Sliding of temperate basal ice on a rough, hard bed: creep mechanisms, pressure melting, and implications for ice streaming

Basal ice motion is crucial to ice dynamics of ice sheets. The classic Weertman model for basal sliding over bedrock obstacles proposes that sliding velocity is controlled by pressure melting and/or ductile flow, whichever is the fastest; it further assumes that pressure melting is limited by heat f...

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Bibliographic Details
Published in:The Cryosphere
Main Author: M. Krabbendam
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-10-1915-2016
https://www.the-cryosphere.net/10/1915/2016/tc-10-1915-2016.pdf
https://doaj.org/article/f0652c4a132542eab4ec64cd8a0ddd35