Huybrechts, Philippe; Rybak, Oleg; Pattyn, Frank; Ruth, Urs; Steinhage, Daniel (2007): Lagrangian back-tracing results for Kohnen station given every 1 m of the depth [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.693812, In supplement to: Huybrechts, P et al. (2007): Ice thinning, upstream advection, and non-climatic biases for the upper 89% of the EDML ice core from a nested model of the Antarctic ice sheet. Climate of the Past, 3(4), 577-589, https://doi.org/10.5194/cp-3-577-2007
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Project(s):
Glaciology @ AWI (AWI_Glac)
Coverage:
Median Latitude: -75.111052 * Median Longitude: 1.558023 * South-bound Latitude: -75.282028 * West-bound Longitude: 0.070445 * North-bound Latitude: -75.002892 * East-bound Longitude: 6.431340
Minimum DEPTH, ice/snow: 10 m * Maximum DEPTH, ice/snow: 2477 m
Event(s):
Kohnen * Latitude: -75.001660 * Longitude: 0.067830 * Elevation: 2892.0 m * Location: Dronning Maud Land, Antarctica * Campaign: Kohnen_based * Basis: Kohnen Station * Method/Device: Research station (RS)
Comment:
DEPTH in ice is modeled real depth; modeled ice equivalent depth at Kohnen: 2753.22 m; Modeled real depth at Kohnen including firn compaction: 2781.846 m; geographical latitude/longitude indicate the place where Kohnen ice was deposited.
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 | LATITUDE | Latitude | Geocode | |||
4 | LONGITUDE | Longitude | Geocode | |||
5 | Depth, relative | Depth rel | % | Huybrechts, Philippe | modelled | |
6 | Depth ice equivalent | Depth i.e. | m | Huybrechts, Philippe | modelled | |
7 | Distance, relative | Dist rel | m | Huybrechts, Philippe | Horizontal distance (m) traveled by particle | |
8 | Surface elevation | Surf elev | m | Huybrechts, Philippe | Surface elevation (m) of the place where ice was deposited at the time of deposition | |
9 | Bias | Bias | Huybrechts, Philippe | Difference in surface elevation (m) at the place of particle origin between today and time of deposition | ||
10 | Bias | Bias | Huybrechts, Philippe | Difference in surface elevation (m) between Kohnen and the place of origin for present-day topography | ||
11 | Bias | Bias | Huybrechts, Philippe | Total elevation change between Kohnen today and place of particle deposition at time of deposition (m), sum of columns 9 and 10 | ||
12 | Bias | Bias | Huybrechts, Philippe | Total non-climatic biases for surface temperature (ºC) calculated using present-day spatial gradient of -0.01171 ºC/m | ||
13 | Bias | Bias | Huybrechts, Philippe | Total non-climatic biases for d18O (per mil ) calculated using present-day spatial gradient of -0.00957 ?/m | ||
14 | Function | Function | Huybrechts, Philippe | Thinning function taking into account firn compaction | ||
15 | Function | Function | Huybrechts, Philippe | Thinning function without firn compaction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
27148 data points
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