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solvers:hydrologydc [Elmer/Ice Wiki]

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Double Continuum Equivalent Hydrological Model

General Description

The model consist of two solvers, one is used for the inefficient drainage system (IDSSolver) and the other one for the efficient drainage system (EPLSolver). Each compute the water head by mean of a diffusion equation based on Darcy's law. The two can be coupled by a transfer equation (a UserFunction is associated for this purpose)

Example

Two basic tests can be found in [ELMER_TRUNK]/elmerice/Tests/Hydro_SedOnly and [ELMER_TRUNK]/elmerice/Tests/Hydro_Coupled.

Reference

When used this solver can be cited using the following reference :
de Fleurian, B.; Gagliardini, O.; Zwinger, T.; Durand, G.; Le Meur, E.; Mair, D. & Råback, P. A double continuum hydrological model for glacier applications The Cryosphere, 2014, 8, 137-153

solvers/hydrologydc.1448361459.txt.gz · Last modified: 2015/11/24 10:37 by gag
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