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埃克曼效应
海洋表层的风生海流在黏性力及科里奥利力耦合作用下,随深度增加,海流流速递减且方向连续右转(北半球)或左转(南半球),形成三维空间内速度矢量端点连线绕垂直轴呈螺旋形态的海流结构效应。
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Artibonite River
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