PISM, A Parallel Ice Sheet Model
stable v2.1.1 committed by Constantine Khrulev on 2024-12-04 13:36:58 -0900
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Process model which computes pseudo-plastic yield stress for the subglacial layer. More...
#include "pism/basalstrength/MohrCoulombYieldStress.hh"
#include "pism/basalstrength/MohrCoulombPointwise.hh"
#include "pism/util/Grid.hh"
#include "pism/util/Mask.hh"
#include "pism/util/error_handling.hh"
#include "pism/util/io/File.hh"
#include "pism/util/MaxTimestep.hh"
#include "pism/util/pism_utilities.hh"
#include "pism/util/Time.hh"
#include "pism/util/array/CellType.hh"
#include "pism/util/array/Forcing.hh"
#include "pism/geometry/Geometry.hh"
#include "pism/coupler/util/options.hh"
Go to the source code of this file.
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Process model which computes pseudo-plastic yield stress for the subglacial layer.
The output variable of this submodel is tauc
, the pseudo-plastic yield stress field that is used in the ShallowStressBalance objects. This quantity is computed by the Mohr-Coulomb criterion [SchoofTill], but using an empirical relation between the amount of water in the till and the effective pressure of the overlying glacier resting on the till [Tulaczyketal2000].
The "dry" strength of the till is a state variable which is private to the submodel, namely tillphi
. Its initialization is nontrivial: either the -topg_to_phi
heuristic is used or inverse modeling can be used. (In the latter case tillphi
can be read-in at the beginning of the run. Currently tillphi
does not evolve during the run.)
The effective pressure is derived from the till (pore) water amount (the effective water layer thickness). Then the effective pressure is combined with tillphi to compute an updated tauc
by the Mohr-Coulomb criterion.
This submodel is inactive in floating areas.
Definition in file MohrCoulombYieldStress.cc.