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Taylor, Kendrick C (2000): GISP2 Electrical conductivity measurements (average data). 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: 72.970000 * Longitude: -38.800000
Date/Time Start: 1990-01-01T00:39:00 * Date/Time End: 1990-01-01T00:39:00
Minimum DEPTH, ice/snow: 4.11 m * Maximum DEPTH, ice/snow: 3040.55 m
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
This ECM data represents 0.5 meter averages of the full resolution data. The GISP2 B core was used for the first 100 meters; the D core thereafter. All depths are D core depths, ages are on the Meese/Sowers timescale.
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, ice/snowDepth ice/snowmGeocode
2AGEAgeka BPGeocode
3Conductivity, electrical, iceCond electrTaylor, Kendrick CCalculatedgiven in microamps
5488 data points

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