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Updated: Jul 8, 2026

Evolution of Staircase Structures in Diffusive Convection
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Published on: September 5, 2018

热带和高度大西洋温度在最后一个冰川结束时的同步性

David W Lea1, Dorothy K Pak, Larry C Peterson

  • 1Department of Geological Sciences and Marine Science Institute, University of California, Santa Barbara, CA 93106, USA. lea@geol.ucsb.edu

Science (New York, N.Y.)
|September 6, 2003
PubMed
概括

热带大西洋海面温度 (SST) 紧密跟踪了格陵兰岛和大气中甲在最后一次冰川结束期间的变化. 年轻的干旱期出现了显著的SST下降,与热带融合区的变化有关.

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