Ice Surface Ablation
Ice Surface Ablation is a glaciological process denoting the loss of ice mass from the surface of a glacier through the combined effects of melting, sublimation, and evaporation, distinguished from other ablation mechanisms by its exclusive occurrence at the glacier–atmosphere interface.
295
Publications
18.2K
Citations
822
Authors
326
Institutions
Publications per year
2017–2026
54
Parents
295
1–5 of 295
822
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Geological Survey of Denmark and Greenland
Copenhagen, Denmark
19 h-index
68 publications
3.5K citations

University of Alaska Fairbanks
Fairbanks, United States
15 h-index
29 publications
1.3K citations

Chinese Academy of Sciences
Beijing, China
14 h-index
77 publications
2.9K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
46 publications
3.2K citations
Utrecht University
Utrecht, The Netherlands
13 h-index
28 publications
1.6K citations

Universität Innsbruck
Innsbruck, Austria
12 h-index
21 publications
1.2K citations

Aberystwyth University
Aberystwyth, United Kingdom
11 h-index
27 publications
1.7K citations

University of Bristol
Bristol, United Kingdom
10 h-index
29 publications
2.2K citations
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88 publications · 6.1K citations
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27 publications · 1.2K citations
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14 publications · 902 citations
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JGR · 14 publications · 2.9K citations
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8 publications · 543 citations
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