On the Hamiltonian structure of the planar steady water-wave problem with vorticity

2014 ◽  
Vol 352 (3) ◽  
pp. 205-211 ◽  
Author(s):  
Mark D. Groves ◽  
Athanasios Stylianou

Travelling waves and relative equilibrium states of infinite dimensional hamiltonian systems are considered with particular attention to the water-wave problem. Relative equilibria correspond to solutions that are stationary in a moving frame of reference. The governing equations for relative equilibria are recast as a hamiltonian evolution equation in space. The mass, momentum and energy flux densities play a fundamental role in the spatial hamiltonian structure: the energy flux generates the basic symplectic operator, the momentum flux is the spatial hamiltonian and the mass flux is a second independent (spatial) integral. A complete theory is given for the water-wave problem with surface tension. The hamiltonian structure is used to show the existence of dual variational principles for travelling waves and to give an analysis of a singularity in the dispersion relation for capillary-gravity waves from a spatial hamiltonian systems viewpoint.


Author(s):  
Biswajit Basu ◽  
Calin I. Martin

AbstractWe are concerned here with an analysis of the nonlinear irrotational gravity water wave problem with a free surface over a water flow bounded below by a flat bed. We employ a new formulation involving an expression (called flow force) which contains pressure terms, thus having the potential to handle intricate surface dynamic boundary conditions. The proposed formulation neither requires the graph assumption of the free surface nor does require the absence of stagnation points. By way of this alternative approach we prove the existence of a local curve of solutions to the water wave problem with fixed flow force and more relaxed assumptions.


It is shown in general that the exact solution to every non-degenerate unsteady water-wave problem in a straight channel inclined at arbitrary slope, governed by the non-linear hydraulic equations, can be obtained in terms of the complete elliptic integral of the second kind, E . By means of a non-Newtonian reference frame, every such wave problem for a sloping channel can be replaced by an associated problem for a horizontal channel. For the latter, the partial differential equations become reducible and thus permit hodograph inversion. The Riemann integration method for the resulting Euler-Poisson equation yields an auxiliary function for these hydraulic problems which is transformable into a Legendre function and then into the elliptic integral. In particular, the procedure is applied to obtain the exact solution for the water wave in a sloping channel produced by sudden release of the triangular wedge of water (the reservoir) initially at rest behind a vertical wall. The behaviour of the solution is exhibited for convenience in two level-line charts, and representative wave profiles and velocity distributions are presented.


Author(s):  
Tatsuo Iguchi

In numerical computations of tsunamis due to submarine earthquakes, it is frequently assumed that the initial displacement of the water surface is equal to the permanent shift of the seabed and that the initial velocity field is equal to zero and the shallow-water equations are often used to simulate the propagation of tsunamis. We give a mathematically rigorous justification of this tsunami model starting from the full water-wave problem by comparing the solution of the full problem with that of the tsunami model. We also show that, in some cases, we have to impose a non-zero initial velocity field, which arises as a nonlinear effect.


Wave Motion ◽  
1994 ◽  
Vol 19 (4) ◽  
pp. 367-389 ◽  
Author(s):  
Walter Craig ◽  
Mark D. Groves

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