Ice-Shelf Flexure and Tidal Forcing of Bindschadler Ice Stream, West Antarctica
Viscoelastic models of ice-shelf flexure and ice-stream velocity perturbations are combined into a single efficient flowline model to study tidal forcing of grounded ice. The magnitude and timing of icestream response to tidally driven changes in hydrostatic pressure and/or basal drag are found to d...
Main Authors: | , , , , |
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Format: | Other/Unknown Material |
Language: | unknown |
Published: |
2014
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Subjects: | |
Online Access: | http://hdl.handle.net/2060/20140010302 |