Hamiltonian form and solitary waves of the spatial Dysthe equations
Abstract
The spatial Dysthe equations describe the envelope evolution of the free-surface and potential of gravity waves in deep waters. Their Hamiltonian structure and new invariants are unveiled by means of a gauge transformation to a new canonical form of the evolution equations. An accurate Fourier-type spectral scheme is used to solve for the wave dynamics and validate the new conservation laws, which are satisfied up to machine precision. Traveling waves are numerically constructed using the Petviashvili method. It is shown that their collision appears inelastic, suggesting the non-integrability of the Dysthe equations.
Domains
Fluid mechanics [physics.class-ph] Fluids mechanics [physics.class-ph] Atmospheric and Oceanic Physics [physics.ao-ph] Exactly Solvable and Integrable Systems [nlin.SI] Computational Physics [physics.comp-ph] Fluid Dynamics [physics.flu-dyn] Numerical Analysis [math.NA] Analysis of PDEs [math.AP]
Origin : Files produced by the author(s)
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