A model for polythermal ice incorporating gravity-driven moisture transport

DOI10.1017/jfm.2016.251zbMath1422.86018OpenAlexW2399959875MaRDI QIDQ2973628

C. Schoof, I. J. Hewitt

Publication date: 4 April 2017

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

Full work available at URL: https://semanticscholar.org/paper/ad34d108946ff57434ed0b7393727b0d160bcad7

zbMATH Keywords

porous mediaice sheetssolidification/melting

Mathematics Subject Classification ID

Glaciology (86A40)

Related Items (2)

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Cites Work

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• Introduction to modelling of transport phenomena in porous media
• Flotation and free surface flow in a model for subglacial drainage. Part 1. Distributed drainage
• A mathematical model of polythermal glaciers and ice sheets
• Partial melting in an upwelling mantle column
• Flow in deformable porous media. Part 2 Numerical analysis – the relationship between shock waves and solitary waves
• A continuum–mechanical formulation for shallow polythermal ice sheets
• On the transport of moisture in polythermal glaciers

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