Grounding zone subglacial properties from calibrated active-source seismic methods
The grounding zone of Whillans Ice Stream, West Antarctica, exhibits an abrupt transition in basal properties from the grounded ice to the ocean cavity over distances of less than 0.5–1 km. Active-source seismic methods reveal the downglacier-most grounded portion of the ice stream is underlain by a...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , |
Format: | Text |
Language: | English |
Published: |
2021
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-15-1863-2021 https://tc.copernicus.org/articles/15/1863/2021/ |