Buoyant forces promote tidewater glacier iceberg calving through large basal stress concentrations
Iceberg calving parameterisations currently implemented in ice sheet models do not reproduce the full observed range of calving behaviours. For example, though buoyant forces at the ice front are known to trigger full-depth calving events on major Greenland outlet glaciers, a multi-stage iceberg cal...
Published in: | The Cryosphere |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-13-1877-2019 https://tc.copernicus.org/articles/13/1877/2019/ |