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264 mm was observed at Shimoigusa over 9 h from 2000 to 0500 JST on 4–5 September ( Fig. 8 ). The Myoshoji River a branch of the Arakawa River, overflowed and more than 5000 houses were flooded up to their floorboards. Fig . 8. Accumulated rainfall amount during 1200–0600 JST 4–5 Sep 2005 observed by the Tokyo metropolitan government. b. Observational data Observations used in the experiment consisted of RW and reflectivity observed by the HANEDA and NARITA airport radars, GPS-PWV observed by GPS
264 mm was observed at Shimoigusa over 9 h from 2000 to 0500 JST on 4–5 September ( Fig. 8 ). The Myoshoji River a branch of the Arakawa River, overflowed and more than 5000 houses were flooded up to their floorboards. Fig . 8. Accumulated rainfall amount during 1200–0600 JST 4–5 Sep 2005 observed by the Tokyo metropolitan government. b. Observational data Observations used in the experiment consisted of RW and reflectivity observed by the HANEDA and NARITA airport radars, GPS-PWV observed by GPS
