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Updated: Jul 30, 2025

Evolution of Staircase Structures in Diffusive Convection
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インド洋の塩分濃度増減 氷河期の海洋循環回復

Sophie Nuber1,2,3, James W B Rae4, Xu Zhang5

  • 1School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK. snuber@ntu.edu.tw.

Nature
|May 10, 2023
PubMed
まとめ

氷河期は海水位が下がるため,インド洋の塩分度が上昇し,海洋循環に影響を与えました. 脱氷時に放出された塩分は,大西洋南側転覆循環と地球気候に影響を与えた.

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