Titlebook: Numerical Modeling of Sea Waves; Dmitry V. Chalikov Book 2016 Springer International Publishing Switzerland 2016 Benjamin-Feir instability

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Three-Dimensional Modeling of Potential Waves,scheme is based on the surface-following non-orthogonal curvilinear coordinate system. Velocity potential is represented as a sum of analytical and nonlinear components. The Poisson equation for the nonlinear component of velocity potential is solved iteratively. Fourier transform method, the second

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e of linear equations of motion which, in the tight-binding representation, define continuous random networks within the space occupied by the material. We then turn to macroscopically disordered materials and, using porous rocks as an example, introduce certain relevant topological concepts. In par

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Dmitry V. Chalikovby Frank [222]. In most text books and scientific papers the Vavilov-Cherenkov effect is considered in terms of Fourier components. To obtain an answer in physical space the inverse Fourier transform should be performed. The divergent integrals which occur obscure the physical picture. As far as we

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