Deformation, warming and softening of Greenland’s ice by refreezing meltwater
13. Climate action
01 natural sciences
0105 earth and related environmental sciences
DOI:
10.1038/ngeo2179
Publication Date:
2014-06-13T09:03:35Z
AUTHORS (9)
ABSTRACT
When basal meltwater refreezes, the resulting warm ice can influence the flow dynamics of the ice sheet above. An analysis of airborne gravity and radar data identifies extensive basal-ice units across the northern Greenland ice sheet that coincide with areas of deformed ice and fast ice flow.
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