The linear stability theory of wind-wave generation is revisited with an emphasis on the generation of wave groups. The outcome is the fundamental requirement that the group move with a real-valued group velocity. This implies that both the wave frequency and the wavenumber should be complex-valued, and in turn this then leads to a growth rate in the reference frame moving with the group velocity which is in general different from the temporal growth rate. In the weakly nonlinear regime, the amplitude envelope of the wave group is governed by a forced nonlinear Schrödinger equation. The effect of the wind forcing term is to enhance modulation instability both in terms of the wave growth and in terms of the domain of instability in the modul...
One mechanism for the growth of ocean surface waves by wind is through a shear instability that was ...
Rogue wave generation can be explained on the basis of modulational instability. Thepaper reports on...
The modulational instability of gravity wave trains on the surface of water acted upon by wind and u...
A numerical and experimental investigation of modulational instability and breaking of nonlinear wav...
In many physical contexts, notably including deep water waves, modulation instability in one space d...
For weakly nonlinear waves in one space dimension, the nonlinear Schrödinger Equation is widely acce...
Since the work of Benjamin & Feir (1967), water waves propagating in infinite depth are known to be ...
In the wind-driven wave regime, the Miles mechanism gives an estimate of the growth rate of the wave...
In this paper we demonstrate numerical computations of turbulent wind blowing over group of waves th...
Evolution of nonlinear wave groups to breaking under wind forcing was studied by means of a fully no...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
The interaction of wind and water wave groups is investigated theoretically and numerically. A steep...
Waves on the open sea grow under the influence of strong winds. However, most wave models used in of...
The effect of vorticity or shear on the inviscid evolution and instability of surface waves is discu...
A model for the downward transfer of wind momentum is derived for growing waves. It is shown that wa...
One mechanism for the growth of ocean surface waves by wind is through a shear instability that was ...
Rogue wave generation can be explained on the basis of modulational instability. Thepaper reports on...
The modulational instability of gravity wave trains on the surface of water acted upon by wind and u...
A numerical and experimental investigation of modulational instability and breaking of nonlinear wav...
In many physical contexts, notably including deep water waves, modulation instability in one space d...
For weakly nonlinear waves in one space dimension, the nonlinear Schrödinger Equation is widely acce...
Since the work of Benjamin & Feir (1967), water waves propagating in infinite depth are known to be ...
In the wind-driven wave regime, the Miles mechanism gives an estimate of the growth rate of the wave...
In this paper we demonstrate numerical computations of turbulent wind blowing over group of waves th...
Evolution of nonlinear wave groups to breaking under wind forcing was studied by means of a fully no...
This paper analyses the spatial evolution of steep directionally spread transient wave groups on dee...
The interaction of wind and water wave groups is investigated theoretically and numerically. A steep...
Waves on the open sea grow under the influence of strong winds. However, most wave models used in of...
The effect of vorticity or shear on the inviscid evolution and instability of surface waves is discu...
A model for the downward transfer of wind momentum is derived for growing waves. It is shown that wa...
One mechanism for the growth of ocean surface waves by wind is through a shear instability that was ...
Rogue wave generation can be explained on the basis of modulational instability. Thepaper reports on...
The modulational instability of gravity wave trains on the surface of water acted upon by wind and u...