Science (New York, N.Y.)
|July 20, 1973
PubMed
まとめ

インド洋の赤道部では,モンスーンの移行時に,迅速で狭い東向きの流れが形成されます. この海流は,熱線を上げ,沈めて海洋質量構造を大幅に変化させます.

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