Preprints
https://doi.org/10.5194/egusphere-2026-4686
https://doi.org/10.5194/egusphere-2026-4686
26 Oct 2026
 | 26 Oct 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Nonlocal ice strength regularization of the Viscous-Plastic sea ice rheology: resolving ill-posedness and resolution-dependent fracture patterns

Félix St-Denis and L. Bruno Tremblay

Abstract. We implement a nonlocal ice strength regularization in the standard Viscous-Plastic (VP) and Elastic-Viscous-Plastic (EVP) models. To this end, we introduce an inhomogeneous Helmholtz equation for the ice strength that provides a physically based regularization of the ill-posed VP and EVP formulations while preserving the rate-independence of the plastic regime and the material instabilities that give rise to narrow deformation bands. A linear stability analysis of the new system of equations shows that the nonlocal regularization imposes an upper bound on the growth rates of perturbations, a necessary condition for well-posed problems. Those results are confirmed in idealized divergent numerical experiments: the standard (E)VP models yield resolution-dependent solutions with an increasing number of fractures as the spatial resolution is increased, whereas the nonlocal models produce a resolution-independent solution with a single fracture at the center of the ice plate. Numerical experiments demonstrating the ill-posedness of the hyperbolic tangent viscosity regularization previously identified through a linear stability analysis are also presented. With the advent of kilometer-scale sea ice simulations (Δx ≤ 2–3 km), a well-posed rheology is essential to ensure that fracture statistics reflect physical deformation processes rather than numerical instabilities.

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Félix St-Denis and L. Bruno Tremblay

Status: open (until 07 Dec 2026)

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Félix St-Denis and L. Bruno Tremblay

Model code and software

McGill 1D-SIM: model and analysis Félix St-Denis https://doi.org/10.5281/zenodo.21771392

Félix St-Denis and L. Bruno Tremblay
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Latest update: 26 Oct 2026
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Short summary
As the spatial resolution of sea ice models reaches the kilometer scale, it is necessary to ensure that the simulated fracture lines are not resolution-dependent and stem from the physics rather than the numerics. To this end, we implemented an approach such that the ice strength also depends on neighboring points rather than only one in two widely used sea ice models. Through idealised mathematical and numerical experiments, we show that this approach produces resolution-independent fractures.
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