Cold-based Glaciers
Cold-Based Glaciers is a type of glacier characterized by subglacial temperatures that remain at or below the pressure-melting point throughout, preventing basal melting and enabling glacier motion primarily through internal deformation rather than basal sliding.
96
Publications
5K
Citations
248
Authors
136
Institutions
Publications per year
2017–2026
13
Parents
96
Glacial Erosion by the Laurentide Ice Sheet
David E. Sugden · Journal of Glaciology · 1978 · 263 citations
Cold-based mountain glaciers on Mars: Western Arsia Mons
J. W. Head, D. R. Marchant · Geology · 2003 · 244 citations
Thermally controlled glacier surging
A. C. Fowler, Tavi Murray, Felix Ng · Journal of Glaciology · 2001 · 199 citations · Full text
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136

University of Otago
Dunedin, New Zealand
8 h-index
10 publications
290 citations
Université Libre de Bruxelles
Brussels, Belgium
6 h-index
10 publications
373 citations

University of Oslo
Oslo, Norway
5 h-index
16 publications
699 citations
Institute of Arctic and Alpine Research
Boulder, United States
5 h-index
9 publications
925 citations

University of Bristol
Bristol, United Kingdom
5 h-index
9 publications
186 citations

Aberystwyth University
Aberystwyth, United Kingdom
4 h-index
7 publications
244 citations

University of British Columbia
Vancouver, Canada
4 h-index
8 publications
340 citations

University of St Andrews
St Andrews, United Kingdom
4 h-index
4 publications
264 citations
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18 publications · 1.3K citations
16
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10 publications · 290 citations
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7 publications · 701 citations
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7 publications · 124 citations
7
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5 publications · 464 citations
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