“Ekman drift currents”的概念、定义、翻译、参考文献-科学参考

单词	Ekman drift currents
释义	Ekman drift currents Encyclopedia 理学埃克曼漂流释 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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