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
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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