Clouds reflect sunlight and slow down the melting of ice, protecting the Arctic. Ice crystals make clouds heavier and more likely to dissipate, leaving the ice vulnerable to rays of hot sun. But the ice can’t form in the clouds without something to latch on to. That’s where the dust comes in, providing a kind of “seed” or “nucleus” for the ice to form around.
NASA scientists hypothesize that as the ice retreats, more of Greenland’s exposed landmass is shedding dust, which is then carried north by heavy winds to form ice particles in the clouds above. These dust-heavy clouds then disappear more quickly and leave more Arctic ice exposed, hastening the melt.
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