Bohleber, Pascal; Wagenbach, Dietmar; Schöner, Wolfgang; Böhm, Reinhard (2013): Annual means of delta 18O time series Colle Gnifetti ice core KCS [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874163, In supplement to: Bohleber, P et al. (2013): To what extent do water isotope records from low accumulation Alpine ice cores reproduce instrumental temperature series? Tellus Series B-Chemical and Physical Meteorology, 65(1), 20148, https://doi.org/10.3402/tellusb.v65i0.20148
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Coverage:
Latitude: 45.929110 * Longitude: 7.873650
Minimum Elevation: 4450.0 m * Maximum Elevation: 4450.0 m
Event(s):
Colle_Gnifetti_KCS * Latitude: 45.929110 * Longitude: 7.873650 * Elevation: 4450.0 m * Location: Colle Gnifetti, Monte Rosa, Swiss Alps * Method/Device: Ice drill (ICEDRILL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Age | Age | a AD/CE | Bohleber, Pascal | typical dating uncertainty was estimated to be less than 2.5 yrs | |
2 | AGE | Age | ka BP | Bohleber, Pascal | Geocode – typical dating uncertainty was estimated to be less than 2.5 yrs | |
3 | δ18O, water | δ18O H2O | ‰ SMOW | Bohleber, Pascal | nominal annual resolution |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
228 data points
Data
1 Age [a AD/CE] | 2 Age [ka BP] | 3 δ18O H2O [‰ SMOW] |
---|---|---|
1993 | -0.043 | -10.01 |
1992 | -0.042 | -12.55 |
1991 | -0.041 | -11.14 |
1990 | -0.040 | -13.49 |
1989 | -0.039 | -15.44 |
1988 | -0.038 | -13.86 |
1987 | -0.037 | -11.52 |
1986 | -0.036 | -14.22 |
1985 | -0.035 | -15.08 |
1984 | -0.034 | -15.73 |
1983 | -0.033 | -9.98 |
1982 | -0.032 | -15.10 |
1981 | -0.031 | -13.96 |
1980 | -0.030 | -15.31 |
1979 | -0.029 | -10.07 |
1978 | -0.028 | -11.44 |
1977 | -0.027 | -12.29 |
1976 | -0.026 | -13.55 |
1975 | -0.025 | -17.72 |
1974 | -0.024 | -13.31 |
1973 | -0.023 | -11.30 |
1972 | -0.022 | -11.82 |
1971 | -0.021 | -14.62 |
1970 | -0.020 | -10.56 |
1969 | -0.019 | -15.41 |
1968 | -0.018 | -12.17 |
1967 | -0.017 | -13.09 |
1966 | -0.016 | -14.99 |
1965 | -0.015 | -16.28 |
1964 | -0.014 | -13.72 |
1963 | -0.013 | -14.58 |
1962 | -0.012 | -13.45 |
1961 | -0.011 | -17.35 |
1960 | -0.010 | -12.52 |
1959 | -0.009 | -11.05 |
1958 | -0.008 | -13.23 |
1957 | -0.007 | -17.68 |
1956 | -0.006 | -14.85 |
1955 | -0.005 | -14.69 |
1954 | -0.004 | -13.33 |
1953 | -0.003 | -16.02 |
1952 | -0.002 | -11.60 |
1951 | -0.001 | -14.48 |
1950 | 0.000 | -13.96 |
1949 | 0.001 | -10.72 |
1948 | 0.002 | -12.38 |
1947 | 0.003 | -10.40 |
1946 | 0.004 | -13.03 |
1945 | 0.005 | -11.28 |
1944 | 0.006 | -12.61 |
1943 | 0.007 | -16.35 |
1942 | 0.008 | -15.18 |
1941 | 0.009 | -13.02 |
1940 | 0.010 | -18.03 |
1939 | 0.011 | -14.07 |
1938 | 0.012 | -14.73 |
1937 | 0.013 | -10.42 |
1936 | 0.014 | -14.05 |
1935 | 0.015 | -17.01 |
1934 | 0.016 | -14.04 |
1933 | 0.017 | -12.77 |
1932 | 0.018 | -13.55 |
1931 | 0.019 | -12.01 |
1930 | 0.020 | -14.02 |
1929 | 0.021 | -14.24 |
1928 | 0.022 | -18.92 |
1927 | 0.023 | -17.05 |
1926 | 0.024 | -13.78 |
1925 | 0.025 | -10.03 |
1924 | 0.026 | -13.32 |
1923 | 0.027 | -14.99 |
1922 | 0.028 | -13.68 |
1921 | 0.029 | -12.03 |
1920 | 0.030 | -15.88 |
1919 | 0.031 | -14.36 |
1918 | 0.032 | -13.86 |
1917 | 0.033 | -15.20 |
1916 | 0.034 | -13.96 |
1915 | 0.035 | -16.02 |
1914 | 0.036 | -13.06 |
1913 | 0.037 | -11.19 |
1912 | 0.038 | -13.66 |
1911 | 0.039 | -12.98 |
1910 | 0.040 | -14.70 |
1909 | 0.041 | -15.20 |
1908 | 0.042 | -15.47 |
1907 | 0.043 | -14.64 |
1906 | 0.044 | -13.18 |
1905 | 0.045 | -15.67 |
1904 | 0.046 | -14.59 |
1903 | 0.047 | -13.67 |
1902 | 0.048 | -13.53 |
1901 | 0.049 | -15.91 |
1900 | 0.050 | -15.86 |
1899 | 0.051 | -15.22 |
1898 | 0.052 | -19.06 |
1897 | 0.053 | -14.87 |
1896 | 0.054 | -15.87 |
1895 | 0.055 | -18.10 |
1894 | 0.056 | -19.89 |
1893 | 0.057 | -19.94 |
1892 | 0.058 | -17.06 |
1891 | 0.059 | -13.28 |
1890 | 0.060 | -11.14 |
1889 | 0.061 | -15.13 |
1888 | 0.062 | -16.54 |
1887 | 0.063 | -14.96 |
1886 | 0.064 | -14.03 |
1885 | 0.065 | -14.02 |
1884 | 0.066 | -14.12 |
1883 | 0.067 | -14.17 |
1882 | 0.068 | -13.91 |
1881 | 0.069 | -12.77 |
1880 | 0.070 | -12.18 |