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

<div>The AE of rainfall intensity between the values measured at the sites and the simulated results from the four numerical experiments: (a) Event A; (b) Event B.</div>

Advances in Meteorology

fig10

Figure 10

Figure 10: Effect of Data Assimilation Using WRF-3DVAR for Heavy Rain Prediction on the Northeastern Edge of the Tibetan Plateau 