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...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Hunter, Pierce, Meyer, Colin, Minchew, Brent, Haseloff, Marianne, Rempel, Alan
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
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