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

Figure 6

Vertical distribution of absolute vorticity 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) 14:30; (j) 15:00; (k) 15:10; (l) 15:30; (m) 16:30; (n) 17:30; (o) 19:10; (p) 21:30.