  A modified version of the wave-ice interaction model proposed by Williams et
al (2013a,b) is presented for an idealised transect geometry. Wave attenuation
due to ice floes and wave-induced ice fracture are both included in the
wave-ice interaction model. Subgrid spatial and temporal discretisations are
not required in the modified version of the model, thereby facilitating its
future integration into large-scaled coupled models. Results produced by the
new model are compared to results produced by the original model of Williams et
al (2013b).
