Fernandoy, Francisco; Meyer, Hanno; Oerter, Hans; Wilhelms, Frank; Graf, Wolfgang; Schwander, Jakob (2008): Annual means of δ¹⁸O and accumulation rates of firn core DML97C07_04 [dataset]. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA, https://doi.org/10.1594/PANGAEA.704483, In supplement to: Fernandoy, F et al. (2010): Temporal and Spatial variation of stable-isotope ratios and accumulation rates in the hinterland of Neumayer station, East Antarctica. Journal of Glaciology, 56(198), 673-687, https://doi.org/10.3189/002214310793146296
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Project(s):
Glaciology @ AWI (AWI_Glac)
Coverage:
Latitude: -72.064000 * Longitude: -9.558300
Date/Time Start: 2007-01-30T00:00:00 * Date/Time End: 2007-02-01T23:59:00
Minimum DEPTH, ice/snow: 0.5000 m * Maximum DEPTH, ice/snow: 35.5750 m
Event(s):
DML97C07_04 (FB0704) * Latitude: -72.064000 * Longitude: -9.558300 * Date/Time Start: 2007-01-30T00:00:00 * Date/Time End: 2007-02-01T23:59:00 * Elevation: 760.0 m * Recovery: 36 m * Location: Dronning Maud Land, Antarctica * Campaign: Pre-IPICS * Basis: Sampling/drilling ice * Method/Device: Ice drill (ICEDRILL) * Comment: Location: Søråsen South
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, ice/snow | Depth ice/snow | m | Geocode | ||
2 | AGE | Age | ka BP | Geocode | ||
3 | Age | Age | a AD/CE | Oerter, Hans | ||
4 | Depth, top/min | Depth top | m | Oerter, Hans | ||
5 | Depth, bottom/max | Depth bot | m | Oerter, Hans | ||
6 | Accumulation rate ice, water equivalent | Acc rate ice | kg/m2/a | Oerter, Hans | Calculated | |
7 | δ18O, water | δ18O H2O | ‰ SMOW | Oerter, Hans | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
225 data points
Data
1 Depth ice/snow [m] | 2 Age [ka BP] | 3 Age [a AD/CE] | 4 Depth top [m] | 5 Depth bot [m] | 6 Acc rate ice [kg/m2/a] | 7 δ18O H2O [‰ SMOW] |
---|---|---|---|---|---|---|
0.5000 | -0.056 | 2006 | 0.050 | 0.950 | 406 | -25.44 |
1.5750 | -0.055 | 2005 | 0.950 | 2.200 | 561 | -19.80 |
2.6000 | -0.054 | 2004 | 2.200 | 3.000 | 373 | -22.68 |
3.3500 | -0.053 | 2003 | 3.000 | 3.700 | 332 | -24.84 |
4.1500 | -0.052 | 2002 | 3.700 | 4.600 | 368 | -22.81 |
5.3250 | -0.051 | 2001 | 4.600 | 6.050 | 835 | -21.93 |
6.3750 | -0.050 | 2000 | 6.050 | 6.700 | 348 | -24.07 |
7.0500 | -0.049 | 1999 | 6.700 | 7.400 | 378 | -22.02 |
7.9250 | -0.048 | 1998 | 7.400 | 8.450 | 584 | -22.85 |
8.9000 | -0.047 | 1997 | 8.450 | 9.350 | 508 | -24.05 |
9.9000 | -0.046 | 1996 | 9.350 | 10.450 | 634 | -23.22 |
11.0000 | -0.045 | 1995 | 10.450 | 11.550 | 648 | -22.35 |
12.2000 | -0.044 | 1994 | 11.550 | 12.850 | 775 | -23.48 |
13.1500 | -0.043 | 1993 | 12.850 | 13.450 | 360 | -22.39 |
13.7750 | -0.042 | 1992 | 13.450 | 14.100 | 393 | -23.47 |
14.6000 | -0.041 | 1991 | 14.100 | 15.100 | 612 | -23.15 |
15.3750 | -0.040 | 1990 | 15.100 | 15.650 | 337 | -22.18 |
16.1000 | -0.039 | 1989 | 15.650 | 16.550 | 554 | -23.80 |
16.8500 | -0.038 | 1988 | 16.550 | 17.150 | 374 | -21.51 |
17.4750 | -0.037 | 1987 | 17.150 | 17.800 | 407 | -21.82 |
18.1500 | -0.036 | 1986 | 17.800 | 18.500 | 442 | -23.49 |
18.8250 | -0.035 | 1985 | 18.500 | 19.150 | 411 | -23.51 |
19.5000 | -0.034 | 1984 | 19.150 | 19.850 | 448 | -23.47 |
20.1500 | -0.033 | 1983 | 19.850 | 20.450 | 384 | -23.11 |
20.8500 | -0.032 | 1982 | 20.450 | 21.250 | 514 | -24.15 |
21.6750 | -0.031 | 1981 | 21.250 | 22.100 | 549 | -19.87 |
22.6250 | -0.030 | 1980 | 22.100 | 23.150 | 682 | -21.95 |
23.5250 | -0.029 | 1979 | 23.150 | 23.900 | 494 | -22.57 |
24.5000 | -0.028 | 1978 | 23.900 | 25.100 | 799 | -21.11 |
25.5500 | -0.027 | 1977 | 25.100 | 26.000 | 600 | -22.70 |
26.4000 | -0.026 | 1976 | 26.000 | 26.800 | 551 | -22.33 |
27.2250 | -0.025 | 1975 | 26.800 | 27.650 | 582 | -22.91 |
27.9500 | -0.024 | 1974 | 27.650 | 28.250 | 409 | -23.15 |
28.5250 | -0.023 | 1973 | 28.250 | 28.800 | 375 | -22.58 |
29.1750 | -0.022 | 1972 | 28.800 | 29.550 | 511 | -23.82 |
29.9750 | -0.021 | 1971 | 29.550 | 30.400 | 587 | -21.00 |
30.6750 | -0.020 | 1970 | 30.400 | 30.950 | 381 | -22.00 |
31.2000 | -0.019 | 1969 | 30.950 | 31.450 | 350 | -24.65 |
31.8250 | -0.018 | 1968 | 31.450 | 32.200 | 524 | -22.67 |
32.5500 | -0.017 | 1967 | 32.200 | 32.900 | 496 | -20.98 |
33.2500 | -0.016 | 1966 | 32.900 | 33.600 | 495 | -21.51 |
33.9000 | -0.015 | 1965 | 33.600 | 34.200 | 426 | -23.35 |
34.5250 | -0.014 | 1964 | 34.200 | 34.850 | 465 | -24.39 |
35.0750 | -0.013 | 1963 | 34.850 | 35.300 | 326 | -24.07 |
35.5750 | -0.012 | 1962 | 35.300 | 35.850 | 401 | -24.91 |