期刊
GEOPHYSICAL RESEARCH LETTERS
卷 42, 期 6, 页码 1800-1807出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL063192
关键词
moulins
资金
- National Science Foundation (CReSIS) [ANT-0424589, ARC-1023382, ARC-1023364]
- Polar Program of the Netherlands Organisation for Scientific Research
- Office of Polar Programs (OPP)
- Directorate For Geosciences [1023364, 1023382] Funding Source: National Science Foundation
Moulins are important conduits for surface meltwater to reach the bed of the Greenland Ice Sheet. It has been proposed that in a warming climate, newly formed moulins associated with the inland migration of supraglacial lakes could introduce surface melt to new regions of the bed, introducing or enhancing sliding there. By examining surface strain rates, we found that the upper limit to where crevasses, and therefore moulins, are likely to form is similar to 1600m. This is also roughly the elevation above which lakes do not drain completely. Thus, meltwater above this elevation will largely flow tens of kilometers through surface streams into existing moulins downstream. Furthermore, results from a thermal ice sheet model indicate that the similar to 1600m crevassing limit is well below the wet-frozen basal transition (similar to 2000m). Together, these data sets suggest that new supraglacial lakes will have a limited effect on the inland expansion of melt-induced seasonal acceleration.
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