Natalie L Roberts1, Alexander M Piotrowski, Jerry F McManus

  • 1Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. nr297@cam.ac.uk

Science (New York, N.Y.)
|January 2, 2010
PubMed
概括

在最后一次脱冰期间,海洋循环的变化是同步的,影响了深水源和翻转率. 像海因里希事件1这样的千年规模的事件只影响浅层翻转,与整个海洋气候变化不同.

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