LaTex file, 16 pages, 4 figuresIn the limit of small values of the aspect ratio parameter (or wave steepness) which measures the amplitude of a surface wave in units of its wave-length, a model equation is derived from the Euler system in infinite depth (deep water) without potential flow assumption. The resulting equation is shown to sustain periodic waves which on the one side tend to the proper linear limit at small amplitudes, on the other side possess a threshold amplitude where wave crest peaking is achieved. An explicit expression of the crest angle at wave breaking is found in terms of the wave velocity. By numerical simulations, stable soliton-like solutions (experiencing elastic interactions) propagate in a given velocities range ...
Why do ocean waves break? Understanding this important and obvious property of the ocean surface has...
A curious feature of the ordinary linear theory of irregular waves is that the particle trajectories...
Ocean waves forced by the wind are multidirectional, even if the wind direction is steady. Direction...
In the limit of small values of the aspect ratio parameter (or wave steepness) which measures the am...
Short-crested waves are defined as propagating surface gravity waves which are doubly-periodic in th...
The highest standing surface wave at infinite depth is a classical hydrodynamic problem, illuminated...
Short-crested waves are three-dimensional waves that may be generated through a reflection of a two-...
In the oceanographic literature, short-crestedness of waves is often assumed to be the same feature ...
In order to describe the dynamics of monochromatic surface waves in deep water, we derive a nonlinea...
International audienceShort-crested waves are three-dimensional waves that may be generated through ...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
Most of the studies on the kinematics and dynamics of surface waves were focused for years on two-di...
In this paper, we study the critical ratio between the amplitudes of two overtaking solitary waves o...
Numerical calculations of the resonant interactions of three-dimensional short-crested waves very ne...
The breaking of waves is an important mechanism for a number of physical, chemical and biological pr...
Why do ocean waves break? Understanding this important and obvious property of the ocean surface has...
A curious feature of the ordinary linear theory of irregular waves is that the particle trajectories...
Ocean waves forced by the wind are multidirectional, even if the wind direction is steady. Direction...
In the limit of small values of the aspect ratio parameter (or wave steepness) which measures the am...
Short-crested waves are defined as propagating surface gravity waves which are doubly-periodic in th...
The highest standing surface wave at infinite depth is a classical hydrodynamic problem, illuminated...
Short-crested waves are three-dimensional waves that may be generated through a reflection of a two-...
In the oceanographic literature, short-crestedness of waves is often assumed to be the same feature ...
In order to describe the dynamics of monochromatic surface waves in deep water, we derive a nonlinea...
International audienceShort-crested waves are three-dimensional waves that may be generated through ...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
Most of the studies on the kinematics and dynamics of surface waves were focused for years on two-di...
In this paper, we study the critical ratio between the amplitudes of two overtaking solitary waves o...
Numerical calculations of the resonant interactions of three-dimensional short-crested waves very ne...
The breaking of waves is an important mechanism for a number of physical, chemical and biological pr...
Why do ocean waves break? Understanding this important and obvious property of the ocean surface has...
A curious feature of the ordinary linear theory of irregular waves is that the particle trajectories...
Ocean waves forced by the wind are multidirectional, even if the wind direction is steady. Direction...