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Record #126173:

The connection between ice dynamics and paleoclimate from ice cores: a study of Taylor Dome, Antarctica / E.D. Waddington, D.L. Morse, Pieter M. Grootes, E.J. Steig.

Title: The connection between ice dynamics and paleoclimate from ice cores: a study of Taylor Dome, Antarctica / E.D. Waddington, D.L. Morse, Pieter M. Grootes, E.J. Steig.
Author(s): Waddington, E. D.
Morse, D. L.
Grootes, Pieter M.
Steig, E. J.
Date: 1993.
Publisher: Berlin: Springer
In: Ice in the climate system. (1993.),
Abstract: Data from snow-pit measurements and from weather stations demonstrate that climate signal is incorporated into firn at Taylor Dome, where ice core is to be drilled to bedrock in 1993-94 austral season. Field observations of ice surface and bedrock topography, as well as ice movement, allow creation and verification of dynamics and thermodynamics models which are used as site-evaluation tools to predict deep-temperature characteristics, depth--age scale, expected depth of ice-age transition, and expected thickness of annual layers in core.
Notes:

In: Ice in the climate system / W. Richard Peltier, ed.

Keywords: 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.324.5 -- Land ice, flow.
551.583.3 -- Climatic changes, Quaternary.
551.336 -- Ice ages.
551.79 -- Quaternary.
551.588.5 -- Climate, relationship with ice.
551.578.46 -- Snow cover and snow patches.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*762.4) -- Scott Coast.
SPRI record no.: 126173

MARCXML

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245 04 ‡aThe connection between ice dynamics and paleoclimate from ice cores :‡ba study of Taylor Dome, Antarctica /‡cE.D. Waddington, D.L. Morse, Pieter M. Grootes, E.J. Steig.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 499-516 :‡bdiags., map.
490 0# ‡aNATO ASI Series. Series I, Global environmental change ;‡v12
500 ## ‡aIn: Ice in the climate system / W. Richard Peltier, ed.
520 3# ‡aData from snow-pit measurements and from weather stations demonstrate that climate signal is incorporated into firn at Taylor Dome, where ice core is to be drilled to bedrock in 1993-94 austral season. Field observations of ice surface and bedrock topography, as well as ice movement, allow creation and verification of dynamics and thermodynamics models which are used as site-evaluation tools to predict deep-temperature characteristics, depth--age scale, expected depth of ice-age transition, and expected thickness of annual layers in core.
650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc
650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc
650 07 ‡a551.324.5 -- Land ice, flow.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*762.4) -- Scott Coast.‡2udc
700 1# ‡aWaddington, E. D.
700 1# ‡aMorse, D. L.
700 1# ‡aGrootes, Pieter M.
700 1# ‡aSteig, E. J.
773 0# ‡7nnam ‡aW. Richard Peltier, ed. ‡tIce in the climate system. ‡dBerlin : Springer, 1993. ‡wSPRI-126141
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004