LARGE ARCTIC TEMPERATURE CHANGE AT THE WISCONSIN-HOLOCENE GLACIAL TRANSITION

摘要

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 degrees 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 degrees C colder than at present over the Greenland ice sheet.