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东格陵兰海流
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东格陵兰海流
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理学
东格陵兰海流
释
east Greenland cold current
东格陵兰海流
源自北冰洋,具有低温、低盐特性,表层水温0~2.4℃,春季多冰山和浮冰。受大气环流影响,沿格陵兰岛东岸向南流的寒流。向北转入大西洋的拉布拉多海。
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