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Analysis of the 13 May 2005 Knox County Texas Tornadic Event. Derek R. Deroche National Oceanic and Atmospheric Administration National Weather Service WFO San Angelo, TX. Blake E. Michaleski University of South Alabama Meteorology Program, Department of Earth Sciences Mobile, Alabama. - PowerPoint PPT Presentation
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Analysis of the 13 May 2005 Knox County Texas Tornadic Event
Derek R. DerocheNational Oceanic and Atmospheric
AdministrationNational Weather Service
WFO San Angelo, TX
Blake E. Michaleski
University of South AlabamaMeteorology Program,
Department of Earth SciencesMobile, Alabama
ABSTRACT
On 13 May 2005, two tornados occurred across portions of Knox County, Texas as part of a larger severe weather outbreak. The first tornado was observed visually by several storm chasers, including the authors, as well as remotely by the Doppler on Wheels (DOW) mobile radar. The second tornado was completely rain wrapped during its life cycle, therefore it was only observed remotely by the DOW team. The tornados moved through sparsely populated areas with no reported damage.
Convective initiation occurred across north-central Texas with a supercell that originated near Paducah in Cottle County. As this storm moved southeast across Cottle County and into Knox County, it underwent an occlusion of the mesocyclone. The original circulation was able to maintain itself with a new storm scale circulation developing along the outflow boundary intersection of the rear-flank downdraft and the forward-flank downdraft. Thus, a ‘double supercell’ structure evolved with the forward supercell being the tornado-producing storm.
The case study presented herein will examine the Knox County event in several aspects including a synoptic analysis, a mesoscale analysis of the boundary layer, direct visual observations, as well as an analysis of DOW and Weather Surveillance Radar-1988 Doppler (WSR-88D) observations. Access to DOW data will allow an examination of WSR-88D data against the finescale resolution of the DOW mobile radar to correlate the vortex signatures generated by both. Later research and papers will attempt to build on this case study by examining 30m above ground level DOW measurements with actual surface wind velocities.
Radar Presentation
Synoptic Scale Analysis
Mesoscale Analysis
Tornado 1: 2340 (12km NNE Benjamin, TX) nearly stationary to 2346 (12 km NE of Benjamin), Peak V=49 m/s,
Tornado 2: 0009 (6 km W of Vera, TX) moves S, then ESE, then SE, crossing Hefner, TX at 0037, then
5 km east of Goree, TX by 0052. Peak V=79 m/s at 0029.
Cross Sectional Analysis 2343 Z 13 May 2005
0.5° Base Reflectivity
0.5° Base Reflectivity
0.5° Base Reflectivity
0.5° 2-D X Sect Storm Relative Velocity
0.5° 2-D X Sect Base Reflectivity
0.5° 3-D X Sect Base Reflectivity
Doppler On Wheels 3 (DOW3) Analysis 2342 Z 13 May 2005
Uncalibrated ReflectivityEdited Doppler Velocity
Edited Doppler Velocity
Edited Doppler Velocity
Uncalibrated Reflectivity
Uncalibrated Reflectivity
Cross Sectional Analysis 0040 – 0045 Z 13 May 2005
0045 Z 0.5° Base Reflectivity 0045 Z 0.5° 2-D X Sect Storm Relative Velocity
0040 Z 0.5° Storm Relative Velocity
0040 Z 0.5° 2-D X Sect Storm Relative Velocity
0045 Z 0.5° Base Reflectivity 0045 Z 0.5° 3-D X Sect Storm Relative Velocity
Edited Doppler Velocity
Edited Doppler Velocity
Edited Doppler Velocity
Uncalibrated Reflectivity
Uncalibrated Reflectivity
Uncalibrated Reflectivity
Doppler On Wheels 3 (DOW3) Analysis 0027 Z 13 May 2005