Research highlights

Three-dimensional imaging of ocean waves in the Antarctic marginal ice zone during an explosive polar cyclone (Alberello et al, Nat Comms, 2022)
Change in complex-resonant frequencies (white bullets) caused by increasing ice-shelf thickening. Background is a representation of complex-valued reflection coefficient in complex frequency space (Bennetts & Meylan, SIAM J Appl Math, 2021).
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Fastest measured ice drift speed (0.75m/s), for a pancake floe in the Antarctic marginal ice zone during a series of polar cyclones (Alberello et al, J Geophy Res, 2019)
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A graded resonator array that amplifies incident water waves at selected locations (Bennetts et al., J Fluid Mech, 2018)
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A theoretical model of water wave overwash of a step (green) vs a CFD model (Skene et al, J Fluid Mech, 2018)