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Modelling the brittle to granular transition in sea ice

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SIPW05 - SIP Follow on: Mathematics of sea ice in the twenty-first century

The thin ice covering the polar oceans is a complex geomaterial that experiences rheological transitions between a brittle solid state, such as in the pack, and a dense or loose granular regime, such as in active shear zones or the MIZ . This talk will present some ongoing work that aims to improve both the physical and numerical representation of these transitions in the framework of a continuum, elasto-viscous-brittle model. 

This talk is part of the Isaac Newton Institute Seminar Series series.

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