Flotation and free surface flow in a model for subglacial drainage. Part 2. Channel flow

Flotation and free surface flow in a model for subglacial drainage. Part 2. Channel flow

We present a new model of subglacial drainage incorporating flow in a network of channels and a porous sheet, with water exchange between the two determined by pressure gradients. The sheet represents the average effect of many linked cavities, whilst the channels emerge from individual cavities tha...

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Bibliographic Details
Main Authors:	Hewitt, I, Schoof, C, Werder, M
Format:	Journal article
Language:	English
Published:	2012

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