Research Article

Improving the Predictability of Severe Convective Weather Processes by Using Wind Vectors and Potential Temperature Changes: A Case Study of a Severe Thunderstorm

Figure 9

Vertical cross sections of radial wind speed as seen by Doppler radar at the WUHN station on July 27, 2007, at 8:14 p.m., azimuth at 342.00° (left), 8:26 p.m., azimuth at 345.00° (center), and 8:38 p.m., azimuth at 352.00° (right). The units for the radial wind speed are m/s.