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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Published in | Journal of glaciology Vol. 52; no. 177; pp. 267 - 280 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Cambridge, UK
Cambridge University Press
2006
International Glaciological Society |
Subjects | |
Online Access | Get full text |
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