Firn Processes
Firn Processes is the geophysical transformation sequence in which snow undergoes densification, recrystallization, and pore closure under the influence of temperature gradients, overburden pressure, and meltwater percolation, ultimately transitioning into glacial ice within the porous, intergranular medium of firn.
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184
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142
C. Goujon, J. M. Barnola, Catherine Ritz · Journal of Geophysical Research Atmospheres · 2003 · 292 citations · Full text
Greenland meltwater storage in firn limited by near-surface ice formation
Horst Machguth, D. van As, Jason E. Box et al. · Nature Climate Change · 2016 · 269 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
18 h-index
67 publications
5.2K citations
University of Washington
Seattle, United States
16 h-index
39 publications
2.9K citations
Utrecht University
Utrecht, The Netherlands
16 h-index
57 publications
6.8K citations
Laboratoire de Glaciologie et Géophysique de l’Environnement
Saint-Martin-d'Hères, France
13 h-index
43 publications
3.2K citations
University of Colorado Boulder
Boulder, United States
12 h-index
19 publications
1.2K citations
Earth and Space Research
Seattle, United States
12 h-index
31 publications
2.3K citations
University of Copenhagen
Copenhagen, Denmark
10 h-index
25 publications
716 citations
Goddard Space Flight Center
Greenbelt, United States
9 h-index
15 publications
1.3K citations
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28 publications · 1.9K citations
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17 publications · 805 citations
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11 publications · 774 citations
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JGR · 7 publications · 960 citations
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