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

Figure 10

Longitude-height cross section of graupel mixing ratio at 32.1°N; the mixing ratio of graupel is represented by solid lines (start value: 0.5 g/kg; interval: 1 g/kg); the updraft velocity is represented by shaded color; the thick dotted line is the 0°C isotherm on June 27: (a) 13:30; (b) 14:00; (c) 15:00; (d) 15:30; (e) 16:00; (f) 18:00; (g) 19:00; (h) 20:00; (i) 21:00.