Fig. 6From: Large dependency of charge distribution in a tropical cyclone inner core upon aerosol number concentrationTemporal evolution of maximum wind velocity at z = 1 km as 150 min (min) moving averaged value with N0 = 10 cm−3 (green), N0 = 100 cm− 3 (red), and N0 = 1000 cm− 3 (blue)Back to article page