Fig. 10From: Evaluation of cloud and precipitation processes in regional and global models with ULTIMATE (ULTra-sIte for Measuring Atmosphere of Tokyo metropolitan Environment): a case study using the dual-polarization Doppler weather radarsa The same as Fig. 6a, showing the horizontal distribution of radar reflectivity (elevation angle 0.7°) for the NICAM-NSW6 simulation. Vertical cross sections of specific density of b cloud water, c rain, d cloud ice, e snow, and f graupel. The contours in the cross section show the temperature [°C]. The hatched area indicates vertical velocity stronger than 1 m s−1Back to article page