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A modified version of the wave-ice interaction model proposed by Williams etal (2013a,b) is presented for an idealised transect geometry. Wave attenuationdue to ice floes and wave-induced ice fracture are both included in thewave-ice interaction model. Subgrid spatial and temporal discretisations arenot required in the modified version of the model, thereby facilitating itsfuture integration into large-scaled coupled models. Results produced by thenew model are compared to results produced by the original model of Williams etal (2013b).

An idealised wave-ice interaction model without subgrid spatial and temporal discretisations