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An experimental model of transmission of ocean waves by an ice floe ispresented. Thin plastic plates with different material properties andthicknesses are used to model the floe. Regular incident waves with differentperiods and steepnesses are used, ranging from gently-sloping to storm-likeconditions. A wave gauge is used to measure the water surface elevation in thelee of the floe. The depth of wave overwash on the floe is measured by a gaugein the centre of the floe's upper surface. Results show transmitted waves areregular for gently-sloping incident waves but irregular for storm-like incidentwaves. The proportion of the incident wave transmitted is shown to decrease asincident wave steepness increases, and to be at its minimum for an incidentwavelength equal to the floe length. Further, a trend is noted for transmissionto decrease as the mean wave height in the overwash region increases.

An idealised experimental model of ocean surface wave transmission by an ice floe