USGS海洋学家和这份研究报告共同作者多兰(Kara Doran)解释:「因为格陵兰冰原(Greenland Ice Sheet)融化后的淡水流入海洋,干扰循环导致洋流速 度减缓。
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以上来源于: WordNet
But the Greenland ice sheet is not one solid, smooth mass of ice.
但是,格陵兰冰盖不是一个牢固光滑的冰体。
Several metres of sea level rise is now inevitable as the Greenland ice sheet disappears.
现在,随着格陵兰冰原的消失,海平面上升几米已是不可避免。
The giant Greenland ice sheet may be more resistant to temperature rise than experts realised.
也许广袤的格林兰冰原对温度升高的抵御能力比专家们估计的要强得多。
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