The theory for criticality presented in Part 1 is extended to the unsteady problem, and a new formulation of the Benjamin–Feir instability for Stokes waves in finite depth coupled to a mean flow, which takes the criticality matrix as an organizing centre, is presented. The generation of unsteady dark solitary waves at points of stability changes and their connection with the steady dark solitary waves of Part 1 are also discussed.</p
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
Abstract. We consider the stability of periodic gravity free-surface water waves traveling downstrea...
The theory for criticality presented in Part I is extended to the unsteady problem, and a new formul...
A generalization of criticality – called secondary criticality – is introduced and applied to finite...
A generalization of criticality - called secondary criticality - is introduced and applied to finite...
Various classes of steady and unsteady dark solitary waves (DSWs) are known to exist in modulation e...
Various classes of steady and unsteady dark solitary waves (DSWs) are known to exist in modulation e...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Access restricted to the OSU CommunityRecently, a new approach to certain flow problems, called the ...
The Benjamin–Feir instability is a modulational instability in which a uniform train of oscillatory ...
We consider a full set of harmonics for the Stokes wave in deep water in the absence of viscosity, a...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Full nonlinear equations for one-dimensional potential surface waves were used for investigation of ...
This talk will examine the stability properties of representative cases of nonlinear dispersive wave...
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
Abstract. We consider the stability of periodic gravity free-surface water waves traveling downstrea...
The theory for criticality presented in Part I is extended to the unsteady problem, and a new formul...
A generalization of criticality – called secondary criticality – is introduced and applied to finite...
A generalization of criticality - called secondary criticality - is introduced and applied to finite...
Various classes of steady and unsteady dark solitary waves (DSWs) are known to exist in modulation e...
Various classes of steady and unsteady dark solitary waves (DSWs) are known to exist in modulation e...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Access restricted to the OSU CommunityRecently, a new approach to certain flow problems, called the ...
The Benjamin–Feir instability is a modulational instability in which a uniform train of oscillatory ...
We consider a full set of harmonics for the Stokes wave in deep water in the absence of viscosity, a...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Full nonlinear equations for one-dimensional potential surface waves were used for investigation of ...
This talk will examine the stability properties of representative cases of nonlinear dispersive wave...
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
Abstract. We consider the stability of periodic gravity free-surface water waves traveling downstrea...