Freaque wave statistics is analysed based on the data of South East coast of the Brazil. It is shown that such waves can be both due to linear and nonlinear dynamics. The wave climate in this area is very often dominated by a few uncorrelated wave systems and then the superposition of waves from different directions become likely. The available wave data was measured by wave buoys deployed off Rio de Janeiro State coast, where swell coming from the south are usually concomitant with northeast windsea generated by the South Atlantic anticyclone
An extremely large ('freak') wave is a typical though rare phenomenon observed in the sea. Special t...
This study is justified by the need to incorporate the analysis of atmospheric circulation condition...
As ondas geradas por tempestades causam as alterações mais significativas na costa arenosa. Este tra...
Freak waves occur abundantly in Campos Basin, located on the north-east coast of Rio de Janeiro, Bra...
A detailed climatology of ocean wind waves in the South Atlantic Ocean, based on ERA-5 reanalysis an...
Freak waves occur abundantly in Campos Basin, located on the northeast coast of Rio de Janeiro, Braz...
In this study, 30 years of sea state data, reconstructed by the wave generation model WWIII for the ...
Using the wave model SWAN (simulating waves nearshore), high waves on the southwestern Atlantic gene...
This work presents analyses of the atmospheric conditions and the hindcast of the surface wave field...
This work presents analyses of the atmospheric conditions and the hindcast of the surface wave field...
Understanding how wave climate variability and its trends change over time are crucial analyses requ...
This paper aims to identify the circulation associated with Easterly Wave Disturbances (EWDs) that p...
This paper provides a description of the wave climate off the Brazilian coast based on an eleven-yea...
This paper provides a description of the wave climate off the Brazilian coast based on an eleven-yea...
Abstract The wave energy potential on the Brazilian coast is estimated using in-situ buoy data and m...
An extremely large ('freak') wave is a typical though rare phenomenon observed in the sea. Special t...
This study is justified by the need to incorporate the analysis of atmospheric circulation condition...
As ondas geradas por tempestades causam as alterações mais significativas na costa arenosa. Este tra...
Freak waves occur abundantly in Campos Basin, located on the north-east coast of Rio de Janeiro, Bra...
A detailed climatology of ocean wind waves in the South Atlantic Ocean, based on ERA-5 reanalysis an...
Freak waves occur abundantly in Campos Basin, located on the northeast coast of Rio de Janeiro, Braz...
In this study, 30 years of sea state data, reconstructed by the wave generation model WWIII for the ...
Using the wave model SWAN (simulating waves nearshore), high waves on the southwestern Atlantic gene...
This work presents analyses of the atmospheric conditions and the hindcast of the surface wave field...
This work presents analyses of the atmospheric conditions and the hindcast of the surface wave field...
Understanding how wave climate variability and its trends change over time are crucial analyses requ...
This paper aims to identify the circulation associated with Easterly Wave Disturbances (EWDs) that p...
This paper provides a description of the wave climate off the Brazilian coast based on an eleven-yea...
This paper provides a description of the wave climate off the Brazilian coast based on an eleven-yea...
Abstract The wave energy potential on the Brazilian coast is estimated using in-situ buoy data and m...
An extremely large ('freak') wave is a typical though rare phenomenon observed in the sea. Special t...
This study is justified by the need to incorporate the analysis of atmospheric circulation condition...
As ondas geradas por tempestades causam as alterações mais significativas na costa arenosa. Este tra...