June 4th 2003

This event was a Mesoscale Convective System (MCS) that developed early in the morning in North Texas and Southwestern Oklahoma. It is typical for that time of year. It propagated to the NE and was over the KOUN radar in mid morning. By that time, the system developed a mesoscale convective vortex in its NW part which caused formation of three intense cells.

VCP 43 - EL=0.5 deg

LONG PRT

Reflectivity - Long PRT - Non PC - EL=0.5

Reflectivity

 Spectrum Width - Long PRT - Non PC - EL=0.5

Spectrum Width

SHORT PRT

 Velocity - Short PRT - Non PC - EL=0.5

Non PC Doppler Velocity

 Velocity - Short PRT - PC - EL=0.5

PC Doppler Velocity

MEDIUM PRT

 Velocity - Medium PRT - Non PC - EL=0.5

Non PC Doppler Velocity

 Velocity - Medium PRT - PC - EL=0.5

PC Doppler Velocity

 

VCP 43 - EL=1.5 deg

LONG PRT

 Reflectivity - Long PRT - Non PC - EL=1.5

Reflectivity

 Spectrum Width - Long PRT - Non PC - EL=1.5

Spectrum Width

SHORT PRT

 Velocity - Short PRT - Non PC - EL=1.5

Non PC Doppler Velocity

 Velocity - Short PRT - PC - EL=1.5

PC Doppler Velocity