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.
Original language | English (US) |
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Pages (from-to) | 455-458 |
Number of pages | 4 |
Journal | Science |
Volume | 270 |
Issue number | 5235 |
State | Published - Oct 20 1995 |
All Science Journal Classification (ASJC) codes
- General