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A theory for the spinup of tropical depressions

✍ Scribed by D. J. Raymond; S. L. Sessions; Ž. Fuchs


Publisher
John Wiley and Sons
Year
2007
Tongue
English
Weight
195 KB
Volume
133
Category
Article
ISSN
0035-9009

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✦ Synopsis


Abstract

Recent advances in our understanding of the physics of precipitation over tropical oceans is married with vorticity dynamics to produce a simple theory for the development or non‐development of tropical depressions. This early phase of tropical cyclogenesis is perhaps the least understood part of the whole process. The theory predicts a finite amplitude threshold for intensification, with weaker disturbances decaying. Furthermore, only disturbances with radii larger than a critical value develop. Rough estimates of this critical radius place it near 1600 km, though better estimates of various parameters could change this value significantly. Copyright © 2007 Royal Meteorological Society


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