Satellite observations of snowfall regimes over the Greenland Ice Sheet
<p>The mass of the Greenland Ice Sheet (GrIS) is decreasing due to increasing surface melt and ice dynamics. Snowfall both adds mass to the GrIS and has the capacity to reduce surface melt by increasing surface brightness, reflecting additional solar radiation back to space. Modeling the GrIS’...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-12-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/14/4379/2020/tc-14-4379-2020.pdf |