Casebook 3 June 2003: Difference between revisions
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==CSU-CHILL Casebook: 3 June, 2003== | ==CSU-CHILL Casebook: 3 June, 2003== | ||
During the early evening hours of 3 June 2003 UTC (local date 2 June), a line of thunderstorms developed immediately east and south of the CSU-CHILL radar. By 01 UTC, the low level outflow from these storms had become quite strong with some areas of aliased outbound (positive) radial velocities. The individual convective precipitation cores produced varying amounts of differential propagation phase shift (<math>\psi_{dp}</math>). An example of these storm to storm <math>\psi_{dp}</math> variations can be seen in the second elevation angle PPI sweep made at 0102:43 UTC. | During the early evening hours of 3 June 2003 UTC (local date 2 June), a line of thunderstorms developed immediately east and south of the CSU-CHILL radar. By 01 UTC, the low level outflow from these storms had become quite strong with some areas of aliased outbound (positive) radial velocities. The individual convective precipitation cores produced varying amounts of differential propagation phase shift (<math>\psi_{dp}</math>). An example of these storm to storm <math>\psi_{dp}</math> variations can be seen in the second elevation angle PPI sweep made at 0102:43 UTC. | ||
[http://chill.colostate.edu/java/vchill.php?sweep=xlab.chill.colostate.edu:2510*/dsk/dnf/data/2003/06/03/%20DIR*CHL20030603_012246%20COMSUR%20PPI*Sweep%2002¢er=40.,-40.&range=70.&plot=PHIDP example in VCHILL] | |||
[[Casebook 26 May 2003|prev]] [[Casebook 19 June 2003|next]] | [[Casebook 26 May 2003|prev]] [[Casebook 19 June 2003|next]] | ||
Revision as of 07:40, 19 December 2007
CSU-CHILL Casebook: 3 June, 2003
During the early evening hours of 3 June 2003 UTC (local date 2 June), a line of thunderstorms developed immediately east and south of the CSU-CHILL radar. By 01 UTC, the low level outflow from these storms had become quite strong with some areas of aliased outbound (positive) radial velocities. The individual convective precipitation cores produced varying amounts of differential propagation phase shift (). An example of these storm to storm variations can be seen in the second elevation angle PPI sweep made at 0102:43 UTC.
