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geostrophic currents
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geostrophic currents
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地转流
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geostrophic currents
地转流
当由海水密度分布不均匀所产生的水平压强梯度力与水平地转偏向力平衡时所产生的理想海流,这种近似在忽略湍流摩擦力作用的较深的海洋内区广泛存在。
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