The 8 June 1995 McLean, Texas, Storm. Part I: Observations of Cyclic Tornadogenesis
Open Access
- 1 November 2002
- journal article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 130 (11) , 2626-2648
- https://doi.org/10.1175/1520-0493(2002)130<2626:tjmtsp>2.0.co;2
Abstract
On 8 June 1995 scientists participating in the Verification of the Origins of Rotation in Tornadoes Experiment (VORTEX) collected airborne Doppler radar data in a storm that produced a family of tornadoes near McLean, Texas. The Electra Doppler Radar (ELDORA) scanned three significant tornadoes during their formative and mature stages; one of the tornadoes was of F4/F5 intensity. Evidence from pseudo-dual-Doppler analyses of the ELDORA data reveals a process of cyclic tornado formation qualitatively similar to that depicted in previous conceptual models. In particular, the rear-flank gust front appears to play a major role in determining the location of the next vortex in the series. When a tornado forms, a small region (3–5 km wide) of outflow surges ahead of the tornado, producing a local bulge in the gust front. A new vorticity maximum may form near the leading edge of the outflow. In contrast to what is suggested by earlier conceptual models, intersection of the rear-flank gust front with a w... Abstract On 8 June 1995 scientists participating in the Verification of the Origins of Rotation in Tornadoes Experiment (VORTEX) collected airborne Doppler radar data in a storm that produced a family of tornadoes near McLean, Texas. The Electra Doppler Radar (ELDORA) scanned three significant tornadoes during their formative and mature stages; one of the tornadoes was of F4/F5 intensity. Evidence from pseudo-dual-Doppler analyses of the ELDORA data reveals a process of cyclic tornado formation qualitatively similar to that depicted in previous conceptual models. In particular, the rear-flank gust front appears to play a major role in determining the location of the next vortex in the series. When a tornado forms, a small region (3–5 km wide) of outflow surges ahead of the tornado, producing a local bulge in the gust front. A new vorticity maximum may form near the leading edge of the outflow. In contrast to what is suggested by earlier conceptual models, intersection of the rear-flank gust front with a w...Keywords
This publication has 51 references indexed in Scilit:
- A Numerical Simulation of Cyclic MesocyclogenesisJournal of the Atmospheric Sciences, 1999
- Mobile Sounding Observations of a Tornadic Storm near the Dryline: The Canadian, Texas Storm of 7 May 1986Monthly Weather Review, 1988
- Doppler Radar Sampling Limitations in Convective StormsJournal of Atmospheric and Oceanic Technology, 1985
- Observations of Two Colorado Thunderstorms by Means of a Zenith-Pointing Doppler RadarJournal of Applied Meteorology, 1980
- Flow in Severe Thunderstorms Observed bu Dual-Doppler RadarMonthly Weather Review, 1977
- Multiple Vortex Features in the Tornado Cyclone and the Occurrence of Tornado FamiliesMonthly Weather Review, 1976
- Tornado characteristics revealed by Doppler radarGeophysical Research Letters, 1975
- A Theory for the Determination of Wind and Precipitation Velocities with Doppler RadarsJournal of the Atmospheric Sciences, 1969
- Airflow and Precipitation Trajectories Within Severe Local Storms Which Travel to the Right of the WindsJournal of the Atmospheric Sciences, 1964
- AN OPERATIONAL OBJECTIVE ANALYSIS SYSTEMMonthly Weather Review, 1959