Please use this identifier to cite or link to this item:

Re-Examining Tropical Cyclone Radial Structure From Flight-Level Aircraft Observations: Implications For Vortex Resiliency And Intensification

File Description SizeFormat 
uhm_ms_3860_r.pdfVersion for non-UH users. Copying/Printing is not permitted3.85 MBAdobe PDFView/Open
uhm_ms_3860_uh.pdfVersion for UH users3.85 MBAdobe PDFView/Open

Item Summary

Title: Re-Examining Tropical Cyclone Radial Structure From Flight-Level Aircraft Observations: Implications For Vortex Resiliency And Intensification
Authors: Mallen, Kevin J.
Issue Date: May 2004
Abstract: The importance of the radial structure on two aspects of the tropical cyclone (TC) intensity change problem is addressed: the vortex resiliency to ambient vertical wind shear and rapid vortex intensification. Theoretical studies, based on vortex Rossby wave (VRW) dynamics, have established that the degree of vortex broadness in the near-core region beyond the radius of maximum wind (RMW) determines the realignment or tilting over of a TC vortex in vertically sheared environments. The sensitivity of the initial specification of idealized vortices demonstrated by numerical simulations brings into question how well the "true" nature of TC radial structure is represented by some commonly used idealized vortices. Although the importance of the initial radial structure on the rate of vortex intensification is not well established theoretically, the issue of whether unique aspects of the swirling wind structure are observed prior to rapid intensification events is also addressed. The primary circulation of TCs is re-examined by utilizing flight-level observations collected from Atlantic and eastern Pacific storms during 1977-2001, in which several hundred radial profiles of azimuthal-mean tangential wind and relative vorticity are constructed from over five thousand flight leg segments. This comprehensive analysis principally reaffirms that real TC structure is characterized by a relatively slow tangential wind decrease beyond the RMW and a monotonically decreasing skirt of significant cyclonic relative vorticity. These characteristics, however, are found to be conspicuously absent in some idealized vortices frequently used in theoretical studies of TC evolution. Secondly, an investigation of the relationship between the initial tangential wind structure and the future intensification rate reveals that no unique characteristics exist just prior to rapid intensification events. The restricted range observed in the tangential wind parameters for a limited number of cases, however, suggest that necessary conditions may exist for rapid intensification. Although the radial structure appears to be critical for the vortex resiliency, the sole importance of the initial swirling wind structure on the intensification remains inconclusive.
Rights: All UHM dissertations and theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission from the copyright owner.
Appears in Collections:M.S. - Meteorology

Please contact if you need this content in an ADA compliant alternative format.

Items in ScholarSpace are protected by copyright, with all rights reserved, unless otherwise indicated.