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Ekman drift currents
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Ekman drift currents
Encyclopedia
理学
埃克曼漂流
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Ekman drift currents
埃克曼漂流
理想化的无边界、无限深和密度均匀的海洋,因海面受稳定的风长时间作用,吹动表层海水运动。通过湍流黏性力,动量逐层向下传递,引起各层海水的运动,在运动过程中,同时受到地转偏向力的作用而改变方向和大小,当两者达到平衡时出现的稳定海流。又称风漂流。
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