Parameter and state estimation with a time-dependent adjoint marine ice sheet model
To date, assimilation of observations into large-scale ice models has consisted predominantly of time-independent inversions of surface velocities for basal traction, bed elevation, or ice stiffness, and has relied primarily on analytically derived adjoints of glaciological stress balance models. To...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2013-11-01
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Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/7/1659/2013/tc-7-1659-2013.pdf |