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

<div>Spatial distribution of the rainfall accumulation for the durations of the two events shown in Thiessen polygons: (a) Event A; (b) Event B.</div>

Advances in Meteorology

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Figure 3

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