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Strong mesocyclone on a thunderstorm near Tuscaloosa, Alabama, that was analyzed as fitting the characteristics of a TVS.It was associated with a tornado.. A tornadic vortex signature, abbreviated TVS, is a Pulse-Doppler radar weather radar detected rotation algorithm that indicates the likely presence of a strong mesocyclone that is in some stage of tornadogenesis. [1]
The tornado then caused high-end EF0 to EF1 damage to homes and trees in another neighborhood before briefly reaching low-end EF2 strength again as it moved directly over SR 119, where more large tree trunks were snapped. [74] Radar image of EF3 Eagle Point tornado at peak intensity as it struck Eagle Point at 1841Z on 3-25-2021.
An example of a tornado warning polygon issued by the National Weather Service. A tornado warning (SAME code: TOR) is a public warning that is issued by weather forecasting agencies to an area in the direct path of a tornado, or a severe thunderstorm capable of producing one, and advises individuals in that area to take cover.
The 2008 Atlanta tornado outbreak was a destructive and deadly tornado outbreak that affected the Southeastern United States on March 14–15, 2008. The most infamous tornado of the outbreak occurred on March 14 when an isolated but strong EF2 tornado caused widespread damage across Downtown Atlanta, Georgia, including to the CNN Center and to the Georgia Dome, which was hosting the 2008 SEC ...
Often, news of a tornado would reach a local weather office after the storm. However, with the advent of weather radar, areas near a local office could get advance warning of severe weather. The first public tornado warnings were issued in 1950 and the first tornado watches and convective outlooks came about in 1952.
Beginning at midnight July 7 and ending at 11 p.m. July 10, the National Weather Service (NWS) issued 201 tornado warnings as Beryl moved inland, with 97 warnings issued on July 8.
Classic-style hook echo of the F5 1999 Bridge Creek-Moore tornado.. A hook echo is a pendant or hook-shaped weather radar signature as part of some supercell thunderstorms.It is found in the lower portions of a storm as air and precipitation flow into a mesocyclone, resulting in a curved feature of reflectivity.
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