Thermal controls on ice stream shear margins
Ice stream discharge responds to a balance between gravity, basal friction and lateral drag. Appreciable viscous heating occurs in shear margins between ice streams and adjacent slow-moving ice ridges, altering the temperature-dependent viscosity distribution that connects lateral drag to marginal s...
Published in: | Journal of Glaciology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
2021
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Subjects: | |
Online Access: | https://nrl.northumbria.ac.uk/id/eprint/45464/ https://doi.org/10.1017/jog.2020.118 https://nrl.northumbria.ac.uk/id/eprint/45464/9/thermal-controls-on-ice-stream-shear-margins.pdf https://nrl.northumbria.ac.uk/id/eprint/45464/1/thermal-controls-on-ice-stream-shear-margins.pdf |