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Large arctic temperature change at the Wisconsin-Holocene glacial transition

Science
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Abstract

Analysis of borehole temperature and Greenland Ice Sheet Project II ice-core isotopic composition reveals that the warming from average glacial conditions to the Holocene in central Greenland was large, approximately 15??C. This is at least three times the coincident temperature change in the tropics and mid-latitudes. The coldest periods of the last glacial were probably 21??C colder than at present over the Greenland ice sheet.
Publication type Article
Publication Subtype Journal Article
Title Large arctic temperature change at the Wisconsin-Holocene glacial transition
Series title Science
Volume 270
Issue 5235
Year Published 1995
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Science
First page 455
Last page 458
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