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

Figure 1

Comparison of 24 h accumulated precipitation in C10 (a), C1000 (b), and C100 (c) runs with observations (d) at 0000 UTC on 23 September.

(a)

(b)

(c)

(d)