Firn Compaction
Firn compaction is a physicochemical process within the cryosphere whereby loose, granular snow undergoes densification into glacier ice through intergranular deformation and bonding under the influence of overlying snow load and atmospheric conditions, distinguishing it from other firn processes by its role in reducing pore space and enabling mass transfer within the glacier mass balance system.
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Louise Sandberg Sørensen, Sebastian B. Simonsen, Karina Nielsen et al. · The cryosphere · 2011 · 229 citations · Full text
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Goddard Space Flight Center
Greenbelt, United States
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31 publications
6.7K citations
Utrecht University
Utrecht, The Netherlands
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26 publications
1.3K citations
University of Washington
Seattle, United States
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9 publications
356 citations
Earth and Space Research
Seattle, United States
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9 publications
356 citations
Stinger Ghaffarian Technologies (United States)
Greenbelt, United States
4 h-index
9 publications
3.2K citations
University of Maryland, College Park
College Park, United States
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3 publications
109 citations
University of Copenhagen
Copenhagen, Denmark
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5 publications
852 citations

Delft University of Technology
Delft, The Netherlands
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473 citations
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