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

Figure 8

Longitude-height cross section of cloud droplet and ice crystal mixing ratio at 32.1°N; the mixing ratio of cloud droplets is represented by shade color; the mixing ratio of ice crystals is represented by solid lines (start value: 0.0001 g/kg; interval: 0.5 g/kg from 0.1 to 3.1 g/kg); the wind vector is represented by arrows; the thick dotted line is the 0°C isotherm on June 27: (a) 11:00; (b) 12:00; (c) 13:00; (d) 13:10; (e) 13:20; (f) 13:30; (g) 14:00; (h) 15:00; (i) 15:30; (j) 16:00; (k) 17:00; (l) 18:00; (m) 19:00; (n) 20:00; (o) 21:00; (p) 22:00.