Changes in the Velocity Structure of the Greenland Ice Sheet
摘要：
Using satellite radar interferometry observations of Greenland, we detected widespread glacier acceleration below 66° north between 1996 and 2000, which rapidly expanded to 70° north in 2005. Accelerated ice discharge in the west and particularly in the east doubled the ice sheet mass deficit in the last decade from 90 to 220 cubic kilometers per year. As more glaciers accelerate farther north, the contribution of Greenland to sea-level rise will continue to increase.
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关键词：
Experimental/ glaciology radiowave interferometry remote sensing by radar spaceborne radar/ Greenland ice sheet velocity structure changes satellite radar interferometry observations glacier acceleration ice discharge ice sheet mass deficit sea-level rise/ A9240V Glaciers and ice sheets A9330K Islands
DOI：
10.1126/science.1121381
被引量：
年份：
2006
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