东格陵兰洋流（East Greenland Current）由源自北冰洋，带来冰冻、低盐度、往南的水流沿著东格陵兰岸边。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。
参见
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