Fourth order nonlinear evolution equations are derived for two counter-propagating surface gravity wave packets in deep water in the presence of wind flowing over water. The resulting equations are asymptotically exact and nonlocal. Stability analysis is made for a uniform standing surface gravity wave train for longitudinal perturbation on the basis of these equations. Graphs are plotted for maximum growth rate of instability and for wave number at marginal stability against wave steepness for some different values of dimensionless wind velocity. Significant deviations are noticed between the results obtained from third order and fourth order nonlinear evolution equations. This paper has an application in rough waves. References ...
A new singular-perturbation method is introduced for the solution of multiple-scale problems. The us...
AbstractThis paper deals with the two- and three-dimensional nonlinear water waves generated by a st...
In this thesis we study nonlinear and breaking deep-water surface waves. First, we consider the vort...
For a three-dimensional gravity capillary wave packet in the presence of a thin thermocline in deep ...
Fourth order nonlinear evolution equations, which are a good starting point for the study of nonline...
A fourth order nonlinear evolution equation, which is a good starting point for the study of nonline...
A nonlinear spectral transport equation for the narrow band Gaussian random surface wave trains is d...
The effect of randomness on the stability of deep water surface gravity waves in the presence of a t...
We extend the evolution equation for weak nonlinear gravity–capillary waves by including fifth-ord...
A new nonlinear Schrödinger equation (NLSE) is presented for ocean surface waves. Earlier derivation...
Nonlinear initial-boundary value problem on deep-water gravity waves of finite amplitude is solved a...
In this work we develop nonlinear models to study the propagation of surface water waves.The Nonline...
A nonlinear Schrödinger equation for the envelope of two-dimensional gravity-capillary waves propaga...
A review of three-dimensional waves on deep-water is presented. Three forms of three-dimensionality,...
The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings bet...
A new singular-perturbation method is introduced for the solution of multiple-scale problems. The us...
AbstractThis paper deals with the two- and three-dimensional nonlinear water waves generated by a st...
In this thesis we study nonlinear and breaking deep-water surface waves. First, we consider the vort...
For a three-dimensional gravity capillary wave packet in the presence of a thin thermocline in deep ...
Fourth order nonlinear evolution equations, which are a good starting point for the study of nonline...
A fourth order nonlinear evolution equation, which is a good starting point for the study of nonline...
A nonlinear spectral transport equation for the narrow band Gaussian random surface wave trains is d...
The effect of randomness on the stability of deep water surface gravity waves in the presence of a t...
We extend the evolution equation for weak nonlinear gravity–capillary waves by including fifth-ord...
A new nonlinear Schrödinger equation (NLSE) is presented for ocean surface waves. Earlier derivation...
Nonlinear initial-boundary value problem on deep-water gravity waves of finite amplitude is solved a...
In this work we develop nonlinear models to study the propagation of surface water waves.The Nonline...
A nonlinear Schrödinger equation for the envelope of two-dimensional gravity-capillary waves propaga...
A review of three-dimensional waves on deep-water is presented. Three forms of three-dimensionality,...
The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings bet...
A new singular-perturbation method is introduced for the solution of multiple-scale problems. The us...
AbstractThis paper deals with the two- and three-dimensional nonlinear water waves generated by a st...
In this thesis we study nonlinear and breaking deep-water surface waves. First, we consider the vort...