A theoretical model describing the propagation of gravity waves on ice-covered waters is developed. The ice-water system is approximated as a two-layer viscous and immiscible Newtonian fluid. The model is validated against existing viscous models by using laboratory and in situ collected wave data.
Dispersion and attenuation of gravity waves in ice: a two-layer viscous fluid model with experimental data validation
De Carolis G;
2002
Abstract
A theoretical model describing the propagation of gravity waves on ice-covered waters is developed. The ice-water system is approximated as a two-layer viscous and immiscible Newtonian fluid. The model is validated against existing viscous models by using laboratory and in situ collected wave data.File in questo prodotto:
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