Add to ORKGNumerical results are presented to show that, for small-amplitude roughness, individual wave elevations attenuate at a far slower rate than the corresponding e ective wave elevation for both ocean waves travelling over a rough seabed in intermediate depth and waves in a thin plate in vacuo. Use of the e ective wave elevation, there- fore, results in misleading predictions of attenu- ation
Extreme wave statistics of unidirectional and counter-propagating seas are investigated, for the spe...
The local response of an ocean with slowly varying mean flow, stratification, and topography to two ...
The possibility of a rough seabed causing localisation of ocean waves in intermediate water depth is...
Numerical results are presented to show that, for small-amplitude roughness, individual wave elevati...
• Simulations obtained for water waves over rough seabed and waves in rough in vacuo plate. • Attenu...
Based on high-resolution laboratory data of instantaneous surface elevation and fluid velocity assoc...
Waves attenuate with distance travelled into rough and randomly disordered media. This is reminiscen...
The existence of ®exural waves con ned to the free edge of a ®uid-loaded plate is established theor...
The breaking of waves is an important mechanism for a number of physical, chemical and biological pr...
LaTex file, 16 pages, 4 figuresIn the limit of small values of the aspect ratio parameter (or wave s...
This paper concerns the statistical distribution of the crest heights associated with surface waves ...
A new set of laboratory experiments to examine the short-term statistics of crest elevation and wave...
International audienceIt is well known that wave induced bottom oscillations become more and moreneg...
Design criteria in ocean engineering, whether this is one in 50 years or one in 5000 years event, ar...
The transmission of water waves under vertical thin plates, e.g., offshore floating breakwaters, osc...
Extreme wave statistics of unidirectional and counter-propagating seas are investigated, for the spe...
The local response of an ocean with slowly varying mean flow, stratification, and topography to two ...
The possibility of a rough seabed causing localisation of ocean waves in intermediate water depth is...
Numerical results are presented to show that, for small-amplitude roughness, individual wave elevati...
• Simulations obtained for water waves over rough seabed and waves in rough in vacuo plate. • Attenu...
Based on high-resolution laboratory data of instantaneous surface elevation and fluid velocity assoc...
Waves attenuate with distance travelled into rough and randomly disordered media. This is reminiscen...
The existence of ®exural waves con ned to the free edge of a ®uid-loaded plate is established theor...
The breaking of waves is an important mechanism for a number of physical, chemical and biological pr...
LaTex file, 16 pages, 4 figuresIn the limit of small values of the aspect ratio parameter (or wave s...
This paper concerns the statistical distribution of the crest heights associated with surface waves ...
A new set of laboratory experiments to examine the short-term statistics of crest elevation and wave...
International audienceIt is well known that wave induced bottom oscillations become more and moreneg...
Design criteria in ocean engineering, whether this is one in 50 years or one in 5000 years event, ar...
The transmission of water waves under vertical thin plates, e.g., offshore floating breakwaters, osc...
Extreme wave statistics of unidirectional and counter-propagating seas are investigated, for the spe...
The local response of an ocean with slowly varying mean flow, stratification, and topography to two ...
The possibility of a rough seabed causing localisation of ocean waves in intermediate water depth is...