图像中巨大的白色圆形结构就是东格陵兰洋流搬运多年的海冰冰块。
The large white circular shapes in this image are pieces of multiyear ice carried to this location by the East Greenland Current.
洋流带来的冰山形状巨大、体积厚重；所以显而易见，格陵兰岛沿岸的浮冰大部分是来自于其他地方（不是由当地海水结冰形成）。
Ice carried by this current occurs in large, thick pieces, and the ice in this swath along the Greenland coast almost certainly originated elsewhere.
更多热量到达了格陵兰和北极的冰区，所以冷洋流沿着欧洲海岸线向下流动，欧洲就会经历较冷的天气。
More heat is over the ice fields of Greenland and the Arctic, so colder water flows down along the European coastline, thus colder weather in Europe.
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