Simulation of the Microphysical Processes and Effect of Latent Heat on a Heavy Rainfall Event in Beijing |
Figure 1 Comparison of radar echoes at a, b 0800 and c, d 1800 BST 21 July units: dBz in the a, c simulation and b, d observation, and accumulated rainfall amount at 0800 21 July to 0800 BST 22 July units: mm in the e simulation and f observation. |
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