On the steady-state fully resonant progressive waves in water of finite depth

Abstract The steady-state fully resonant wave system, consisting of two progressive primary waves in finite water depth and all components due to nonlinear interaction, is investigated in detail by means of analytically solving the fully nonlinear wave equations as a nonlinear boundary-value problem. It is found that multiple steady-state fully resonant waves exist in some cases which have no exchange of wave energy at all, so that the energy spectrum is time-independent. Further, the steady-state resonant wave component may contain only a small proportion of the wave energy. However, even in these cases, there usually exist time-dependent periodic exchanges of wave energy around the time-independent energy spectrum corresponding to such a steady-state fully resonant wave, since it is hard to be exactly in such a balanced state in practice. This view serves to deepen and enrich our understanding of the resonance of gravity waves.

[1]  M. Longuet-Higgins,et al.  An experiment on third-order resonant wave interactions , 1966, Journal of Fluid Mechanics.

[2]  O. M. Phillips,et al.  Wave interactions - the evolution of an idea , 1981, Journal of Fluid Mechanics.

[3]  Lev Shemer,et al.  On modifications of the Zakharov equation for surface gravity waves , 1984, Journal of Fluid Mechanics.

[4]  S. Liao,et al.  Beyond Perturbation: Introduction to the Homotopy Analysis Method , 2003 .

[5]  O. Phillips On the dynamics of unsteady gravity waves of finite amplitude Part 1. The elementary interactions , 1960, Journal of Fluid Mechanics.

[6]  M. Stiassnie,et al.  On Zakharov's kernel and the interaction of non-collinear wavetrains in finite water depth , 2009, Journal of Fluid Mechanics.

[7]  N. E. Huang,et al.  Measurements of third-order resonant wave interactions , 1966 .

[8]  Shijun Liao,et al.  Homotopy Analysis Method in Nonlinear Differential Equations , 2012 .

[9]  Shijun Liao On the homotopy multiple-variable method and its applications in the interactions of nonlinear gravity waves , 2011 .

[10]  Chris Swan,et al.  The evolution of large non-breaking waves in intermediate and shallow water. I. Numerical calculations of uni-directional seas , 2011, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[11]  G. Whitham Mass, momentum and energy flux in water waves , 1962, Journal of Fluid Mechanics.

[12]  A. Osborne,et al.  Four-wave resonant interactions in the classical quadratic Boussinesq equations , 2009, Journal of Fluid Mechanics.

[13]  Francis P. Bretherton,et al.  Resonant interactions between waves. The case of discrete oscillations , 1964, Journal of Fluid Mechanics.

[14]  G. T. Csanady,et al.  Wave interactions and fluid flows , 1987 .

[15]  D. Yue,et al.  Theory and applications of ocean surface waves. Part 2: nonlinear aspects , 2005 .

[16]  M. Longuet-Higgins,et al.  Resonant interactions between two trains of gravity waves , 1962, Journal of Fluid Mechanics.

[17]  Per A. Madsen,et al.  Third-order theory for multi-directional irregular waves , 2012, Journal of Fluid Mechanics.

[18]  K. Stewartson,et al.  On three-dimensional packets of surface waves , 1974, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

[19]  D. J. Benney Non-linear gravity wave interactions , 1962, Journal of Fluid Mechanics.

[20]  Vladimir E. Zakharov,et al.  Stability of periodic waves of finite amplitude on the surface of a deep fluid , 1968 .

[21]  S. Liao An optimal homotopy-analysis approach for strongly nonlinear differential equations , 2010 .

[22]  S. Liao A uniformly valid analytic solution of two-dimensional viscous flow over a semi-infinite flat plate , 1999, Journal of Fluid Mechanics.