Articles | Volume 8, issue 2
https://doi.org/10.5194/tc-8-721-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.Adjoint accuracy for the full Stokes ice flow model: limits to the transmission of basal friction variability to the surface
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2020Cited articles
Amestoy, P. R., Duff, I. S., L'Excellent, J.-Y., and Koster, J.: A Fully Asynchronous Multifrontal Solver Using Distributed Dynamic Scheduling, SIAM Journal on Matrix Analysis and Applications, 23, 15–41, 2001.
Balise, M. J. and Raymond, C. F.: Transfer of basal sliding variations to the surface of a linearly viscous glacier, J. Glaciol., 31, 308–318, 1985.
Christianson, B.: Reverse accumulation and attractive fixed points, Optimization Methods and Software, 3, 311–326, 1994.
Cuffey, K. M. and Paterson, W. S. B.: The Physics of Glaciers, Academic Press, 2010.
DassFlow Software: Data assimilation for free-surface Flows, open source freeware, http://www-gmm.insa-toulouse.fr/ monnier/DassFlow, 2007.