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

Figure 5

Distribution of absolute vorticity at 8 km on June 27: (a) 07:00; (b) 08:00; (c) 09:00; (d) 10:00; (e) 11:00; (f) 12:00; (g) 14:00; (h) 16:00; (i) 17:00; (j) 18:00; (k) 19:10; (l) 20:00.