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...
Main Author: | Emanuel, Kerry Andrew (Contributor) |
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Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor), Massachusetts Institute of Technology. Program in Atmospheres, Oceans, and Climate (Contributor) |
Format: | Article |
Language: | English |
Published: |
American Meteorological Society,
2012-10-09T14:00:11Z.
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Subjects: | |
Online Access: | Get fulltext |
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