Add to ORKGHurricane is one of the most impressive air-sea interaction features in the world. Heat transferred from the ocean through the turbulent processes in hurricane boundary layer (HBL) i
Capturing TC intensity change remains a great challenge for most state-of-the-art operational foreca...
CBLAST was an effort conceived by the Office of Naval Research (ONR) to fill a gap in our understand...
Atmospheric models are strongly dependent on the turbulent exchange of momentum, sensible heat and m...
It is widely accepted that air–sea interaction is one of the key factors in controlling tropical cyc...
The extreme high winds, intense rainfall, large ocean waves, and copious sea spray in hurricanes pus...
Modifications were made to Corgnati's (1971) steady state, symmet-rical hurricane model, which ...
While the previous studies of the impacts of air–sea interaction on tropical cyclones (TCs) generall...
It is well-recognized that tropical cyclone (TC) intensity is strongly modulated by air-sea interact...
The ocean temperature (especially the Sea Surface Temperature (SST)) is very important to the format...
Observations suggest that under extreme wind speed conditions there is a widespread disruption of th...
The influence of convective heating on movement and vertical coupling of tropical cyclones (TCs) is ...
A recent advance in the Coupled Ocean–Atmosphere Mesoscale Prediction System (COAMPS) is de-scribed ...
The kinetic energy budget of hurricanes ’ asymmetry is calculated using scale interaction approach. ...
It is well recognized that air-sea interaction affects the development and modulation of tropical cy...
As part of the ONR sponsored Coupled Boundary Layer/Air-Sea Transfer (CBLAST) experiment, data from ...
Capturing TC intensity change remains a great challenge for most state-of-the-art operational foreca...
CBLAST was an effort conceived by the Office of Naval Research (ONR) to fill a gap in our understand...
Atmospheric models are strongly dependent on the turbulent exchange of momentum, sensible heat and m...
It is widely accepted that air–sea interaction is one of the key factors in controlling tropical cyc...
The extreme high winds, intense rainfall, large ocean waves, and copious sea spray in hurricanes pus...
Modifications were made to Corgnati's (1971) steady state, symmet-rical hurricane model, which ...
While the previous studies of the impacts of air–sea interaction on tropical cyclones (TCs) generall...
It is well-recognized that tropical cyclone (TC) intensity is strongly modulated by air-sea interact...
The ocean temperature (especially the Sea Surface Temperature (SST)) is very important to the format...
Observations suggest that under extreme wind speed conditions there is a widespread disruption of th...
The influence of convective heating on movement and vertical coupling of tropical cyclones (TCs) is ...
A recent advance in the Coupled Ocean–Atmosphere Mesoscale Prediction System (COAMPS) is de-scribed ...
The kinetic energy budget of hurricanes ’ asymmetry is calculated using scale interaction approach. ...
It is well recognized that air-sea interaction affects the development and modulation of tropical cy...
As part of the ONR sponsored Coupled Boundary Layer/Air-Sea Transfer (CBLAST) experiment, data from ...
Capturing TC intensity change remains a great challenge for most state-of-the-art operational foreca...
CBLAST was an effort conceived by the Office of Naval Research (ONR) to fill a gap in our understand...
Atmospheric models are strongly dependent on the turbulent exchange of momentum, sensible heat and m...