Large arctic temperature change at the Wisconsin-Holocene glacial transition

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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.

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Publication type Article
Publication Subtype Journal Article
Title Large arctic temperature change at the Wisconsin-Holocene glacial transition
Series title Science
DOI 10.1126/science.270.5235.455
Volume 270
Issue 5235
Year Published 1995
Language English
Publisher American Association for the Advancement of Science
Description 4 p.
First page 455
Last page 458
Country Greenland
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