Seasonal variations in the flow of land-terminating glaciers in central-west Greenland using Sentinel-1 imagery
Land-terminating sectors of the Greenland ice sheet flow faster in summer after surface meltwater reaches the subglacial drainage system. Speedup occurs when the subglacial drainage system becomes saturated, leading to a reduction in the effective pressure which promotes sliding of the overlying ice...
Published in: | Remote Sensing |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2018
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Subjects: | |
Online Access: | https://eprints.lancs.ac.uk/id/eprint/130371/ https://doi.org/10.3390/rs10121878 |