We suggest that there exists a natural bandwidth of wave trains, including trains of wind-generated waves with a continuous spectrum, determined by their steepness. Based on laboratory experiments with monochromatic waves, we show that, if no side-band perturbations are imposed, the ratio between the wave steepness and bandwidth is restricted to certain limits. These limits are consistent with field observations of narrow-banded wind-wave spectra if a characteristic width of the spectral peak and average steepness are used. The role of the wind in such modulation is also discussed
This paper extends our previous study of the breaking probability of dominant deep water gravity sur...
Data from a spatial array of wave gauges is analysed using the Wavelet Directional Method (WDM) to d...
[1] Microwave and acoustic systems operated in the large wind-wave tank in Luminy, Marseille, France...
Modulations of deep water waves are studied by a new formalism of spectral filtering. For single-mod...
This paper presents a comprehensive set of field experiments investigating the form of the asymptoti...
This paper presents a comprehensive set of field experiments investigating the form of the asymptoti...
International audienceThe effect of wind forcing on monochromatic modulated water waves was investig...
This paper describes a comprehensive field experiment aimed at determining the form of the asymptoti...
The modulational instability of gravity wave trains on the surface of water acted upon by wind and u...
In the open ocean the formation of large waves is non-linear. This non-linearity modifies the shape ...
International audienceWe experimentally study the properties of nonlinear surface gravity waves in a...
International audienceThis paper reports on laboratory experiment results on wind-driven surface wav...
The experimental data from the Southern Ocean Waves Experiment (SOWEX) and the Duck, North Carolina ...
We extend the Miles mechanism of wind-wave generation to finite depth. A beta-Miles linear growth ra...
Knowledge about the hydrodynamic modulation of microscale wind waves by long waves is needed for mic...
This paper extends our previous study of the breaking probability of dominant deep water gravity sur...
Data from a spatial array of wave gauges is analysed using the Wavelet Directional Method (WDM) to d...
[1] Microwave and acoustic systems operated in the large wind-wave tank in Luminy, Marseille, France...
Modulations of deep water waves are studied by a new formalism of spectral filtering. For single-mod...
This paper presents a comprehensive set of field experiments investigating the form of the asymptoti...
This paper presents a comprehensive set of field experiments investigating the form of the asymptoti...
International audienceThe effect of wind forcing on monochromatic modulated water waves was investig...
This paper describes a comprehensive field experiment aimed at determining the form of the asymptoti...
The modulational instability of gravity wave trains on the surface of water acted upon by wind and u...
In the open ocean the formation of large waves is non-linear. This non-linearity modifies the shape ...
International audienceWe experimentally study the properties of nonlinear surface gravity waves in a...
International audienceThis paper reports on laboratory experiment results on wind-driven surface wav...
The experimental data from the Southern Ocean Waves Experiment (SOWEX) and the Duck, North Carolina ...
We extend the Miles mechanism of wind-wave generation to finite depth. A beta-Miles linear growth ra...
Knowledge about the hydrodynamic modulation of microscale wind waves by long waves is needed for mic...
This paper extends our previous study of the breaking probability of dominant deep water gravity sur...
Data from a spatial array of wave gauges is analysed using the Wavelet Directional Method (WDM) to d...
[1] Microwave and acoustic systems operated in the large wind-wave tank in Luminy, Marseille, France...