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Cuffey, Kurt M; Clow, Gary D (1999): GISP2 accumulation rate history [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.56075

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Related to:
Cuffey, Kurt M; Clow, Gary D (1997): Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. Journal of Geophysical Research: Oceans, 102(C12), 26383-26396, https://doi.org/10.1029/96JC03981
Cuffey, Kurt M; Clow, Gary D; Alley, Richard B; Stuiver, Minze; Waddington, Edwin D; Saltus, Richard W (1995): Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition. Science, 270(5235), 455-458, https://doi.org/10.1126/science.270.5235.455
GRIP/GISP (1997): The Greenland Summit Ice Cores CD-ROM GISP2/GRIP. National Snow and Ice Data Center, University of Colorado at Boulder, and World Data Center for Paleoclimatology, National Geophysical Data Center, Boulder Colorado, CD-ROM, grip-gisp.iso
Project(s):
Greenland Ice Core Projects (GRIP/GISP/NGRIP)
Coverage:
Latitude: 72.970000 * Longitude: -38.800000
Date/Time Start: 1990-01-01T00:39:00 * Date/Time End: 1990-01-01T00:39:00
Minimum Elevation: 3208.0 m * Maximum Elevation: 3208.0 m
Event(s):
GISP2 * Latitude: 72.970000 * Longitude: -38.800000 * Date/Time: 1990-01-01T00:39:00 * Elevation: 3208.0 m * Recovery: 3053 m * Campaign: GISP * Basis: Sampling/drilling ice * Method/Device: Drilling/drill rig (DRILL) * Comment: GISP2 is a combination of the shallow B and the deeper D core; about 200 ka
Comment:
Accumulation rate values were calculated de-straining the depth-age scale of Meese, Sowers, et al. 3 Versions correspond to 3 different ice dynamics situations, as described in Cuffey and Clow (1997). Each one assumes a different value for the retreat distance of the ice sheet margin during the deglaciation.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPGeocode
2Accumulation of snow/ice per yearAcc ratecm/aCuffey, Kurt Msee reference(s)ice-equivalent accumulation rate, calculated assuming a 50 kilometer retreat of the ice sheet margin during deglaciation
3Accumulation of snow/ice per yearAcc ratecm/aCuffey, Kurt Msee reference(s)ice-equivalent accumulation rate, calculated assuming a 100 kilometer retreat of the ice sheet margin during deglaciation.
4Accumulation of snow/ice per yearAcc ratecm/aCuffey, Kurt Msee reference(s)ice-equivalent accumulation rate, calculated assuming a 200 kilometer retreat of the ice sheet margin during deglaciation; this is probably the most accurate of the three
Size:
33933 data points

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