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Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: 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 radars

Fig. 2

a 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 5 km. b The calculation domains for ASUCA for the 5 km mesh model (green) and the 1 km mesh model (red)

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