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Problems
The aim of this Section is to describe which solvers and user functions can be used to solve a given type of glaciological problems.
Elmer/Ice capabilities are listed below:
Full-Stokes equation but also
SIA,
SSA, Diagnostic or transient
Various
rheology (Glen’s law, firn/snow and two anisotropic flow laws)
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Evolution equations for density,
fabric, …
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Evaluation of the eigenvalues and eigenvectors of a tensor (strain-rate, stress)
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Inverse methods (linear adjoint and Arthern and Gudmundsson's 2010 methods)
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Highly parallel Stokes solver