Wave–sea-ice interactions in a brittle rheological framework
نویسندگان
چکیده
Abstract. As sea ice extent decreases in the Arctic, surface ocean waves have more time and space to develop grow, exposing marginal zone (MIZ) frequent energetic wave events. Waves can fragment cover over tens of kilometres, prospect increasing activity has sparked recent interest interactions between wave-induced fragmentation lateral melting. The impact this on dynamics, however, remains mostly unknown, although it is thought that fragmented experiences less resistance deformation than pack ice. Here, we introduce a new coupled framework involving spectral model WAVEWATCH III neXtSIM, which includes Maxwell elasto-brittle rheology. This rheological enables efficiently track keep “memory” level damage. We propose damage increases when occurs. used modelling system investigate potential such local mechanism kinematics. Focusing Barents Sea, found internal stress decrease resulting from its by resulted dynamical MIZ, particularly areas where compact. Sea drift enhanced for both on-ice off-ice wind conditions. Our results importance considering wave–sea-ice forecast applications. They also suggest likely modulate area advected away ocean, potentially contributing observed past, current future decline Arctic.
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ژورنال
عنوان ژورنال: The Cryosphere
سال: 2021
ISSN: ['1994-0424', '1994-0416']
DOI: https://doi.org/10.5194/tc-15-431-2021