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最后一次冰川退化和最后一次冰川间海平面上升的海洋强迫

Peter U Clark1,2, Feng He3, Nicholas R Golledge4,5

  • 1College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA. clarkp@onid.orst.edu.

Nature
|January 31, 2020
PubMed
概括

由于大西洋南部翻转循环 (AMOC) 的增加,海平面在最后一次脱冰期间上升得更快. 这种增强的强迫也导致了极地冰层在最后的间冰期 (LIG) 中的冰损失较大.

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