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来自维基百科,自由的百科全书
东格陵兰洋流(East Greenland Current)由源自北冰洋,带来冰冻、低盐度、往南的水流沿着东格陵兰岸边。东格陵兰洋流为形成近极地环流(gyre)的五条主要洋流之一,并提供北冰洋的冰冻水源流往大西洋的一个主要途径。
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