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傾斜流
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傾斜流
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因风力、降水、气压变化或大量河水注入的影响，造成海平面倾斜，使海水由高处流向低处所形成的海流。在地球偏转力的作用下，其流向在北半球偏右，在南半球偏左。
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更新时间：2026/5/27 4:10:19