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Updated: Jun 7, 2026

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
最後の氷河期最大期における大西洋深海の逆流
César Negre1, Rainer Zahn, Alexander L Thomas
1Institut de Ciència i Tecnologia Ambientals (ICTA), Universitat Autònoma de Barcelona, 08193 Bellaterra, Spain. cesar@negre.us
Nature
|November 5, 2010
まとめ
大西洋南極の転覆循環 (MOC) は,最後の氷河期最大期中に逆転した可能性があり,南洋から北に流れる深い水は,今日のパターンとは違います.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 海洋学 海洋学 海洋学
背景:
- 大西洋南極の転覆循環 (MOC) は,熱を再分配し,深海を換気することで,地球温暖化に決定的な役割を果たしています.
- 過去のMOCの行動,特に最後の氷河期最大期の間は,代理人の矛盾した証拠で議論されています.
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