Numerical Simulation of the Effect of Cloud Condensation Nuclei Concentration on the Microphysical Processes in Typhoon Usagi

Figure 5

Comparison of radar maximum reflectivity in C10 (a), C1000 (b), and C100 (c) runs with observation (d) at 0000 UTC on 22 September. The radar observation is sourced from the China Weather News.

(a)

(b)

(c)

(d)