In both the ocean and the atmosphere, the interaction of a density stratified flow with topography can generate large-amplitude, horizontally propagating internal solitary waves. Often these waves are observed in regions where the waveguide properties vary in the direction of propagation. In this article we consider nonlinear evolution equations of the Kortewegde Vries type, with variable coefficients, and use these models to review the properties of slowly-varying periodic and solitary waves
The Korteweg – de Vries (KdV) equation is a fundamental mathematical model for the description of we...
It is now generally accepted that solitary waves are a commonly occurring and important dynamical f...
International audienceA higher-order extension of the familiar Korteweg-de Vries equation is derived...
In the coastal oceans, the interaction of currents (such as the barotropic tide) with topography can...
Solitary water waves are long nonlinear waves that can propagate steadily over long distances. They ...
The basic theory of internal solitary waves is reviewed, with the main emphasis on applications to t...
Large-amplitude, horizontally-propagating internal wave trains are commonly observed in the coastal ...
Abstract:- Internal solitary waves are commonly observed in the coastal ocean and atmospheric bounda...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
International audienceThe propagation of large- amplitude internal waves in the ocean is studied her...
A higher-order extension of the familiar Korteweg-de Vries equation is derived for internal solita...
This paper presents a horizontally two-dimensional theory based on a variable-coefficient Kadomtsev-...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
The propagation of large- amplitude internal waves in the ocean is studied here for the case when th...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
The Korteweg – de Vries (KdV) equation is a fundamental mathematical model for the description of we...
It is now generally accepted that solitary waves are a commonly occurring and important dynamical f...
International audienceA higher-order extension of the familiar Korteweg-de Vries equation is derived...
In the coastal oceans, the interaction of currents (such as the barotropic tide) with topography can...
Solitary water waves are long nonlinear waves that can propagate steadily over long distances. They ...
The basic theory of internal solitary waves is reviewed, with the main emphasis on applications to t...
Large-amplitude, horizontally-propagating internal wave trains are commonly observed in the coastal ...
Abstract:- Internal solitary waves are commonly observed in the coastal ocean and atmospheric bounda...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
International audienceThe propagation of large- amplitude internal waves in the ocean is studied her...
A higher-order extension of the familiar Korteweg-de Vries equation is derived for internal solita...
This paper presents a horizontally two-dimensional theory based on a variable-coefficient Kadomtsev-...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
The propagation of large- amplitude internal waves in the ocean is studied here for the case when th...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
The Korteweg – de Vries (KdV) equation is a fundamental mathematical model for the description of we...
It is now generally accepted that solitary waves are a commonly occurring and important dynamical f...
International audienceA higher-order extension of the familiar Korteweg-de Vries equation is derived...