PISM, A Parallel Ice Sheet Model  stable v2.1-1-g6902d5502 committed by Ed Bueler on 2023-12-20 08:38:27 -0800

◆ fracture_induced_softening()

void pism::stressbalance::SSAFD::fracture_induced_softening ( const array::Scalar fracture_density)
protectedvirtual

Correct vertically-averaged hardness using a parameterization of the fracture-induced softening.

See T. Albrecht, A. Levermann; Fracture-induced softening for large-scale ice dynamics; (2013), The Cryosphere Discussions 7; 4501-4544; DOI:10.5194/tcd-7-4501-2013

Note that this paper proposes an adjustment of the enhancement factor:

\[E_{\text{effective}} = E \cdot (1 - (1-\epsilon) \phi)^{-n}.\]

Let \(E_{\text{effective}} = E\cdot C\), where \(C\) is the factor defined by the formula above.

Recall that the effective viscosity is defined by

\[\nu(D) = \frac12 B D^{(1-n)/(2n)}\]

and the viscosity form of the flow law is

\[\sigma'_{ij} = E_{\text{effective}}^{-\frac1n}2\nu(D) D_{ij}.\]

Then

\[\sigma'_{ij} = E_{\text{effective}}^{-\frac1n}BD^{(1-n)/(2n)}D_{ij}.\]

Using the fact that \(E_{\text{effective}} = E\cdot C\), this can be rewritten as

\[\sigma'_{ij} = E^{-\frac1n} \left(C^{-\frac1n}B\right) D^{(1-n)/(2n)}D_{ij}.\]

So scaling the enhancement factor by \(C\) is equivalent to scaling ice hardness \(B\) by \(C^{-\frac1n}\).

Definition at line 1363 of file SSAFD.cc.

References pism::Component::m_config, pism::stressbalance::ShallowStressBalance::m_flow_law, pism::Component::m_grid, m_hardness, and phi.

Referenced by compute_hardav_staggered().