Fig. 2From: 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 Schematic image of the grid structure of stretch-NICAM. The grid structure for g-level 4 is shown for readability. The actual grid used for the simulation is at g-level 9, whose grid can be obtained by subdividing the grid of g-level 4. Navy contours show the areas of the grid interval of g-level 9 at 1.5, 2, 3, 4, and 5Â km. b The calculation domains for ASUCA for the 5Â km mesh model (green) and the 1Â km mesh model (red)Back to article page