这一段的锢囚锋和高空暖舌带来与极地空气团天气相反的变化。
The passage is an occluded front and trowal brings a change back to polar air-mass weather.
空气含水量越高导致更多的降雪,反过来,这意味着更多的极地冰盖
More moisture in the air results in more snowfall which, in turn, means more polar ice... read more.
在整个喜马拉雅冰川,同样吸收辐射的大量尘埃和其它空气中的污染物可能掩盖了黑碳的影响。 “北极地区基本上距离尘埃污染源非常远,冰雪很洁净,因此影响就特别大。”
Over Himalayan glaciers, large amounts of dust -- which also absorb radiation -- and other pollutants in the air may dampen the effect.
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