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ocean circulation
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ocean circulation
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理学
大洋环流
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ocean circulation
大洋环流
大洋海水在海面风应力的驱动下,以及在太阳辐射、结冰融冰、降水和蒸发等热盐效应作用下,形成大范围的海水密度分布不均匀,便产生水平压强梯度力,使海水由某个海域向另一海域流动,形成首尾相接的独立环流系统或流旋。又称洋流。
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