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~~NOTOC~~
===== Basal Hydrology models =====
There is two basal hydrology models implemented right now in Elmer/Ice.
==== Double Continuum Equivalent Hydrological Model ====
=== General Description ====
The model consist of two solvers, one is used for the inefficient drainage system ([[:solvers:idssolver|IDSSolver]]) and the other one for the efficient drainage system ([[:solvers:eplsolver|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 using the
[[userfunctions:watertransfer|WaterTransfer user function]].
=== 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. & RÃ¥back, P. A double continuum hydrological model for glacier applications The Cryosphere, 2014, 8, 137-153
==== GlaDS model (Werder et al., 2013) ====
=== General Description ====
The model consists of three solvers described on [[solvers:glads|this page]]. User functions will be made available for the coupling with ice flow (Stokes or SSA).