An idealized wave-ice interaction model without subgrid spatial or temporal discretizations

A new numerical implementation is proposed for a wave–ice interaction model. It is applied to an idealized transect geometry. Wave attenuation due to ice floes and wave-induced ice fracture are both included in the model. The new method alleviates the need for subgrid spatial or temporal discretizat...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Bennetts, L., O'Farrell, S., Uotila, P., Squire, V.
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2015
Subjects:
Online Access:http://hdl.handle.net/2440/95708
https://doi.org/10.3189/2015AoG69A599
Description
Summary:A new numerical implementation is proposed for a wave–ice interaction model. It is applied to an idealized transect geometry. Wave attenuation due to ice floes and wave-induced ice fracture are both included in the model. The new method alleviates the need for subgrid spatial or temporal discretizations, thereby facilitating future integration of wave–ice interactions into large-scale coupled models. Luke G. Bennetts, Siobhan O, Farrell, Petteri Uotila, Vernon A. Squire