Affiliation:
1. Department of Geological and Atmospheric Science, Iowa State University, Ames, Iowa
2. National Technical Systems, Littleton, Colorado
3. WindLogics Inc., Grand Rapids, Minnesota
Abstract
Abstract
Since the spring of 2002, tornadoes were sampled on nine occasions using Hardened In-Situ Tornado Pressure Recorder probes, video probes, and mobile mesonet instrumentation. This study describes pressure and, in some cases, velocity data obtained from these intercepts. In seven of these events, the intercepted tornadoes were within the radar-indicated or visually identified location of the supercell low-level mesocyclone. In the remaining two cases, the intercepted tornadoes occurred outside of this region and were located along either the rear-flank downdraft gust front or an internal rear-flank downdraft surge boundary.
The pressure traces, sometimes augmented with videography, suggest that vortex structures ranged from single-cell to two-cell, quite similar to the swirl-ratio-dependent continuum of vortex structures shown in laboratory and numerical simulations. Although near-ground tornado observations are quite rare, the number of contemporary tornado measurements now available permits a comparative range of observed pressure deficits for a wide variety of tornado sizes and intensities to be presented.
Publisher
American Meteorological Society
Reference62 articles.
1. A numerical simulation of cyclic tornadogenesis.;Adlerman,2000
2. In situ observations of the 21 April 2007 Tulia, Texas tornado.;Blair;Electron. J. Severe Storms Meteor.,2008
3. Measurements in the vicinity of severe thunderstorms and tornadoes with TOTO: 1982–1983 results.;Bluestein,1983
4. Mesocyclone evolution and tornadogenesis: Some observations.;Brandes;Mon. Wea. Rev.,1978
5. Tornadic thunderstorm characteristics determined with Doppler radar.;Brandes,1993
Cited by
93 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献