-2827 9800 1956 29 XX -280599999-2958-2928-2850-2822-2809-2713-2797-2711-2780-2772-2813 9800 1957 -2742-2765-2897-2962-2972-2845-2804-2757-2665-2649-2759-2707-2794 9800 1958 -2847-2838-3035-2965-2900-2860-2789-2757-2800-2708-2821-2753-2839 9800 1959 23 -96 -102 -34 -122 -53 32 -4 -41 56 48 14 -23 6993 1960 30 XX -107 -132 -242 -135 -134 -23 12 -5899999 -130 81 13 -78 6993 1961 -73 25 53 -73 -6 30 104 111 106 193 98 66 53 6993 1962 313031 - 120 -74 -138 -144 -104 -21 -18999999999999999 -27 -1499999 6993 1963 2831 - 2349999999999 -156 -101 -75 -19 -1 40 103 191 999999 6993 1964 31 5 3 1 3XX -20 -103 -227 -132 11 -4 2899999 105 -7 128 23 -18 6993 1965 28 XX 3199999 -206 -127 -130 -16 38 -1 67 43 21 83 -18 6993 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Nevlunghavn 040/311 RLR(1964) is 9.8m below BM F38N3 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Nevlunghavn 040/311 RLR(1964) is 9.8m below BM F38N3 OSLO 040321 59 54 N 10 45 E04242008 101 14 0 0 1885 312831303130 - 999999999999999999999999999999 1155 1097 1272 1201 1157 138299999 6140 1886 1094 851 928 1031 1008 1128 1234 1255 1228 1052 1235 1280 1110 6140 1887 1181 1163 1015 990 1042 1100 1209 1241 1228 1191 1132 1196 1141 6140 1888 1099 867 878 904 1122 1076 1225 1253 1194 1294 1244 1205 1113 6140 1889 1112 1012 990 896 996 1092 1159 1285 1156 1072 1249 1196 1102 6140 1890 1375 953 1106 1013 1023 1127 1312 1272 1198 1328 1140 977 1152 6120 1914 31 6 2 1 1143130 9 - 99999 220 49 74 38 15 399999999999 -80 77 33999999 7266 1915 13 1 931313031 513 - -45 -76 -50 2 -90 -2899999999999999999999 -25 -21499999 7266 1916 1 2 1 292 -3 -225 -73 -48 59 87 37 34 110 178 48 41 7266 1917 3 2 6 1 5 9 2 3 5XX -205 -113 -216 -121 -169 16 -18 42 257 260 229 76 3 7266 1918 31 3 7 131 7 3 - 99999 50 -180 -312 -204 2 1799999 251 97 34 6599999 7266 1919 8 1012 XX -158 -196 -146 -123 -211 -9 -8 118 177 -53 -146 -56 -72 7266 1920 1015 310 2XX 101 73 27 -42 48 -16 226 74 -3 -150 98 -72 29 7266 1921 1 2 31 4 1 1 XX 221 -136 114 -119 -61 -5999999 60 37 124 -74 266 37 7266 1922 9 31 4 4XX -99 -73 -103 -254 -33 7 12399999 -5 -68 102 86 -24 7266 1923 5 3 4 230 6 1 1 5 4 2XX 104 -195 -289 -234 3399999 51 129 170 279 202 22 29 7266 1924 31 3 1214 9 4 12 2XX 99999 -67 -89 -125 -13 -4 176 213 321 201 61 241 77 7266 1925 3 5 211 6 331 410 2 2 4XX 281 89 -169 -71 -86 -2399999 131 156 136 68 189 66 7266 1926 2 3 2 7 431 2 3 1 XX 41 -77 -37 -137 -63 2099999 158 180 162 296 237 78 7266 1927 2 231 XX 297 -28 -58 64 -34 11799999 185 129 234 62 -179 73 7266 1928 4 331 6 31 - 30 4 -261 -213 -236 2199999 87 20 89 969999999999 7266 1929 3 1 831 3XX -270 -383 -165 -156 -129 54 9599999 103 259 213 313 -7 7266 1930 1 3 4 31 XX 290 -171 49 -153 -63 -2099999 50 -70 174 177 -39 25 7266 1931 7 4 31 8 3 XX -74 -72 -263 -231 -136 1599999 -6 -112 130 12 169 -50 7266 1932 2 631 2 XX 245 -147 -172 -52 -190 -16899999 30 209 156 74 68 10 7266 1933 3 731 XX 49 19 -117 -164 -225 -10899999 90 -118 -45 -209 -198 -93 7266 1934 134 31 -137 -233 -17 -65 -90 69 77 213 -36 -77 -11 7266 1935 2 1 -86 144 -229 -165 -246 -16 49 -28 132 266 10 10 -16 7266 1936 2 28 -205 -318 -218 -319 -87 90 60 -167 36 19 250 -67 7266 1937 6 -168 -89 -312 -267 -150 4 10 -96 111 -75 -52 -302 -120 7266 1938 5 3 67 -129 99 -141 -140 42 -4 -5 -6 211 304 -65 22 7266 1939 -7970-7811-8098-7999-8100-7900-7787-7909-7974-8161-7826-7986-7960 99999 1940 -278 -322 -222 -214 -237 -154 23 43 158 -98 129 -71 -103 7266 1941 -353 -289 -272 -372 -306 -128 -110 50 -161 -106 -294 4 -193 7266 1942 -404 -452 -389 -297 -196 -102 -24 -25 93 167 -9 39 -131 7266 1943 5 -138 128 -130 112 -57 -44 8 57 74 109 14 -73 2 7266 1944 1 31XX 112 -193 -175 -168 -191 -17 -24 10 59 -4 -5299999 -58 7266 1945 31 4 XX 99999 -40 -104 -84 -84 83 -2 -69 -39 1 -146 -56 -49 7266 1946 15 -73 -47 -245 -6 -179 106 4 102 136 -139 -22 -112 -47 7266 1947 6 3 3 3 3 6 -255 -430 -259 -67 -280 -113 -41 -188 35 -98 -57 -178 -154 7266 1948 4 1 -183 -267 -143 -117 -204 -17 17 71 153 120 29 63 -37 7266 1949 1 1 13 5 6 118 156 -176 71 -227 -227 -225 -93 -200 -31 -147 42 -77 7266 1950 6 -350 -151 -239 -196 -326 -90 -146 -126 69 -31 -223 -250 -169 7266 1951 713 2 -327 -366 -345 -216 -370 -214 -113 -80 -87 -115 -32 238 -156 7266 1952 5 -42 -133 -292 -163 -168 58 -28 20 19 -119 -147 -109 -92 7266 1953 1 1 -48 -276 -215 -135 -151 -168 52 74 31 -13 164 -4 -55 7266 1954 10 1 -243 -392 -251 -271 -347 -23 20 24 205 122 -28 107 -81 7266 1955 4 31 9 XX -106 -266 -337 -298 -89 -11999999 -154 5 6 -79 -3 -127 7266 1956 30 XX -133 -467 -335 -268 -111 -80 -110 499999 30 -117 -72 -149 7266 1957 3 -34 -108 -224 -334 -297 -153 -116 -39 47 93 -62 -15 -102 7266 1958 5 1510 6 12 XX -200 -234 -425 -320 -184 -192 -120 -57 -143 16 -76 -142 -180 7266 1959 7 4 -158 -242 -250 -176 -279 -136 -108 -156 -166 -111 -202 -219 -181 7266 1960 -319 -373 -494 -351 -357 -130 -154 -134 -185 -351 -163 -185 -266 7266 1961 -272 -161 -73 -278 -222 -81 -86 -51 -75 -20 -61 -99 -123 7266 1962 31 XX 99999 -206 -348 -327 -264 -131 -159 31 -73 -17 -233 -183 -173 7266 1963 -444 -431 -406 -362 -230 -213 -88 -124 -24 -5 -49 -160 -210 7266 1964 2 2 -194 -274 -444 -308 -195 -147 -61 -131 -79 -163 -45 -77 -176 7266 1965 2831 8 - -1669999999999 -261 -285 -147 -112 -83 -47 -66 -186 -22599999 7266 1966 11 6 71530 9XX -365 -318 -179 -386 -206 -146 -35 -89 -38 -15599999 -56 -181 7266 1967 4 2 -322 -165 63 -273 -210 -91 -71 -35 -62 244 7 -57 -77 7266 1968 -206 -294 -112 -226 -236 -121 -246 -215 -199 -35 -307 -259 -204 7266 1969 1 1 -312 -439 -470 -314 -346 -229 -88 -197 -96 -6 47 -339 -232 7266 1970 5 2 -367 -299 -315 -263 -308 -249 -30 -185 -85 -60 -123 -196 -204 7266 1971 3114 9 3XX -150 -221 -409 -324 -284 -205 -21899999 -182 55 -83 -63 -198 7266 1972 729 2 31313031 - -51299999 -399 -188 -280 -17999999999999999999999 -12 -6199999 7266 1973 9 4 -207 -132 -249 -288 -222 -209 -168 -160 -231 -228 -11 -128 -185 7266 1974 10313130 - -117 -191 -491 -510 -419 -188999999999999999 -337 -207 9599999 7266 1975 7 96 -279 -323 -388 -305 -228 -127 -158 24 -170 -147 14 -163 7266 1976 2 -105 -298 -334 -271 -221 -235 -127 -103 -199 -271 -83 -124 -198 7266 1977 1 1 2 -166 -374 -325 -294 -368 -266 -232 -287 -172 -47 100 -219 -222 7266 1978 9 6 -232 -570 -316 -490 -494 -229 -221 -237 -157 -163 26 -444 -301 7266 1979 2 1 -461 -446 -250 -377 -218 -162 -106 -118 11 -302 -53 -130 -217 7266 1980 -390 -415 -439 -346 -392 -235 -206 -135 -112 -100 -219 -67 -254 7266 1981 6 531 8 XX -188 -296 -192 -41399999 -131 -160 -199 -155 -32 25 -271 -180 7266 1982 5 -350 -264 -222 -304 -238 -283 -266 -85 -32 -247 64 -2 -183 7266 1983 4 8 178 -454 -209 -291 -236 -198 -210 -207 -47 103 -90 -140 -151 7266 1984 31 5 XX -186 -414 -527 -388 -390 -345 -264 -304 -26599999 -223 -169 -317 7266 1985 14 4 -437 -432 -432 -388 -429 -235 -167 42 -141 -128 -254 -201 -279 7266 1986 5 -346 -670 -330 -559 -219 -304 -202 -234 -160 -39 -25 -112 -262 7266 1987 5 31 5 13 9 XX -520 -394 -451 -466 -449 -29399999 -246 -107 -92 -163 -222 -322 7266 1988 -140 -218 -372 -430 -405 -284 -139 -75 -85 -209 -208 -170 -228 7266 1989 9 -27 17 -180 -408 -279 -206 -225 -74 -170 -130 -173 -146 -170 7266 1990 14 176 -19 -277 -381 -284 -240 -198 -219 -200 -274 -207 -178 7266 1991 312831303130313130 1 - 999999999999999999999999999999999999999999999 -274 -82 -13699999 7266 1992 -210 -229 -274 -368 -296 -353 -222 -103 -204 -391 -104 -123 -240 7266 1993 117 -319 -357 -440 -412 -288 -181 -194 -426 -387 -425 -154 -287 7266 1994 -194 -601 -176 -356 -375 -171 -290 -293 -277 -254 -186 -36 -265 7266 1995 2 -194 -29 -218 -405 -379 -289 -245 -313 -347 -72 -325 -453 -274 7266 1996 1 6 12 -532 -522 -664 -499 -459 -296 -227 -328 -435 -183 -176 -362 -387 7266 1997 -352 -73 -256 -387 -378 -362 -380 -285 -110 -195 -374 -342 -293 7266 1998 -233 -112 -362 -447 -401 -257 -136 -155 -299 -112 -284 -191 -249 7266 1999 -170 -195 -377 -345 -349 -238 -194 -277 -194 -204 -150 -108 -234 7266 2000 -176 -110 -335 -454 -292 -219 -278 -229 -308 -128 -117 -84 -228 7266 2001 -280 -439 -411 -422 -422 -272 -225 -195 -324 -49 -144 -359 -294 7266 2002 -145 -20 -255 -370 -327 -217 -214 -313 -289 -381 -434 -570 -296 7266 2003 -183 -414 -378 -475 -268 -211 -267 -233 -226 -268 -295 -217 -285 7266 2004 -289 -308 -404 -414 -350 -237 -241 -243 -65 -240 -210 -88 -257 7266 2005 -62 -528 -511 -392 -315 -318 -256 -164 -147 -219 -53 -347 -274 7266 2006 3 -428 -473 -556 -317 -365 -312 -292 -305 -205 -154 25 37 -279 7266 2007 28 -397 -285 -404 -237 -319 -124 -200 -178 -245 -241 -175 -229 7266 2008 -112 -114 -229 -388 -455 -226 -235 -195 -335 14 -186 -357 -235 7266 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Oslo 040/321 RLR(1964) is 15.0m below BM G35N38 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Oslo 040/321 RLR(1964) is 15.0m below BM G35N38 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1991 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. OSCARSBORG 040331 59 40 N 10 37 E04241964 66 14 0 0 1872 31 30 - 99999 704 704 666 861 826 952 932 1115 105299999 76899999 6347 1873 1118 703 530 557 373 519 704 876 1096 1159 967 1065 806 6347 1874 313130313031 - 666 197 175 801 821 87799999999999999999999999999999999999 6347 1875 31283130 - 99999999999999999999 839 980 888 983 1021 770 719 92399999 6347 1876 798 648 830 715 615 840 1007 980 959 860 582 527 780 6347 1877 3130 - 730 7469999999999 757 978 1062 946 924 1069 1209 91899999 6347 1878 761 847 797 639 947 929 894 918 1097 1004 790 763 866 6347 1879 628 688 695 672 735 1062 960 987 1087 965 725 905 842 6347 1880 725 795 789 769 709 824 1038 943 957 777 1085 1067 873 6347 1881 629 505 815 627 670 778 929 1074 680 674 1052 984 785 6347 1882 965 864 730 657 757 812 934 1031 904 826 840 580 825 6347 1953 312831303130 831 1 - 999999999999999999999999999999 221799999 2066 2090 2312 214399999 5012 1954 1948 1788 1891 1871 1779 2051 2101 2120 2280 2231 2117 2223 2035 5012 1955 31 1 1 1 XX 99999 1852 1807 1793 2038 1991 2030 1974 2104 2136 2068 2136 1995 5012 1956 1 1 1 6 31XX 2032 1699 1829 1866 2014 2033 2019 2123 2004 2115 200699999 1976 5012 1957 312831303130 3130313031 - 999999999999999999999999999999 1991999999999999999999999999999999 5012 1958 3128 6 313031 - 9999999999 1684 1814 1957 1927 2047 2076 196399999999999999999999 5012 1959 31283130 5 4 - 99999999999999999999 1845 1981 2004 1994 1966 2021 1923 193199999 5012 1960 31 31 - 99999 179299999 1801 1810 2011 1989 1989 1959 1743 1958 189999999 5012 1961 3128313031303131 1 2 6 - 9999999999999999999999999999999999999999 2106 2153 2118 210899999 5012 1962 3 2126 1894 1768 1852 1909 2040 2011 2206 2100 2158 1936 1985 1998 5012 1963 31 3 4 1 13 3XX 1694 170999999 1807 1949 1998 2073 2039 2118 2141 2150 2038 1969 5012 1964 1130313031 3 2 1 9 - 1978 1946 173299999999999999999999 1990 2088 1991 2069 202899999 5012 1965 111410 1214 2 1 9XX 1956 1741 1675 1848 1876 2173 2038 2041 2080 2070 1954 1906 1959 5012 1966 228 110 6 2 3 2 2XX 171599999 1946 1744 1846 1961 2067 2017 2151 1986 1964 2072 1959 5012 1967 3128 73031 9 23130313031 - 9999999999 21899999999999 2047 2114999999999999999999999999999999 5012 1968 31 130 313130313012 - 99999 1862 202799999 1913 20319999999999999999999999999 189199999 5012 1969 10 6 6 2 10 615 7 2 3 XX 1846 1745 1777 1820 1778 1849 2004 1973 2053 2110 2182 1823 1913 5012 1971 11 15 1992 1914 1746 1832 1852 1929 1874 2002 1942 2103 2038 2054 1946 5012 1972 1 215 1682 1683 1736 1860 1823 2041 1935 1935 1894 1908 2079 1880 1870 5012 1973 1880 1932 1865 1850 1875 1946 1978 1971 1909 1871 2094 1994 1930 5012 1974 2027 1938 1644 1621 1727 1913 2047 1956 2131 1792 1919 2219 1911 5012 1975 3 2208 1845 1786 1712 1790 1888 1985 1946 2124 1931 1938 2093 1939 5012 1976 3130313031 - 1977 1781 1744 1783 1779 1871 1859999999999999999999999999999999 5012 1977 3128313031 1 3 1 - 9999999999999999999999999 1871 1902 1805 1918 1997 2132 185399999 5012 1978 4 1880 1575 1817 1620 1682 1894 1930 1912 1962 1959 2087 1683 1837 5012 1979 5 1231XX 1669 1640 1775 1612 1843 1887 1940 1973 2076 1790 200799999 1835 5012 1980 1710 1663 1632 1740 1730 1899 1891 1948 2000 2049 1922 2053 1854 5012 1981 1924 1817 1853 1687 1762 1948 1968 1942 1999 2185 2184 1905 1932 5012 1982 1848 1966 1984 1859 1902 1871 1918 2067 2107 1893 2178 2083 1973 5012 1983 6 2219 1623 1859 1763 1836 1955 1956 1918 2083 2269 2040 1992 1957 5012 1984 1933 1706 1599 1697 1689 1806 1860 1848 1890 2112 1929 1918 1833 5012 1985 1667 1668 1640 1779 1739 1904 1996 2108 1993 1984 1874 1936 1859 5012 1986 5 411 4 1816 1442 1841 1597 1906 1831 1929 1837 1917 2059 2131 2049 1870 5012 1987 1611 1761 1666 1688 1719 1837 1841 1943 2075 2009 1973 1980 1842 5012 1988 4 4 2045 1969 1771 1725 1757 1907 2081 2126 2141 1995 2034 2044 1971 5012 1989 2165 2188 2050 1753 1870 1917 1884 2038 1960 2005 2030 2047 1991 5012 1990 131303131 1 2 1 - 2197 2346 2136 191999999999999999999999 1912 1955 1868 192399999 5012 1991 3 7 1952 1607 1679 1759 1687 1893 1866 1924 1976 1818 2035 1986 1850 5012 1992 1914 1901 1854 1766 1829 1777 1894 2013 1917 1743 2028 1991 1886 5012 1993 2228 1804 1767 1694 1718 1842 1933 1935 1709 1752 1709 1976 1840 5012 1994 1 1 2 9 1934 1544 1956 1769 1756 1951 1832 1840 1861 1878 1940 2085 1863 5012 1995 2 1 1925 2090 1912 1723 1756 1845 1878 1817 1794 2053 1826 1684 1858 5012 1996 13 1 10 211 XX 1608 1597 1511 1630 1680 1835 1878 1771 1698 1947 1959 1769 1744 5012 1997 1783 2054 1866 1743 1756 1777 1754 1844 2012 1933 1762 1800 1839 5012 1998 1313 1905 2010 1764 1697 1728 1873 1988 1972 1892 2225 1845 1941 1891 5012 1999 1959 1936 1762 1787 1783 1892 1930 1854 1935 1925 1971 2019 1896 5012 2000 2 1 1 2 1 1953 2021 1801 1686 1848 1897 1853 1903 1820 1983 2016 2048 1902 5012 2001 2 1843 1687 1719 1717 1712 1861 1904 1937 1816 2087 1984 1774 1838 5012 2002 1995 2111 1874 1771 1809 1916 1913 1824 1844 1755 1704 1575 1839 5012 2003 1912 1715 1753 1657 1866 1918 1854 1891 1893 1868 1846 1917 1842 5012 2004 1849 1828 1733 1718 1784 1885 1884 1891 2066 1893 1922 2040 1875 5012 2005 2067 1608 1631 1743 1815 1811 1873 1958 1975 1908 2070 1787 1855 5012 2006 3 1702 1661 1578 1815 1768 1797 1828 1829 1924 1976 2156 2162 1851 5012 2007 2151 1736 1847 1719 1887 1809 2004 1917 1936 1870 1879 1946 1894 5012 2008 2013 2005 1898 1745 1684 1909 1895 1940 1798 2134 1941 1775 1895 5012 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Oskarsborg 040/331 RLR(1964) is 9.5m below BMG35N 138 =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Oskarsborg 040/331 RLR(1964) is 9.5m below BMG35N 138 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-OCT-93 : DATA UP TO 1986 FROM AUTHORITY CODE 03 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1990 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 28-Jan-2009 : Following the input of revised data values station made Metric awaiting datum information. =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 06-Apr-2009 : 2007/8 mean sea level values entered as METRIC only awaiting confirmation of a datum query. VIKER 040341 59 02 N 10 57 E04241992 19 4 0 0 1990 31283130313031313031 6 7 - 99999999999999999999999999999999999999999999999999 596 59199999 6505 1991 6 1 1 603 289 364 405 358 559 524 587 630 532 690 641 514 6505 1992 570 566 507 440 483 438 551 659 568 423 695 623 544 6505 1993 5 851 460 435 385 402 507 588 577 402 437 393 636 506 6505 1994 410 2 3 1 1 618 237 626 426 432 608 479 517 513 529 618 727 530 6505 1995 14 2 2 574 744 578 405 444 502 543 492 575 696 465 361 529 6505 1996 31 1 11 XX 99999 307 210 305 374 497 553 453 440 616 625 446 439 6505 1997 10 1 310 3 2 2 3XX 513 716 527 412 449 473 398 495 631 583 444 533 515 6505 1998 4 3 2 559 669 440 399 402 527 634 625 528 693 514 599 551 6505 1999 622 601 446 460 462 543 572 530 600 581 624 679 560 6505 2000 6 621 684 475 387 514 525 534 575 493 668 646 681 568 6505 2001 536 377 414 394 391 516 560 587 498 755 636 456 511 6505 2002 3 672 767 548 467 478 556 555 509 502 438 397 292 513 6505 2003 625 380 421 340 528 579 532 563 572 542 540 579 518 6505 2004 532 504 422 396 461 551 551 580 711 559 592 701 547 6505 2005 713 282 335 416 486 485 553 631 643 582 711 468 527 6505 2006 1 390 359 287 491 452 463 495 519 594 657 810 805 527 6505 2007 808 456 528 410 555 516 667 585 616 563 574 644 578 6505 2008 685 671 572 445 375 572 554 611 477 778 609 473 568 6505 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 30-MAR-95 : tide gauge network modernised, new equipment installed in 1990 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 2000Apr25 : Viker 040/341 RLR(1992) is 10.3m below TGBM (G37 N111) STROMSTAD 050001 58 57 N 11 11 E05011964 62 4 0 0 1900 3000 2880 2850 2920 3060 3107 3090 3119 3099 3173 2951 3247 3041 4123 1901 3070 2952 2810 3008 2888 3135 3015 3067 2975 3113 3056 3006 3008 4123 1902 3243 2922 3041 2846 2918 2927 3072 3112 3030 3073 3097 3074 3030 4123 1903 3143 3313 3139 3003 3014 2974 3125 3267 3084 3117 3217 2992 3116 4123 1904 3100 2903 2779 3024 2957 3026 3077 3096 2997 3131 3149 3181 3035 4123 1905 3023 3003 2971 2869 2915 2966 3079 3104 3107 2980 2987 3206 3018 4123 1906 3144 3030 3045 2906 2920 2978 3081 3088 2970 3043 3066 3069 3028 4123 1907 2972 3026 2928 2893 2917 3079 3035 3201 3097 3080 3049 2968 3020 4123 1908 3061 3006 2717 2768 2922 2988 2985 3061 3029 2931 3093 3025 2966 4123 1909 3073 2914 2767 2868 2903 2963 3140 3125 2992 3262 3093 3140 3020 4123 1910 3163 3079 2947 2949 2938 2928 3027 3003 2973 2928 2886 3049 2989 4123 1911 2993 3121 2862 2893 2984 2981 3015 3015 3126 2961 3124 3059 3011 4123 1912 2910 2984 2995 2837 3026 3051 3011 3125 3026 3005 3117 3333 3035 4123 1913 2928 3073 3124 2884 2949 3079 3004 2987 2937 3046 3321 3169 3042 4123 1914 3068 3161 2985 3011 2967 2964 3027 3036 3095 2889 3074 3157 3036 4123 1915 2941 2874 2885 2934 2871 2917 3099 3086 2931 2794 2959 2894 2932 4123 1916 3253 2968 2781 2906 2918 3008 3040 2965 3005 3070 3124 3055 3008 4123 1917 2781 2914 2782 2859 2812 2956 2929 3017 3151 3149 3187 2983 2960 4123 1918 2985 3004 2766 2716 2797 2969 2987 3046 3157 3071 3040 3056 2966 4123 1919 2860 2786 2846 2892 2780 2947 2967 3117 3155 2915 2892 2971 2927 4123 1920 3091 3075 2985 2950 2976 2961 3083 3034 2961 2823 3055 2903 2992 4123 1921 3211 2826 3053 2839 2970 2938 3008 3048 3013 3053 2873 3204 3003 4123 1922 2805 2900 2910 2837 3004 3007 3053 3063 2948 2913 3045 3081 2964 4123 1923 3090 2764 2792 2778 3038 3052 3045 3088 3137 3290 3027 3006 3009 4123 1925 3154 3061 2812 2969 2935 3003 2956 3085 3083 3055 2978 3078 3014 4123 1926 2887 2860 2970 2862 2943 3045 2985 3099 3073 2991 3071 2980 2981 4123 1927 3050 2910 2910 2990 2870 3000 3010 3153 3101 3135 2997 2711 2986 4123 1928 3036 3005 2735 2798 2788 3025 3135 3079 3039 3093 3059 3018 2984 4123 1929 2692 2614 2868 2857 2853 3012 3030 3119 3082 3214 3164 3233 2980 4123 1930 3179 2795 2969 2786 2927 2962 3028 3049 2920 3094 3179 2976 2990 4123 1931 2967 2921 2774 2798 2876 3042 3097 3011 2901 3141 3033 3152 2977 4123 1932 3237 2842 2851 2956 2868 2941 3056 3031 3193 3102 3100 3100 3024 4123 1933 3020 2914 2879 2871 2870 2912 3041 3075 2907 2959 2815 2831 2925 4123 1934 3059 2990 2849 2770 2974 2929 2949 3047 3064 3191 2983 2945 2979 4123 1935 2917 3114 2771 2868 2767 3005 3066 2979 3140 3247 3038 3032 2994 4123 1936 3060 2826 2733 2856 2733 2942 3097 3045 2832 3040 3059 3264 2958 4123 1937 1880 2040 1790 1880 1960 2060 2010 1960 2130 1990 2040 1830 1964 5073 1938 2070 1786 2133 1937 1945 2080 2058 2066 2005 2270 2296 1973 2054 5073 1939 1936 2108 1822 1924 1815 1996 2100 2018 1842 1777 2093 1884 1941 5073 1940 1861 1810 1884 1861 1859 1830 2080 2076 2130 1988 2108 1937 1952 5073 1946 312831 - 999999999999999 2024 1888 2158 2061 2090 2170 1943 2041 197099999 5073 1947 1841 1571 1804 1997 1787 1943 2019 1881 2071 1942 2137 1928 1911 5073 1948 1960 1883 1980 1935 1908 2050 2045 2106 2161 2125 2045 2110 2026 5073 1949 2188 2061 1783 2025 1945 1996 1977 2095 1999 2153 2019 2213 2038 5073 1950 1927 2056 1929 2021 1885 2062 1995 2021 2230 2086 2011 1956 2017 5073 1951 1935 1836 1796 1928 1780 1855 2017 2070 1798 1919 2068 2339 1946 5073 1952 2045 1969 1829 1913 1895 2073 2019 2057 2047 1959 1917 1962 1974 5073 1953 1989 1828 1887 1950 1930 1954 2109 2138 2086 2053 2196 2067 2017 5073 1954 1840 1756 1861 1806 1766 2033 2064 2059 2214 2164 2013 2138 1978 5073 1955 1991 1837 1801 1798 2008 1972 1958 1944 2067 2073 2040 2109 1968 5073 1956 1972 1659 1838 1841 1968 1992 1995 2095 2007 2049 2023 2029 1957 5073 1957 2061 1988 1894 1773 1828 1961 2000 2027 2100 2217 2024 2084 1997 5073 1958 1927 1905 1730 1813 1926 1940 2030 2028 1995 2055 1972 1985 1942 5073 1959 2003 1864 1888 1930 1853 1964 2002 1965 1920 2013 1936 1945 1941 5073 1960 1835 1790 1703 1807 1824 1972 1984 2006 1954 1797 2021 1989 1890 5073 1961 1937 2027 2119 1918 1958 2091 2101 2123 2069 2137 2089 2060 2052 5073 1962 2 1 3130 5 - 2133 1954 1834 1834 1870 1995 19969999999999 2054 1889 194199999 5073 1963 1 1 2 1 1 1 1 1 7 1698 1696 1767 1773 1865 1910 1961 1939 2082 2107 2106 1987 1908 5073 1964 5 2 5 4 6 3 4 5 2 5 5 5 1941 1863 1695 1838 1957 2003 2026 1979 2035 1958 2134 2060 1957 5073 1965 XXXXXXXXXXXXXXXXXXXXXXXX 1993 1795 1794 1817 1844 2089 1997 2004 2017 2025 1916 1973 1939 5073 1966 1729 1916 1935 1729 1875 1939 2026 2024 2124 2000 1936 2029 1939 5073 1967 1821 1984 2227 1905 1982 2058 2032 2028 2025 2262 2103 2019 2037 5073 =========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-JUN-91 : Stromstad 050/001 RLR(1964) is 9.5m below BM No1173Z =========================== BENCHMARK INFORMATION UPDATE ADDED 12-JUL-93 : Stromstad 050/001 RLR(1964) is 9.5m below BM No1173Z SMOGEN 050011 58 22 N 11 13 E05241964 98 6 0 0 1911 -3609-3461-3701-3644-3646-3625-3588-3557-3464-3593-3425-3512-3569 10753 1912 -3636-3574-3556-3686-3574-3519-3564-3464-3547-3533-3473-3293-3535 10753 1913 -3628-3519-3445-3652-3630-3530-3564-3558-3603-3518-3246-3390-3524 10753 1914 -3526-3443-3571-3589-3610-3625-3568-3550-3481-3648-3503-3399-3543 10753 1915 -3615-3669-3679-3655-3700-3663-3514-3506-3607-3748-3592-3646-3633 10753 1916 -3333-3599-3739-3679-3666-3601-3561-3548-3567-3486-3455-3537-3564 10753 1917 -3790-3679-3779-3712-3770-3650-3628-3537-3421-3419-3414-3577-3615 10753 1918 -3551-3565-3779-3813-3775-3613-3578-3541-3411-3523-3558-3531-3603 10753 1919 -3715-3716-3699-3692-3773-3610-3568-3455-3439-3615-3637-3609-3627 10753 1920 -3487-3526-3598-3621-3601-3613-3515-3554-3567-3701-3544-3657-3582 10753 1921 -3391-3717-3538-3726-3641-3629-3567-3522-3547-3515-3660-3371-3569 10753 1922 -3714-3645-3648-3737-3620-3585-3532-3516-3596-3665-3501-3491-3604 10753 1923 -3502-3737-3809-3778-3617-3561-3534-3484-3463-3332-3470-3587-3573 10753 1924 -3667-3671-3725-3729-3664-3597-3517-3517-3418-3524-3573-3456-3588 10753 1925 -3425-3540-3744-3696-3682-3616-3617-3532-3487-3518-3598-3475-3578 10753 1926 -3629-3685-3593-3695-3662-3592-3585-3495-3506-3522-3473-3567-3584 10753 1927 -3520-3665-3660-3580-3701-3533-3564-3490-3473-3449-3570-3786-3583 10753 1928 -3529-3585-3791-3754-3784-3575-3469-3509-3554-3507-3491-3608-3596 10753 1929 -3841-3916-3723-3719-3721-3585-3555-3523-3531-3415-3452-3429-3618 10753 1930 -3453-3818-3672-3832-3713-3685-3595-3564-3674-3503-3421-3620-3629 10753 1931 -3616-3710-3828-3766-3716-3590-3506-3575-3647-3457-3563-3470-3620 10753 1932 -3440-3756-3739-3642-3726-3656-3562-3571-3443-3491-3514-3525-3589 10753 1933 -3649-3680-3729-3713-3734-3682-3587-3537-3667-3612-3759-3743-3674 10753 1934 -3546-3608-3719-3780-3662-3662-3634-3545-3551-3430-3589-3617-3612 10753 1935 -3665-3509-3777-3714-3797-3636-3549-3606-3465-3390-3559-3567-3603 10753 1936 -3540-3740-3830-3740-3830-3670-3550-3570-3700-3540-3570-3400-3640 10753 1937 1940 2100 1870 1910 1950 2060 2070 2040 2160 2050 2080 1890 2010 5070 1938 2181 1981 2198 2009 2006 2113 2078 2087 2068 2267 2306 1996 2107 5070 1939 2015 2124 1856 1993 1892 2018 2106 2028 1977 1835 2116 2008 1997 5070 1940 1860 1827 1940 1893 1890 1952 2064 2106 2210 2022 2240 2023 2002 5070 1941 1828 1827 1859 1797 1866 1998 2020 2165 1983 2033 1888 2151 1951 5070 1942 1807 1793 1823 1833 1944 1991 2065 2043 2139 2227 2113 2171 1996 5070 1943 2015 2199 1999 2145 1997 2042 2101 2164 2139 2167 2116 2042 2094 5070 1944 2208 1952 1969 1975 1955 2085 2075 2094 2147 2065 2089 2091 2059 5070 1945 1964 2055 2038 2039 2048 2144 2093 2088 2083 2127 2033 2087 2067 5070 1946 2072 2099 1926 2053 1957 2138 2092 2135 2219 1989 2097 1994 2064 5070 1947 1841 1693 1869 2014 1816 1970 2022 1944 2096 1959 2092 1981 1941 5070 1948 2013 1908 1965 1960 1901 2026 2035 2099 2162 2138 2076 2090 2031 5070 1949 2136 2060 1805 2124 1925 2007 2021 2129 2060 2180 2090 2248 2065 5070 1950 1959 2113 1986 2068 1942 2068 2065 2074 2225 2134 2081 2026 2062 5070 1951 1989 1917 1871 1953 1855 1969 2044 2070 2064 1970 2108 2307 2010 5070 1952 2093 2021 1864 1923 1927 2083 2034 2101 2109 2031 2006 2024 2018 5070 1953 2015 1897 1929 1952 1955 1977 2100 2158 2119 2083 2191 2068 2037 5070 1954 1905 1810 1871 1832 1819 2002 2075 2084 2186 2166 2056 2172 1998 5070 1955 2036 1946 1871 1861 2028 2006 1998 1997 2107 2128 2072 2168 2018 5070 1956 2017 1714 1855 1878 1977 1999 2040 2115 2037 2107 2050 2053 1987 5070 1957 2075 2034 1903 1804 1849 1974 2012 2073 2151 2197 2061 2098 2019 5070 1958 1976 1966 1821 1854 1942 1971 2058 2059 2008 2125 1994 2071 1987 5070 1959 2034 1930 1912 1965 1872 1980 2026 2004 1974 2064 1954 1933 1971 5070 1960 1833 1806 1690 1786 1877 1991 2022 2052 2023 1905 2092 2044 1927 5070 1961 1973 2048 2119 1983 2006 2106 2128 2166 2138 2146 2116 2085 2084 5070 1962 2152 1977 1903 1873 1921 1996 2051 2183 2113 2130 1979 2029 2026 5070 1963 1 1781 1828 1825 1806 1868 1916 1969 1999 2053 2114 2141 2034 1944 5070 1964 1972 1915 1743 1839 1917 1986 2034 2023 2072 2012 2136 2087 1978 5070 1965 2015 1827 1878 1878 1870 1988 2040 2035 2062 2071 2018 2040 1977 5070 1966 XX XXXX 1812 1950 1989 1829 1924 1976 2072 2045 2161 2066 2001 2084 1992 5070 1967 1895 2027 2182 1947 1971 2029 2029 2066 2073 2314 2122 2116 2064 5070 1968 XX 1986 1925 2031 1921 1898 1978 1899 1939 1983 2095 1912 1937 1959 5070 1969 XX XX XX 1880 1738 1789 1848 1868 1932 2001 1975 2043 2110 2214 1867 1939 5070 1970 XXXX XX 1863 1906 1878 1892 1880 1915 2086 1994 2061 2110 2077 1986 1971 5070 1971 XX 2007 1927 1785 1840 1855 1925 1963 2031 1968 2105 2111 2074 1966 5070 1972 XX 1790 1795 1826 1910 1888 2001 1940 1943 1946 1963 2171 2129 1942 5070 1973 XX 1956 2062 1938 1918 1929 1959 2006 1983 1984 1965 2163 2061 1994 5070 1974 2052 1954 1730 1670 1797 1971 2092 2021 2177 1917 2029 2244 1971 5070 1975 2257 1931 1888 1805 1837 1897 1964 1975 2121 1993 2002 2148 1985 5070 1976 2060 1894 1837 1831 1845 1919 1931 1870 1884 1943 2025 1919 1913 5070 1977 XX 1894 1865 1891 1930 1821 1938 1963 1907 2027 2072 2214 1983 1959 5070 1978 1989 1758 1941 1754 1753 1939 1950 1968 2063 2051 2146 1852 1930 5070 1979 1832 1826 1919 1815 1853 1890 1965 1968 2057 1844 2045 1983 1916 5070 1980 1874 1809 1731 1808 1831 1949 1938 1996 2064 2095 2016 2136 1937 5070 1981 2019 1933 1960 1763 1860 1970 2021 1982 2041 2164 2179 1997 1991 5070 1982 1938 1924 1948 1873 1925 1923 1942 2069 2119 1968 2212 2163 2000 5070 1983 2280 1796 1963 1880 1902 1890 1918 1895 2064 2202 2019 2004 1984 5070 1984