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MOC
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MOC
Encyclopedia
理学
第四纪大洋环流
释
meridional overturning circulation; MOC
经向翻转流
由于南大洋和北大西洋表层海水在海面风力的驱动以及结冰、融冰、降水和蒸发等热盐效应作用下,造成大范围的海水密度分布不均匀,使南大洋形成的深层水向北流动,在北半球海洋深部上翻并向南流动;在北大西洋形成的深层水也一并向南流动,这些南向的洋流在南大洋西风驱动的上升流作用下最终回到南大洋,进而形成的洋流。
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