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大西洋南部循环的崩和快速恢复与降冰气候变化有关

J F McManus1, R Francois, J-M Gherardi

  • 1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. jmcmanus@whoi.edu

Nature
|April 23, 2004
PubMed
概括

大西洋南部翻转循环在最后一次脱冰期间几乎停止了,特别是在海因里希事件H1.1周围. 其随后的重新加速与主要的区域变暖事件相吻合,证实了它在突然气候变化中的作用.

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