Casebook 11 July 2001: Difference between revisions
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==CSU-CHILL Casebook: 11 July, 2001== | ==CSU-CHILL Casebook: 11 July, 2001== | ||
An area of severe thunderstorms approached the city of Greeley from the southwest around 0200 UTC. Strong, low level outflow winds developed as the storm began to affect the city. Considerable roof and tree damage was incurred. The outflow generated a well defined arcus cloud that was photographed from the CHILL radar site. The radar was located between the gust front / fine line and the main precipitation core at 0225 UTC. By 0347 UTC, strong convection had become quite widespread across much of the CHILL radar's northeast azimuth quadrant. | An area of severe thunderstorms approached the city of Greeley from the southwest around 0200 UTC. Strong, low level outflow winds developed as the storm began to affect the city. Considerable roof and tree damage was incurred. The outflow generated a well defined arcus cloud that was photographed from the CHILL radar site. The radar was located between the gust front / fine line and the main precipitation core at 0225 UTC. By 0347 UTC, strong convection had become quite widespread across much of the CHILL radar's northeast azimuth quadrant. | ||
[http://chill.colostate.edu/java/vchill.php?sweep=xlab.chill.colostate.edu:2510*/dsk/dnf/data/2001/07/11/%20DIR*CHL20010711_022302%20GUSTSUR%20PPI*Sweep%2003¢er=0.,0.&range=25.&plot=VelLoad example in VCHILL] | |||
[[Casebook 21 June 2001|prev]] [[Casebook 29 August 2002|next]] | [[Casebook 21 June 2001|prev]] [[Casebook 29 August 2002|next]] | ||
Revision as of 06:05, 9 December 2007
CSU-CHILL Casebook: 11 July, 2001
An area of severe thunderstorms approached the city of Greeley from the southwest around 0200 UTC. Strong, low level outflow winds developed as the storm began to affect the city. Considerable roof and tree damage was incurred. The outflow generated a well defined arcus cloud that was photographed from the CHILL radar site. The radar was located between the gust front / fine line and the main precipitation core at 0225 UTC. By 0347 UTC, strong convection had become quite widespread across much of the CHILL radar's northeast azimuth quadrant.
