Thermally driven migration of ice-stream shear margins

DOI10.1017/JFM.2012.438zbMath1275.76211OpenAlexW2096728111MaRDI QIDQ2863496

C. Schoof

Publication date: 21 November 2013

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://semanticscholar.org/paper/46c998168a2fb06e78c1610261fe204521536893

zbMATH Keywords

contact linesice sheetssolidification/melting

Mathematics Subject Classification ID

Stefan problems, phase changes, etc. (80A22) Multiphase and multicomponent flows (76T99) Glaciology (86A40)

Related Items (2)

Ice sheet flow with thermally activated sliding. Part 1: the role of advection ⋮ A boundary layer model for ice stream margins

Cites Work

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• Existence of weak solutions to a system of nonlinear partial differential equations modelling ice streams
• On the distribution of stress and velocity in an ice strip, which is partly sliding over and partly adhering to its bed, by using a Newtonian viscous approximation
• A variational approach to ice stream flow

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