Is the State of the Air‐Sea Interface a Factor in Rapid Intensification and Rapid Decline of Tropical Cyclones?

Tropical storm intensity prediction remains a challenge in tropical meteorology. Some tropical storms undergo dramatic rapid intensification and rapid decline. Hurricane researchers have considered particular ambient environmental conditions including the ocean thermal and salinity structure and int...

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Veröffentlicht in:	Journal of geophysical research. Oceans 2017-12, Vol.122 (12), p.10174-10183
Hauptverfasser:	Soloviev, Alexander V., Lukas, Roger, Donelan, Mark A., Haus, Brian K., Ginis, Isaac
Format:	Artikel
Sprache:	eng
Schlagworte:	Aerodynamic drag Aerodynamics Air Air-sea coupling Amplification Capillary waves Computer simulation Cyclone dynamics Cyclones Drag Drag coefficient Drag coefficients Dynamics Ejection Environmental conditions Geophysics Gravitation Gravity Hurricanes Instability Interface stability Laboratory experiments Mathematical analysis Meteorology Numerical simulations Parameterization Physics rapid decline rapid intensification Sea surface Storms Temperature (air-sea) Tropical climate tropical cyclone Tropical cyclones Tropical depressions Tropical meteorology Tropical storms two‐phase environment Vortex dynamics Wind speed
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