Icemelt Runoff
Icemelt Runoff is a hydrological flux term denoting the portion of streamflow originating specifically from the seasonal melting of glacier ice and snowpack within a cryospheric basin, distinguished from other runoff sources by its direct dependency on phase changes of frozen surface water under climatic forcing.
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2017–2026
5
Variants
Glacial Runoff
Parents
21
Glacier algae accelerate melt rates on the south-western Greenland Ice Sheet
Joseph M. Cook, Andrew Tedstone, Christopher J. Williamson et al. · The cryosphere · 2020 · 164 citations · Full text
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Chinese Academy of Sciences
Beijing, China
3 h-index
9 publications
440 citations
Environment and Climate Change Canada
Ottawa, Canada
2 h-index
5 publications
193 citations
Geological Survey of Denmark and Greenland
Copenhagen, Denmark
2 h-index
4 publications
317 citations
Hainan Marine Monitoring and Forecasting Center
Longhua, China
1 h-index
1 publications
12 citations
Liverpool John Moores University
Liverpool, United Kingdom
1 h-index
1 publications
164 citations

The University of Sydney
Sydney, Australia
1 h-index
1 publications
164 citations
Institute of Arctic and Alpine Research
Boulder, United States
1 h-index
1 publications
79 citations
Brown University
Providence, United States
1 h-index
1 publications
164 citations
1–8 of 41
2 publications · 70 citations
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2 publications · 25 citations
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1 publications · 12 citations
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1 publications · 23 citations
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1 publications · 156 citations
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