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Wave–sea-ice interactions in a brittle rheological framework ArchiMer
Boutin, Guillaume; Williams, Timothy; Rampal, Pierre; Olason, Einar; Lique, Camille.
As sea ice extent decreases in the Arctic, surface ocean waves have more time and space to develop and grow, exposing the marginal ice zone (MIZ) to more frequent and more energetic wave events. Waves can fragment the ice cover over tens of kilometres, and the prospect of increasing wave activity has sparked recent interest in the interactions between wave-induced sea ice fragmentation and lateral melting. The impact of this fragmentation on sea ice dynamics, however, remains mostly unknown, although it is thought that fragmented sea ice experiences less resistance to deformation than pack ice. Here, we introduce a new coupled framework involving the spectral wave model WAVEWATCH III and the sea ice model neXtSIM, which includes a Maxwell elasto-brittle...
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Ano: 2021 URL: https://archimer.ifremer.fr/doc/00679/79084/81534.pdf
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