In August 2012, the Jakobshavn Glacier was flowing and breaking off into the ocean at document speeds, thrice sooner than in earlier years. Because the glacier flowed sooner, it grew to become thinner and extra unstable and in a twist, a pileup of thick ice replenished the glacier’s terminus, slowing it down once more. New work explaining the fast-then-slow motion of Jakobshavn might assist scientists higher predict how tidewater glaciers contribute to sea degree rise.
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