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Progress in Earth and Planetary Science
Fig. 6　 | Progress in Earth and Planetary Science

Fig. 6　

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. 6　

Radar observation by the Narita radar at 04:00 UTC, April 18, 2020. Top row: a horizontal distribution of radar reflectivity [dBZ] (elevation angle 0.7°), vertical cross sections of b radar reflectivity Zhh [dBZ] and c differential reflectivity Zdr [dB]. Bottom row: vertical cross sections of d cloud types, e specific differential phase Kdp [° km−1], and f copolar correlation coefficient ρhv. The vertical cross section is located along the straight line in the upper left figure (azimuth angle 239.5°)

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