A three-dimensional model of wave attenuation in the marginal ice zone

A three‐dimensional model of wave scattering by a large array of floating thin elastic plates is used to predict the rate of ocean wave attenuation in the marginal ice zone in terms of the properties of the ice cover and the incoming wavefield. This is regarded as a small step toward assimilating in...

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Veröffentlicht in:Journal of Geophysical Research: Oceans 2010-12, Vol.115 (C12), p.n/a
Hauptverfasser: Bennetts, L. G., Peter, M. A., Squire, V. A., Meylan, M. H.
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Sprache:eng
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