Ice viscosity governs hydraulic fracture causing rapid drainage of supraglacial lakes
Full-thickness crevasses can transport water from the glacier surface to the bedrock where high water pressures can open kilometre-long cracks along the basal interface, which can accelerate glacier flow. We present a first computational modelling study that describes time-dependent fracture propaga...
Main Authors: | , , , |
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Format: | Text |
Language: | English |
Published: |
2024
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Subjects: | |
Online Access: | https://doi.org/10.5194/egusphere-2024-346 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-346/ |