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Evolution of Staircase Structures in Diffusive Convection
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大西洋の深い西の境界流が南緯8度で渦に分裂する

M Dengler1, F A Schott, C Eden

  • 1Leibniz-Institut für Meereswissenschaften, Düsternbrooker Weg 20, 24105 Kiel, Germany. mdengler@ifm-geomar.de

Nature
|December 24, 2004
PubMed
まとめ

大西洋の深い西側の境界流は,南緯8度で渦に突入し,移動する渦は北大西洋の深水を南へ運ぶ. この断裂は,継続的な流れとは異なり,循環の強度を転覆する電流で発生します.

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