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

Figure 9

Longitude-height cross section of rain and snow mixing ratio at 32.1°N; the mixing ratio of rain is represented by shade color; the mixing ratio of snow 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) 13:00; (b) 13:30; (c) 14:00; (d) 15:00; (e) 15:30; (f) 16:00; (g) 17:00; (h) 18:00; (i) 19:00; (j) 20:00; (k) 21:00; (l) 22:00.