The input of relatively light freshwater also alters circulation patterns that cycle water between Greenland and northern North America, which could lead to more water on the North American end.

 
  • 體積相對輕的淡水流入海洋后,還會(huì )改變格林蘭島和北美洲北部之間的洋流循環(huán)模式,這種情況最終可能導致更多的海水淹沒(méi)北美大陸。
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