A vertical profile of reflectivity has many applications for radar-derived products. For example, a VPR identified as tropical in nature is used to invoke a tropical Z-R for precipitation estimates. Two types of VPRs are computed - one based on the 3D reflectivity field and the other based on individual tilts. Recent RAP model +10C, 0C, -10C and -20C are indicated.
For details see:
Zhang, J., C. Langston, K. Howard, 2008: Brightband Identification Based on Vertical Profiles of Reflectivity from the WSR-88D. J. Atmos. Oceanic Technol., 25, 1859–1872.
Zhang, J., Y. Qi, 2010: A Real-Time Algorithm for the Correction of Brightband Effects in Radar-Derived QPE. J. of Hydrometeorology, 11, 1157-1171.
TIP: If a circle is hollow (no VPR) go back in time to find the most recent detection.

Vertical profile of reflectivity for KVNX
