Proglacial river stage derived from georectified time-lapse camera images, Inglefield Land, Northwest Greenland
The Greenland Ice Sheet is a leading source of global sea level rise, due to surface meltwater runoff and glacier calving. However, given a scarcity of proglacial river gauge measurements, ice sheet runoff remains poorly quantified. This lack of in situ observations is particularly acute in Northwes...
| Published in: | Frontiers in Earth Science |
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| Main Authors: | , , , , , , , , , |
| Format: | Article |
| Language: | English |
| Published: |
Frontiers Media S.A.
2023-06-01
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| Subjects: | |
| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2023.960363/full |
