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Taylor, Kendrick C (2003): GISP2 Electrical conductivity measurements (Core D). PANGAEA,

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Related to:
Chylek, P; Johnson, B; Damiano, P A; Taylor, Kendrick C; Clement, Poul (1995): Biomass burning record and black carbon in the GISP2 ice core. Geophysical Research Letters, 22(2), 89-92,
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
Taylor, Kendrick C; Alley, Richard B; Fiacco, R J; Grootes, Pieter Meiert; Lamorey, G W; Mayewski, Paul Andrew; Spencer, M J (1992): Ice core dating and chemistry by direct-current electrical conductivity. Journal of Glaciology, 38, 325-332,
Taylor, Kendrick C; Alley, Richard B; Lamorey, G W; Mayewski, Paul Andrew (1997): Electrical measurements on the Greenland Ice Sheet Project 2 core. Journal of Geophysical Research: Oceans, 102(C12), 26511-26518,
Taylor, Kendrick C; Lamorey, G W; Doyle, G A; Alley, Richard B; Grootes, Pieter Meiert; Mayewski, Paul Andrew; White, James W C; Barlow, L K (1993): The `flickering switch` of late Pleistocene climate change. Nature, 361(6411), 432-436,
Taylor, Kendrick C; Mayewski, Paul Andrew; Twickler, Mark S; Whitlow, Sallie I (1996): Biomass burning recorded in the GISP2 ice core: a record from eastern Canada? The Holocene, 6(1), 1-6,
Greenland Ice Core Projects (GRIP/GISP/NGRIP)
Latitude: 72.588000 * Longitude: -38.457000
Minimum DEPTH, ice/snow: 100.995 m * Maximum DEPTH, ice/snow: 3041.430 m
GISP2-D * Latitude: 72.588000 * Longitude: -38.457000 * Elevation Start: 3203.0 m * Elevation End: 0.0 m * Campaign: GISP * Basis: Sampling/drilling ice * Method/Device: Drilling/drill rig (DRILL) * Comment: The length of the 3-km borehole at the GISP2 site was measured by two completely independent geophysical logging systems, the University of Copenhagen system (UCPH) and the U.S. Geological Survey's temperature system (USGS). Both systems utilized steel logging cables. The depth calibration factor for the UCPH system was determined from the measured length of the GRIP ice core while the USGS system was calibrated using a fiberglass tape measure with a low coefficient of thermal expansion. The accuracy of the depth measurements for both systems is estimated to be 2-3 m at a depth of 3 km. Inclination/azimuth measurements from the UCPH logger have been used to calculate the true vertical depth of the borehole from the measured total slant length. UCPH/true vertical depth (m):3047.8 slant length (m):3056.5 USGS/true vertical depth (m):3047.9, slant length (m):3056.6
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, ice/snowDepth ice/snowmGeocode
2Conductivity, electrical, currentCond electrµATaylor, Kendrick C
2372386 data points

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