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Updated: Apr 9, 2026

Evolution of Staircase Structures in Diffusive Convection
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海の循環について. 大西洋の南極反転循環を観察する 循環は,避けられない驚きの10年をもたらします

M A Srokosz1, H L Bryden2

  • 1National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK. mas@noc.ac.uk.

Science (New York, N.Y.)
|June 20, 2015
PubMed
まとめ

大西洋南極反転循環 (AMOC) は,気候モデルが予測するよりも早く減速しています. 最近の10年間の観測は,この重要な海洋熱伝送システムにおける重要な変動性と懸念される減少を明らかにしています.

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