东格陵兰洋流

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。
单词 | East Greenland Current |
释义 |
East Greenland Current
中文百科
东格陵兰洋流![]() 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。
英语百科
East Greenland Current 东格陵兰洋流![]() The East Greenland Current (EGC) is a cold, low salinity current that extends from Fram Strait (~80N) to Cape Farewell (~60N). The current is located off the eastern coast of Greenland along the Greenland continental margin. The current cuts through the Nordic Seas (the Greenland and Norwegian Seas) and through the Denmark Strait. The current is of major importance because it directly connects the Arctic to the Northern Atlantic, it is a major contributor to sea ice export out of the Arctic, and it is a major freshwater sink for the Arctic. |
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