Consistent approximations and boundary conditions for ice-sheet dynamics from a principle of least action
The formulation of a physical problem in terms of a variational (or action) principle conveys significant advantages for the analytical formulation and numerical solution of that problem. One such problem is ice-sheet dynamics as described by non-Newtonian Stokes flow, for which the variational prin...
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Veröffentlicht in: | Journal of glaciology 2010-01, Vol.56 (197), p.480-496 |
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Sprache: | eng |
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