Glacial Advance
Glacial Advance is a geomorphological process denoting the forward movement of a glacier's terminus due to a positive mass balance, wherein ice accumulation exceeds ablation over successive years.
517
Publications
28.1K
Citations
1.5K
Authors
607
Institutions
Publications per year
2017–2026
80
Parents
517
Glacial North Atlantic: Sea‐surface conditions reconstructed by GLAMAP 2000
Uwe Pflaumann, Michael Sarnthein, Mark R Chapman et al. · Paleoceanography · 2003 · 367 citations · Full text
Holocene glacial and climatic variations on Spitsbergen, Svalbard
John Inge Svendsen, Jan Mangerud · The Holocene · 1997 · 288 citations
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Institute of Arctic and Alpine Research, United States
7 publications · 473 citations
7
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1–5 of 1.5K
607
ETH Zurich
Zurich, Switzerland
21 h-index
49 publications
3.4K citations
University of Colorado Boulder
Boulder, United States
16 h-index
34 publications
2.3K citations

Centre National de la Recherche Scientifique
Paris, France
16 h-index
69 publications
4.1K citations
University of Bergen
Bergen, Norway
15 h-index
23 publications
1.6K citations
Institute of Arctic and Alpine Research
Boulder, United States
15 h-index
33 publications
1.8K citations
University of Bern
Bern, Switzerland
13 h-index
29 publications
1.6K citations
United States Geological Survey
Reston, United States
13 h-index
24 publications
1.1K citations

University of Canterbury
Christchurch, New Zealand
12 h-index
19 publications
566 citations
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QR · 40 publications · 3.4K citations
29
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31 publications · 1.7K citations
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26 publications · 1.4K citations
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JQS · 26 publications · 1.8K citations
22
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35 publications · 1.5K citations
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