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
Main Authors: Pierce Hunter, Colin Meyer, Brent Minchew, Marianne Haseloff, Alan Rempel
Format: Article
Language:English
Published: Cambridge University Press 2021-06-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143020001185/type/journal_article

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