Numerical Study of a Southwest Vortex Rainstorm Process Influenced by the Eastward Movement of Tibetan Plateau Vortex

<div>Maximum radar reflectivity for merging of precipitation clouds A and B on June 27: (a, e) 21:00 UTC; (b, f) 21:30 UTC; (c, g) 22:00 UTC; (d, h) 22:30 UTC (unit: dBz).</div>

Advances in Meteorology

fig11

Figure 11

Figure 11: Numerical Study of a Southwest Vortex Rainstorm Process Influenced by the Eastward Movement of Tibetan Plateau Vortex 