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

Figure 7

Vertical distribution of relative humidity at 32.1°N on June 27: (a) 07:00; (b) 09:00; (c) 11:00; (d) 13:00; (e) 13:10; (f) 13:20; (g) 13:30; (h) 14:00; (i) 15:00; (j) 16:00; (k) 17:00; (l) 18:00; (m) 19:00; (n) 20:00; (o) 21:00; (p) 22:00.