Glacier Advance
Glacier Advance is a geomorphological process denoting the forward movement of a glacier's terminus relative to its bed, resulting from a positive mass balance that causes the ice front to extend downvalley over successive years.
357
Publications
19.9K
Citations
949
Authors
389
Institutions
Publications per year
2017–2026
65
357
Chronology of the last glacial cycle in the European Alps
Susan Ivy‐Ochs, Hanns Kerschner, Anne U. Reuther et al. · Journal of Quaternary Science · 2008 · 479 citations · Full text
Rapid retreat and acceleration of Helheim Glacier, east Greenland
Ian M. Howat, Ian Joughin, Sławek Tulaczyk et al. · Geophysical Research Letters · 2005 · 303 citations · Full text
1–5 of 357
949
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1–5 of 949
389
ETH Zurich
Zurich, Switzerland
18 h-index
37 publications
2.8K citations
University of Colorado Boulder
Boulder, United States
12 h-index
23 publications
1.6K citations
United States Geological Survey
Reston, United States
12 h-index
19 publications
738 citations
University of Copenhagen
Copenhagen, Denmark
12 h-index
28 publications
1.2K citations
University of Zurich
Zurich, Switzerland
12 h-index
21 publications
2.4K citations
University of Iceland
Reykjavik, Iceland
11 h-index
19 publications
758 citations

Universität Innsbruck
Innsbruck, Austria
11 h-index
18 publications
1.6K citations

Chinese Academy of Sciences
Beijing, China
11 h-index
38 publications
1.6K citations
1–8 of 389
40 publications · 1.9K citations
23
h-index
QR · 24 publications · 2.1K citations
20
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23 publications · 1.4K citations
18
h-index
21 publications · 776 citations
17
h-index
15 publications · 1K citations
15
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1–5