We study the long-time evolution of the trailing shelves that form behind solitary waves moving through an inhomogeneous media, within the framework of the variable-coeffecient Korteweg-de Vries equation. We show that the nonlinear evolution of the shelf leads typically to the generation of an undular bore and an expansion fan, which form apart but start to overlap and nonlinearly interact after a certain time interval. The interaction zone expands with time and asymptotically as time goes to infinity occupies the whole perturbed region. Its oscillatory structure strongly depends on the sign of the inhomogeneity gradient of the variable background medium. We describe the nonlinear evolution of the shelves in terms of exact solutions to the ...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
In the coastal oceans, the interaction of currents (such as the barotropic tide) with topography can...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
The Korteweg – de Vries (KdV) equation is a fundamental mathematical model for the description of we...
In both the ocean and the atmosphere, the interaction of a density stratified flow with topography c...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
This paper considers the propagation of shallow-water solitary and nonlinear periodic waves over a g...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
Solitary water waves are long nonlinear waves that can propagate steadily over long distances. They ...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
In the coastal oceans, the interaction of currents (such as the barotropic tide) with topography can...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
We study the long-time evolution of the trailing shelves that form behind solitary waves moving thro...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
We consider the solitary wave solutions of a Korteweg-de Vries equation, where the coefficients in t...
The Korteweg – de Vries (KdV) equation is a fundamental mathematical model for the description of we...
In both the ocean and the atmosphere, the interaction of a density stratified flow with topography c...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
This paper considers the propagation of shallow-water solitary and nonlinear periodic waves over a g...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
Solitary water waves are long nonlinear waves that can propagate steadily over long distances. They ...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
We consider the propagation of a shallow-water undular bore over a gentle monotonic bottom slope con...
In the coastal oceans, the interaction of currents (such as the barotropic tide) with topography can...