Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition

Computer Science

Scientific paper

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Scientific paper

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^circC. 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^circC colder than at present over the Greenland ice sheet.

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