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Limits to future expansion of surface‐melt‐enhanced ice flow into the interior of western Greenland
Author(s) -
Poinar Kristin,
Joughin Ian,
Das Sarah B.,
Behn Mark D.,
Lenaerts Jan T. M.,
Broeke Michiel R.
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl063192
Subject(s) - meltwater , greenland ice sheet , geology , ice stream , elevation (ballistics) , geomorphology , ice sheet , streams , glacier , oceanography , physical geography , hydrology (agriculture) , cryosphere , sea ice , geometry , geography , computer network , mathematics , geotechnical engineering , computer science
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 ~1600 m. 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 ~1600 m crevassing limit is well below the wet‐frozen basal transition (~2000 m). Together, these data sets suggest that new supraglacial lakes will have a limited effect on the inland expansion of melt‐induced seasonal acceleration.