Steady radial ice-sheet flow with fabric evolution

Reorientation of individual crystal glide planes, as isotropic surface ice is deformed during its passage to depth in an ice sheet, creates a fabric and associated anisotropy. We adopt an evolving orthotropic viscous law which was developed to reflect the induced anisotropy arising from the mean rot...

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Bibliographic Details
Published inJournal of glaciology Vol. 52; no. 177; pp. 267 - 280
Main Authors Morland, Leslie W., Staroszczyk, Ryszard
Format Journal Article
LanguageEnglish
Published Cambridge, UK Cambridge University Press 2006
International Glaciological Society
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