Bohleber, Pascal; Wagenbach, Dietmar; Schöner, Wolfgang; Böhm, Reinhard (2013): Annual means of delta 18O time series Colle Gnifetti ice core KCH [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874161, 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: 45.928190 * Longitude: 7.875920
Minimum Elevation: 4450.0 m * Maximum Elevation: 4450.0 m
Event(s):
Colle_Gnifetti_KCH * Latitude: 45.928190 * Longitude: 7.875920 * 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 | -11.29 |
| 1992 | -0.042 | -13.48 |
| 1991 | -0.041 | -12.77 |
| 1990 | -0.040 | -14.21 |
| 1989 | -0.039 | -14.11 |
| 1988 | -0.038 | -12.02 |
| 1987 | -0.037 | -18.02 |
| 1986 | -0.036 | -12.67 |
| 1985 | -0.035 | -13.97 |
| 1984 | -0.034 | -14.86 |
| 1983 | -0.033 | -10.73 |
| 1982 | -0.032 | -9.80 |
| 1981 | -0.031 | -15.91 |
| 1980 | -0.030 | -14.92 |
| 1979 | -0.029 | -14.40 |
| 1978 | -0.028 | -14.28 |
| 1977 | -0.027 | -12.51 |
| 1976 | -0.026 | -13.37 |
| 1975 | -0.025 | -14.60 |
| 1974 | -0.024 | -13.92 |
| 1973 | -0.023 | -14.68 |
| 1972 | -0.022 | -11.83 |
| 1971 | -0.021 | -11.24 |
| 1970 | -0.020 | -11.02 |
| 1969 | -0.019 | -11.84 |
| 1968 | -0.018 | -13.56 |
| 1967 | -0.017 | -15.30 |
| 1966 | -0.016 | -13.01 |
| 1965 | -0.015 | -14.78 |
| 1964 | -0.014 | -15.11 |
| 1963 | -0.013 | -11.46 |
| 1962 | -0.012 | -12.27 |
| 1961 | -0.011 | -15.65 |
| 1960 | -0.010 | -14.03 |
| 1959 | -0.009 | -12.66 |
| 1958 | -0.008 | -13.60 |
| 1957 | -0.007 | -13.42 |
| 1956 | -0.006 | -12.35 |
| 1955 | -0.005 | -14.80 |
| 1954 | -0.004 | -14.80 |
| 1953 | -0.003 | -13.01 |
| 1952 | -0.002 | -13.14 |
| 1951 | -0.001 | -12.42 |
| 1950 | 0.000 | -10.30 |
| 1949 | 0.001 | -11.83 |
| 1948 | 0.002 | -12.76 |
| 1947 | 0.003 | -11.25 |
| 1946 | 0.004 | -13.04 |
| 1945 | 0.005 | -12.93 |
| 1944 | 0.006 | -14.71 |
| 1943 | 0.007 | -17.09 |
| 1942 | 0.008 | -16.37 |
| 1941 | 0.009 | -14.53 |
| 1940 | 0.010 | -14.44 |
| 1939 | 0.011 | -16.26 |
| 1938 | 0.012 | -13.22 |
| 1937 | 0.013 | -13.46 |
| 1936 | 0.014 | -10.82 |
| 1935 | 0.015 | -12.30 |
| 1934 | 0.016 | -17.02 |
| 1933 | 0.017 | -14.45 |
| 1932 | 0.018 | -12.73 |
| 1931 | 0.019 | -15.39 |
| 1930 | 0.020 | -15.89 |
| 1929 | 0.021 | -15.98 |
| 1928 | 0.022 | -15.74 |
| 1927 | 0.023 | -14.70 |
| 1926 | 0.024 | -14.21 |
| 1925 | 0.025 | -15.66 |
| 1924 | 0.026 | -13.55 |
| 1923 | 0.027 | -14.03 |
| 1922 | 0.028 | -14.18 |
| 1921 | 0.029 | -13.33 |
| 1920 | 0.030 | -13.77 |
| 1919 | 0.031 | -13.40 |
| 1918 | 0.032 | -14.30 |
| 1917 | 0.033 | -15.41 |
| 1916 | 0.034 | -16.32 |
| 1915 | 0.035 | -13.79 |
| 1914 | 0.036 | -13.82 |
| 1913 | 0.037 | -13.06 |
| 1912 | 0.038 | -10.93 |
| 1911 | 0.039 | -13.23 |
| 1910 | 0.040 | -14.15 |
| 1909 | 0.041 | -12.64 |
| 1908 | 0.042 | -15.01 |
| 1907 | 0.043 | -14.78 |
| 1906 | 0.044 | -12.82 |
| 1905 | 0.045 | -15.98 |
| 1904 | 0.046 | -17.37 |
| 1903 | 0.047 | -14.34 |
| 1902 | 0.048 | -14.75 |
| 1901 | 0.049 | -14.13 |
| 1900 | 0.050 | -11.88 |
| 1899 | 0.051 | -14.95 |
| 1898 | 0.052 | -16.29 |
| 1897 | 0.053 | -16.09 |
| 1896 | 0.054 | -17.83 |
| 1895 | 0.055 | -14.43 |
| 1894 | 0.056 | -15.61 |
| 1893 | 0.057 | -16.47 |
| 1892 | 0.058 | -13.05 |
| 1891 | 0.059 | -13.06 |
| 1890 | 0.060 | -12.68 |
| 1889 | 0.061 | -12.21 |
| 1888 | 0.062 | -12.51 |
| 1887 | 0.063 | -14.57 |
| 1886 | 0.064 | -12.36 |
| 1885 | 0.065 | -12.53 |
| 1884 | 0.066 | -14.12 |
| 1883 | 0.067 | -11.17 |
| 1882 | 0.068 | -13.06 |
| 1881 | 0.069 | -15.02 |
| 1880 | 0.070 | -14.47 |