Radar Imagery
KRAX Base Reflectivity Image from 2030Z (430 PM EDT) Wednesday, June 23, 2004.
Click on the image to enlarge.
Java Loop of base reflectivity imagery from
krax WSR-88D.
The loop is from 1859Z (259 PM EDT) Wednesday June 23, 2004 through 0158Z (958 PM EDT) Wednesday June 23, 2004.
The thunderstorms were organized into multi-cell segments. Note that the outflow boundaries from thunderstorms
just northwest of Raleigh became better defined as they moved past the Raleigh area, producing additional thunderstorms
in locations southeast of Raleigh.
In terms of storm structure as indicated by radar imagery and by wind damage reports, the most impressive
storm of the day was located in western Halifax County between 4:20 and 4:35 PM EDT (2020Z - 2035Z)”.
The 4-Panel image contains Composite Reflectivity (CR) imagery in the upper left, Vertically Integrated
Liquid (VIL) in the upper right,"8-bit" Reflectivity imagery “(0.5 slice)” in the lower left, and "8-bit"
Storm Relative Velocity imagery “(0.5. slice)” in the lower right.
While the storm relative velocity imagery shows at weak mesocylone, it is the strong reflectivity cores
in the CR and the “8 bit” imagery along with the high VILS that indicate a severe weather threat.
4-Panel KRAX radar imagery from 2035Z (435 PM EDT) Wednesday, June 23, 2004.
Click on the image to enlarge.
The 4-Panel image contains Composite Reflectivity (CR) imagery in the upper left, Vertically Integrated Liquid (VIL)
in the upper right, "8-bit" Reflectivity imagery “(0.5. slice)” in the lower left, and "8-bit" Storm Relative Velocity imagery “(0.5. slice)” in
the lower right.
KRAX plan view and cross section of the Thunderstorm that produced widespread wind damage across
much of western Halifax county from 2020Z (420 PM EDT) on Wednesday, June 23, 2004. Note the greater
than 65 dBZ elevated core ranging from 12,000 to 29,000 feet “and the storm’s “overhang”, indicative
of a strong and sustained updraft.
The image on the left is of Composite Reflectivity (CR) from KRAX. The white line is the location in which the cross
section is taken. The image on the right is of a Reflectivity Cross Section (RCS) taken along the white line
in the Composite Reflectivity (CR) image looking east. Note the greater than 65 dBZ elevated core ranging from 12,000 to 29,000 feet.
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