The theory for criticality presented in Part I 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 I are also discussed.</p
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...
The theory for criticality presented in Part I is extended to the unsteady problem, and a new formul...
The theory for criticality presented in Part 1 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...
The Benjamin–Feir instability is a modulational instability in which a uniform train of oscillatory ...
Full nonlinear equations for one-dimensional potential surface waves were used for investigation of ...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Within the framework of the fully nonlinear water waves equations, we consider a Stokes wavetrain mo...
We consider a full set of harmonics for the Stokes wave in deep water in the absence of viscosity, a...
Access restricted to the OSU CommunityRecently, a new approach to certain flow problems, called the ...
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...
The theory for criticality presented in Part I is extended to the unsteady problem, and a new formul...
The theory for criticality presented in Part 1 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...
The Benjamin–Feir instability is a modulational instability in which a uniform train of oscillatory ...
Full nonlinear equations for one-dimensional potential surface waves were used for investigation of ...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
Within the framework of the fully nonlinear water waves equations, we consider a Stokes wavetrain mo...
We consider a full set of harmonics for the Stokes wave in deep water in the absence of viscosity, a...
Access restricted to the OSU CommunityRecently, a new approach to certain flow problems, called the ...
A possible mechanism that is responsible for the occurrence of rogue waves in the ocean is the Benja...
In the 1960s, Benjamin and Feir, and Whitham, discovered that a Stokes wave would be unstable to lon...
The conditions leading to transition and turbulence appearance at the bottom of a solitary waveare d...