Research Article
Cause Analysis on Eastward Movement of Southwest China Vortex and Its Induced Heavy Rainfall in South China
Figure 7
The distribution of pseudo equivalent potential temperature (K) and the advection (colored shaded in 10−5 K·s−1) at the vertical sections along (a) 104°E, (b) 105°E, and (c) 106°E; (d, f, and g) 25°N and (e) 24°N as well as the horizontal distribution of (h) averaged over 18 UTC June 10 to 18 UTC June 11, 2008, and (i) averaged over 18 UTC June 11 to 00 UTC June 13, 2008.
| (a) 0000 UTC 11 |
| (b) 1200 UTC 11 |
| (c) 0000 UTC 12 |
| (d) 0000 UTC 12 |
| (e) 1200 UTC 12 |
| (f) 0000 UTC 13 |
| (g) 1200 UTC 13 |
| (h) 700 hPa |
| (i) 700 hPa |