Self-Stratification of Tropical Cyclone Outflow. Part II: Implications for Storm Intensification
Tropical cyclones intensify and are maintained by surface enthalpy fluxes that result from the thermodynamics disequilibrium that exists between the tropical oceans and atmosphere. While this general result has been known for at least a half century, the detailed nature of feedbacks between thermody...
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| Format: | Article |
| Language: | en_US |
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American Meteorological Society
2012
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| Online Access: | http://hdl.handle.net/1721.1/73666 https://orcid.org/0000-0002-2066-2082 |