Research Article

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

Figure 7

The regional time-averaged vertical profiles of total latent heating rate (K·h−1) in C10 (a), C100 (b), and C1000 (c) runs from 1200 UTC to 1800 UTC on 22 September.
(a)
(b)
(c)