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Updated: Jul 23, 2026

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
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Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

Published on: March 13, 2017

氷河海洋の温度と酸素同位体組成に対する孔腔流体の制約

Schrag1, Hampt, Murray

  • 1D. P. Schrag, Department of Geological and Geophysical Sciences, Princeton University, Princeton, NJ 08544-1003, USA. G. Hampt, Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA. D. W. Murray, Department of Geological Sciences, Brown University, Providence, RI 02912, USA.

Science (New York, N.Y.)
|June 28, 1996
PubMed
まとめ

最後の氷河期最大期の間,海洋の温度はより低かった. 熱帯大西洋の毛孔液とフォラミニフェラの酸素同位体の分析は,深水温の4°Cの低下を明らかにし,気候再構築に貢献しています.

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