Firn Saturation is a hydrological state in which the pore spaces within the firn layer of a glacier or ice sheet become completely filled with liquid water, marking the condition when infiltration exceeds both retention and refreezing capacities, thereby signifying the onset of near-surface meltwater runoff or redistribution in cold firn environments.
5
Publications
231
Citations
12
Authors
10
Institutions
Publications per year
2017–2026
2
Parents
Publications
5
Authors
12
- AG
2
h-index
- RC
1
h-index
- JT
1
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- JZJulie Z. Miller
Cooperative Institute for Research in Environmental Sciences, United States
1 publications · 15 citations
1
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- TS
1
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1–5 of 12
Institutions
10
United States Geological Survey
Reston, United States
2 h-index
2 publications
111 citations
University of Wyoming
Laramie, United States
1 h-index
1 publications
23 citations
Brigham Young University
Provo, United States
1 h-index
1 publications
15 citations
University of Montana
Missoula, United States
1 h-index
2 publications
46 citations
Stockholm University
Stockholm, Sweden
1 h-index
2 publications
164 citations
University of Maryland, Baltimore County
Baltimore, United States
1 h-index
1 publications
15 citations
Goddard Space Flight Center
Greenbelt, United States
1 h-index
1 publications
15 citations
Stanford University
Stanford, United States
1 h-index
1 publications
15 citations
1–8 of 10
Venues
- Annals of Glaciology
2 publications · 111 citations
2
h-index
- Journal of Glaciology
2 publications · 105 citations
2
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- IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
1 publications · 15 citations
1
h-index
- Geophysical Research Letters
1 publications · 11 citations
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