Asynchrony of Antarctic and Greenland climate change during the last glacial period
A central issue in climate dynamics is to understand how the Northern and Southern hemispheres are coupled during climate events. The strongest of the fast temperature changes observed in Greenland (so-called Dansgaard–Oeschger events) during the last glaciation have an analogue in the temperature r...
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Veröffentlicht in: | Nature (London) 1998-08, Vol.394 (6695), p.739-743 |
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