Ice Sheet Deformation is the permanent, internal distortion of ice mass under stress, distinguished from surface ablation or basal sliding by its origin in the viscous flow of ice within the glacier system.
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Ice Flow of the Antarctic Ice Sheet
Eric Rignot, J. Mouginot, B. Scheuchl · Science · 2011 · 1.3K citations · Full text
Jack D. Ives, George H. Denton, Terence J. Hughes · Mountain Research and Development · 1981 · 844 citations
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Centre National de la Recherche Scientifique
Paris, France
20 h-index
69 publications
6.2K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
18 h-index
56 publications
9.2K citations
British Antarctic Survey
Cambridge, United Kingdom
15 h-index
32 publications
24.2K citations
Durham University
Durham, United Kingdom
14 h-index
27 publications
1.9K citations
University of Alaska Fairbanks
Fairbanks, United States
14 h-index
37 publications
2.9K citations
Jet Propulsion Laboratory
Pasadena, United States
14 h-index
26 publications
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University of Bristol
Bristol, United Kingdom
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20 publications
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The Ohio State University
Columbus, United States
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28 publications
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- Journal of Glaciology
94 publications · 5.7K citations
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- Journal of Geophysical Research Atmospheres
JGR · 25 publications · 3.7K citations
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- Annals of Glaciology
37 publications · 1.5K citations
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- Quaternary Science Reviews
27 publications · 1.7K citations
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- The cryosphere
23 publications · 3.1K citations
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