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: | , , , , , , , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Frontiers Media SA
2023
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Subjects: | |
Online Access: | http://dx.doi.org/10.3389/feart.2023.960363 https://www.frontiersin.org/articles/10.3389/feart.2023.960363/full |