Antarctic ice sheets are melting now three times faster than they did in the 1990s, a new scientific study says.
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During the Holocene, the Greenland and Antarctic ice sheets have been relatively stable, as reflected in the stability of the sea level.
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Mechanisms on the verge of being instigated include loss of Arctic sea ice, shrinkage of the Greenland ice sheet, loss of Antarctic ice shelves, and shrinkage of the Antarctic ice sheets.
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