Titlebook: Waves and Nonlinear Processes in Hydrodynamics; John Grue,Bjørn Gjevik,Jan Erik Weber Book 1996 Kluwer Academic Publishers 1996 Ocean.Scal

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On the Motion of a Rigid Body in Non-Uniform Flowsts; one of a potential type and the other is of a “magnetic” type (i.e., a force proportional to the body’s six velocities which produces .). Note further that there exist certain connections between the magnetic-type forces and the rotating coordinate system, the nature of which lie in the fact tha

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Interaction Between Waves and Slowly Rotating Floating Bodiesng part, being exposed to the wind and wave environment at the sea-surface, and by moorings or tendons for positioning. The system may experience slowly varying oscillations in the horizontal plane at the relatively low natural frequencies of the horizontal modes of motion. These oscillations are de

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Continuous Bores on a Viscous Fluid Down an Inclineng 1994 for a survey). Motivated by interests in chemical engineering, surface tension is emphasized in past studies where the Weber number W. is ususally assumed to be large W. = .(∈.) where ∈ = is a small parameter denoting the depth-to-wavelength ratio. Among the few papers on high Reynolds numbe

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Refraction of Solitons and Wave Jumpsharacteristics without substantial disintegration or loss of identity. A standard example is refraction of linear sinusoidal surface waves due to changes in bathymetry or current. Also a few classes of nonlinear waves display similar behaviour; like Stokes waves (Peregrine 1983), shocks (Whitham 197

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Effect of Film Elasticity on Drift Currents Induced by Growing Wavesys an important role for determining the damping characteristics (Dorrestein 1951). Furthermore, film elasticity affects the wind’s ability to generate such waves (Gottifredi and Jameson 1968; Creamer and Wright 1992). The film elasticity has also a profound influence on the nonlinear development of

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Finite Elements for the Boussinesq Wave Equationsing. The standard simulation models in this field are based on the linear hydrostatic wave equations solved by finite difference methods (Mesinger and Arakawa, 1976; Abott, Petersen and Skovgaard, 1978). In recent years the models have been extended to include also nonlinear and weakly dispersive ef