Firn Percolation
Firn Percolation is a hydrological process in which meltwater derived from snow or ice surfaces infiltrates downward through the porous snowpack and refreezes within the underlying firn layer, distinguished by its role in redistributing mass and energy within polar and glacial environments.
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118
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75
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2017–2026
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Water flow through temperate glaciers
Andrew G. Fountain, Joseph S. Walder · Reviews of Geophysics · 1998 · 747 citations · Full text
Meltwater-induced relocation of chemical species in Alpine firn
Anja Eichler, Margit Schwikowski, H. W. Gäggeler · Tellus B · 2001 · 122 citations · Full text
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Utrecht University
Utrecht, The Netherlands
9 h-index
19 publications
1.4K citations
University of Colorado Boulder
Boulder, United States
8 h-index
10 publications
569 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
4 h-index
4 publications
181 citations
Dartmouth College
Hanover, United States
3 h-index
6 publications
316 citations
Natural Resources Canada
Ottawa, Canada
2 h-index
2 publications
85 citations
Geological Survey of Canada
Ottawa, Canada
2 h-index
2 publications
85 citations
Geological Survey of Denmark and Greenland
Copenhagen, Denmark
2 h-index
7 publications
133 citations

British Antarctic Survey
Cambridge, United Kingdom
2 h-index
2 publications
225 citations
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6 publications · 369 citations
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5 publications · 222 citations
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4 publications · 185 citations
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2 publications · 80 citations
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2 publications · 187 citations
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