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Steig, Eric J (2006): Age model and delta deuterium of ice core Taylor Dome from 20 to 10 kyr. PANGAEA, https://doi.org/10.1594/PANGAEA.472493

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Related to:
Steig, Eric J; Brook, Edward J; White, James W C; Sucher, C M; Bender, Michael L; Lehman, Scott J; Morse, David L; Waddington, Edwin D; Clow, Gary D (1998): Synchronous climate changes in Antarctica and the North Atlantic. Science, 282(5386), 92-95, https://doi.org/10.1126/science.282.5386.92
Steig, Eric J; Morse, David L; Waddington, Edwin D; Stuiver, Minze; Grootes, Pieter Meiert; Mayewski, Paul Andrew; Twickler, Mark S; Whitlow, Sallie I (2000): Wisconsinan and Holocene climate history from an ice core at Taylor Dome, Western Ross Embayment, Antarctica. Geografiska Annaler: Series A, Physical Geography, 82(2-3), 213, https://doi.org/10.1111/j.0435-3676.2000.00122.x
Coverage:
Latitude: -77.783330 * Longitude: 158.716670
Date/Time Start: 1993-01-01T00:00:00 * Date/Time End: 1994-12-31T00:00:00
Minimum DEPTH, ice/snow: 345.60 m * Maximum DEPTH, ice/snow: 379.40 m
Event(s):
Taylor_Dome (TD) * Latitude: -77.783330 * Longitude: 158.716670 * Date/Time Start: 1993-01-01T00:00:00 * Date/Time End: 1994-12-31T00:00:00 * Elevation: 2365.0 m * Recovery: 554.99 m * Location: Antarctica * Campaign: TAYLOR_DOME * Basis: Sampling/drilling ice * Method/Device: Electromechanical drill (EMD)
Comment:
Two timescales are reported here. The original is as reported in Steig et al., Science 282 (1998). This was adjusted slightly to match the flow-model constrained st9810 timescale (Steig et al., Geografiska Annaler, 2000). The adjustment is well within the uncertainties of the timescale and is more the sake of convenience. In general, the st9810 timescale should be used.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, ice/snowDepth ice/snowmGeocode
2Age modelAge modelkaSteig, Eric JAge model, st9810
3Age model, optionalAge model optkaSteig, Eric JAge model, Steig et al (1998)
4δ DeuteriumδD‰ SMOWSteig, Eric J
Size:
600 data points

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