Excitation of Low-Level Energy Wave Accumulations and Tropical Cyclone Formation
A spectral shallow water model is used at the 850 mb level to investigate the effects of cyclonic vorticity on heating in the lower troposphere and how this in turn causes an increase in cyclonic vorticity generation, creating a nonlinear vorticity feedback mechanism. The model is initialized with...
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Format: | Others |
Language: | en_US |
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Georgia Institute of Technology
2005
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Online Access: | http://hdl.handle.net/1853/7282 |