Rapid filamentation zones in intense tropical cyclones

Research output: AbstractPaperpeer-review

Abstract

The rapid filamentation zones in intense tropical cyclones was discussed. Radar data was used to show the weak stratiform precipitation in the moat. It was found that clouds were highly distorted and suppressed in regions where the filamental time was less than the timescale of moist overturning. It was observed that rapid filamentation zones occurred in a circular region at a radius smaller than the initial bactropically unstable ring of vorticity. Analysis shows the nondivergent barotropic system, strain-dominated flow was the reason for the formation of a moat.

Original languageEnglish
Pages443-444
Number of pages2
StatePublished - 2004
Event26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States
Duration: May 3 2004May 7 2004

Conference

Conference26th Conference on Hurricanes and Tropical Meteorolgy
Country/TerritoryUnited States
CityMiami, FL.
Period05/3/0405/7/04

Fingerprint

Dive into the research topics of 'Rapid filamentation zones in intense tropical cyclones'. Together they form a unique fingerprint.

Cite this