On the Rapid Intensification of Hurricane Wilma (2005) CBs may impact hurricane intensification by inducing compensating subsidence of the lower stratospheric air. We conclude that the development of more cbs inside the upper-level radius of maximum wind and the higher altitude of latent heating all appear to be 149.9 Kb. 3
On the Rapid Intensification of Hurricane Wilma (2005) CBs may impact hurricane intensification by inducing compensating subsidence of the lower stratospheric air. We conclude that the development of more cbs inside the upper-level radius of maximum wind and the higher altitude of latent heating all appear to be 152.26 Kb. 3