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傾斜流
释义
傾斜流
qīng xié liú
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:2025/5/29 21:58:06