Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-1339-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-1339-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
A Maxwell elasto-brittle rheology for sea ice modelling
Véronique Dansereau
CORRESPONDING AUTHOR
Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS UMR 5183, Université de Grenoble, Grenoble, France
Jérôme Weiss
Institut des Sciences de la Terre, CNRS UMR 5275, Université de Grenoble, Grenoble, France
Pierre Saramito
Laboratoire Jean Kuntzmann, CNRS UMR 5224, Université de Grenoble, Grenoble, France
Philippe Lattes
TOTAL S.A. – DGEP/DEV/TEC/GEO, Paris, France
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74 citations as recorded by crossref.
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- Scaling Properties of Arctic Sea Ice Deformation in a High‐Resolution Viscous‐Plastic Sea Ice Model and in Satellite Observations N. Hutter et al. 10.1002/2017JC013119
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- Calving glaciers and ice shelves D. Benn & J. Åström 10.1080/23746149.2018.1513819
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- A New Brittle Rheology and Numerical Framework for Large‐Scale Sea‐Ice Models E. Ólason et al. 10.1029/2021MS002685
- Sea ice floe size: its impact on pan-Arctic and local ice mass and required model complexity A. Bateson et al. 10.5194/tc-16-2565-2022
- Comparison of sea ice kinematics at different resolutions modeled with a grid hierarchy in the Community Earth System Model (version 1.2.1) S. Xu et al. 10.5194/gmd-14-603-2021
- Data-driven surrogate modeling of high-resolution sea-ice thickness in the Arctic C. Durand et al. 10.5194/tc-18-1791-2024
- Improving Numerical Accuracy for the Viscous-Plastic Formulation of Sea Ice T. Li et al. 10.2139/ssrn.4158387
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1 citations as recorded by crossref.
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Latest update: 14 Dec 2024
Short summary
In this paper we present a new mechanical modelling framework for the deformation of sea ice on regional and larger scales named Maxwell elasto-brittle. The model successfully reproduces the formation of narrow, oriented leads which concentrate the deformation within the damaged, i.e., fractured, ice as well as the intermittency of the damaging process, and hence represents a relevant contribution to the ongoing development of operational modelling platforms, regional and global climate models.
In this paper we present a new mechanical modelling framework for the deformation of sea ice on...