Case Studies on Convective Storms / Case Study 6, 25 July 1976: Dynamical-microphysical Evolution of a Convective Storm

This storm is the subject of a series of four papers. Studies of the storm environment showed that the storm grew in a weakly sheared environment (2x 10 ����� s �����) with instability of 3 to 4��K. The storm moved toward 200�� at 9 m s ����� and overtook low-level air, so that the relative inflow to the storm was from the southwest, resulting in new growth and updrafts at cloud base in that region.

Radar observations show that the storm formed along a confluence line in a region of isolated convergence. The storm was multicellular in nature with new cells forming rather close (2-4 km) to the main radar echo. Although individual radar cells could be identified during the early stages of the storm, as the storm became more vigorous the reflectivity structure had a quasi-steady state appearance with the main reflectivity region in the southwestern portion of the storm.