Revealing the former bed of Thwaites Glacier using sea-floor bathymetry
The geometry of the sea floor beyond Thwaites Glacier (TG) is a major control on the routing of warm ocean waters towards the ice stream’s grounding zone, which has led to increased mass loss through sub-ice-shelf melting and resulting accelerated ice flow. Nearshore topographic highs act as pinning...
Main Authors: | , , , , , , , , , , , , , , , , , |
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Format: | Text |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-2020-25 https://tc.copernicus.org/preprints/tc-2020-25/ |