Effect of Data Assimilation Using WRF-3DVAR for Heavy Rain Prediction on the Northeastern Edge of the Tibetan Plateau

Figure 7

Differences between rainfall values measured at the sites and those from the numerical experiments for Event A: (a) CTRL; (b) DA-SAT; (c) DA-OBS; (d) DA-BOTH.

(a)

(b)

(c)

(d)