During previous interglacial periods, when glaciers retreated, they left behind open land in their wakes.
在以往的间冰期中,当冰川消退时,它们在尾迹中留下了开阔的土地。
Turns out that when glaciers are cold enough they don't move much.
结果表明,当冰川足够冷的时候,它们几乎就不动了。
Higher air temperatures can increase surface melting, but warm ocean currents accelerate ice loss more when glaciers flow into the sea.
气温升高能够加速冰川表面的融化,但是当冰川漂移入海之后,温暖的洋流对冰雪消融发挥了更重要的推动作用。
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