Gravity waves propagating into an ice-covered ocean: A viscoelastic model

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Wave-ice interactions in the marginal ice zone. Part 1: Theoretical foundations (2013, background): “In viscous models (e.g. Weber, 1987; Keller, 1998; Wang and Shen, 2011a) wave energy is lost to viscous dissipation, so these models are essentially independent of the FSD.”