Preprints
https://doi.org/10.5194/egusphere-2026-1845
https://doi.org/10.5194/egusphere-2026-1845
16 Apr 2026
 | 16 Apr 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Mohr–Coulomb yield curves for viscous-plastic sea ice models: flow rules and failure angles

Damien Ringeisen, Bruno Tremblay, Jean-Francois Lemieux, and Martin Losch

Abstract. Viscous-plastic sea ice models typically overestimate the intersection angle between conjugate pairs of Linear Kinematic Features (LKFs) in uni-axial compression tests. These models employ an elliptical yield curve with a normal flow rule. Mohr-Coulomb yield curve formulations can use different plastic potentials (elliptical, teardrop, parabolic lens) implying different flow rule orientations along the limbs of the Mohr-Coulomb yield envelope. The flow rule affects not only the LKFs intersection angle, but also the numerical convergence of the model and the approach to transitions between viscous and plastic states. Some of the proposed Mohr-Coulomb yield curves results in failure angles in the observations 15–30 degree range, which is generally smaller than the ones obtained with the elliptical yield curve with a normal flow rule. The simulated failure angles are best described by Arthur's theory, where both shape of the yield curve and plastic potential influence the orientation of the failure lines. These new Mohr-Coulomb formulations, in particular the Mohr-Coulomb yield curve with elliptical plastic potential with wide ellipse (e < 2) or the Mohr-Coulomb yield curve with the teardrop plastic potential, provide interesting alternatives to the elliptical yield curve for the modeling of LKFs in high-resolution sea ice models, at the cost of a less efficient numerical convergence.

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Damien Ringeisen, Bruno Tremblay, Jean-Francois Lemieux, and Martin Losch

Status: open (until 28 May 2026)

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Damien Ringeisen, Bruno Tremblay, Jean-Francois Lemieux, and Martin Losch

Model code and software

MITgcm: checkpoint67z J.-M. Campin et al. https://doi.org/10.5281/ZENODO.4968496

MITgcm: Mohr-Coulomb rheologies D. Ringeisen et al. https://doi.org/10.5281/zenodo.19361862

Damien Ringeisen, Bruno Tremblay, Jean-Francois Lemieux, and Martin Losch
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Latest update: 16 Apr 2026
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Short summary
Sea ice moves and deforms as wind and ocean currents push it around, creating narrow fracture lines on the surface. To accurately reproduce these fracture patterns in computer models used for climate predictions and navigation, we tested a mathematical approach to sea ice dynamics, common in other fields but rare in sea ice modeling, to see if it could better capture these patterns. Our results show this approach could improve fracture representation, though it requires more computing power.
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