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Xiang Ni, Chuntao Liu, and Edward Zipser

geographical distribution of median microphysical parameters at 12 km is shown in Fig. 8 . Consistent with high DFR values in Fig. 3b , values of D m over land are typically larger than those over ocean ( Fig. 8a ). G. M. Heymsfield et al. (2010) examined vertical updrafts of different types of tropical deep convection using airborne observations. Results showed that the maximum updrafts of continental convection are stronger than oceanic convection above 10 km. Figure 8 shows larger particle sizes

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