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...

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Bibliographic Details
Main Authors: Hageman, Tim, Mejía, Jessica, Duddu, Ravindra, Martínez-Pañeda, Emilio
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-346
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-346/