Add to ORKGConditions are found for the appearance of non-uniform progressive waves of permanent form from a long-wave modulation of a finite-amplitude Stokes wave on deep water. The waveheight at which the modulated waves can occur is a very slowly decreasing function of the modulation wavelength for values up to 150 times the original wavelength. Some qualitative remarks are made about the problem of determining the stability of the new waves
Numerical solutions of the inviscid equations that describe standing waves of finite amplitude on de...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
A new class of three-dimensional, deep-water gravity waves of permanent form has been found using an...
Nonlinear periodic gravity waves propagating at a constant velocity at the surface of a fluid of inf...
Two different numerical methods are used to demonstrate the existence of and calculate non-symmetric...
Two different numerical methods are used to demonstrate the existence of and calculate non-symmetric...
Steady three-dimensional symmetric wave patterns for finite-amplitude gravity waves on deep water ar...
Steady three-dimensional symmetric wave patterns for finite-amplitude gravity waves on deep water ar...
Plane progressive waves on water of finite or infinite depth are treated under the effect of both gr...
A combination and modification of two existing methods, which involves balancing static and dynamic ...
A weakly nonlinear Hamiltonian model for two-dimensional irrotational waves on water of finite depth...
This paper concerns the description of large transient waves in shallow and intermediate water depth...
A weakly nonlinear Hamiltonian model for two-dimensional irrotational waves on water of finite depth...
A linear stability analysis of finite-amplitude periodic progressive gravity waves on water of finit...
Numerical solutions of the inviscid equations that describe standing waves of finite amplitude on de...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
A new class of three-dimensional, deep-water gravity waves of permanent form has been found using an...
Nonlinear periodic gravity waves propagating at a constant velocity at the surface of a fluid of inf...
Two different numerical methods are used to demonstrate the existence of and calculate non-symmetric...
Two different numerical methods are used to demonstrate the existence of and calculate non-symmetric...
Steady three-dimensional symmetric wave patterns for finite-amplitude gravity waves on deep water ar...
Steady three-dimensional symmetric wave patterns for finite-amplitude gravity waves on deep water ar...
Plane progressive waves on water of finite or infinite depth are treated under the effect of both gr...
A combination and modification of two existing methods, which involves balancing static and dynamic ...
A weakly nonlinear Hamiltonian model for two-dimensional irrotational waves on water of finite depth...
This paper concerns the description of large transient waves in shallow and intermediate water depth...
A weakly nonlinear Hamiltonian model for two-dimensional irrotational waves on water of finite depth...
A linear stability analysis of finite-amplitude periodic progressive gravity waves on water of finit...
Numerical solutions of the inviscid equations that describe standing waves of finite amplitude on de...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...