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Updated: Jul 12, 2026

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

最後の氷河期最大期における亜極北大西洋の中深循環

D W Oppo, S J Lehman

    Science (New York, N.Y.)
    |February 19, 1993
    PubMed
    まとめ

    氷河北大西洋中間水 (GNAIW) は南洋水 (SOW) を層分化し,GNAIWは極地フロントの北に起源を示しています. 大西洋の循環の変化は,過去の大気中の二酸化炭素レベルに影響を及ぼした可能性があります.

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