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Yasushi Fujiyoshi (ILTS, Hokkaido Univ., Japan)

The 8 th GAME International Science Panel Meeting GAME-II Cloud and Precipitation Process Working Group. Yasushi Fujiyoshi (ILTS, Hokkaido Univ., Japan). Cloud and Precipitation Process Working Group / GAME-II. Related Workshop ｓ 24 Mar. 2003: 1 st Meeting on Moist Convection

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Yasushi Fujiyoshi (ILTS, Hokkaido Univ., Japan)

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  1. The 8th GAME International Science Panel MeetingGAME-IICloud and Precipitation ProcessWorking Group Yasushi Fujiyoshi (ILTS, Hokkaido Univ., Japan)

  2. Cloud and Precipitation Process Working Group / GAME-II Related Workshopｓ 24 Mar. 2003: 1st Meeting on Moist Convection at Nagoya Univ., JAPAN 25-26 Aug. 2003: HUBEX meeting for publishing final report at Hokkaido Univ., JAPAN 29-31 Oct. 2003: The Second China-Japan Workshop on Heavy Rainfall Experiment and study　(at Wuhan, China) ? Feb. 2004: 2nd Meeting on Moist Convection 　　　　　　　　at Nagoya University ?) ? 2004: Planning: International meeting on cloud and precipitation

  3. Final Report of GAME/HUBEX (March, 2004) I Outline of HUBEX II Research background of HUBEX III Field report of heavy rainfall and flood during HUBEX IV Land surface processes V Source and transport of water vapor to Mei-yu front VI Mechanism of heavy rainfall VII Regional/Basin scale water/energy budget VIII River runoff and hydrological model IXYangtze river flood in 1998 X4DDA (Regional scale) data set of GAME/HUBEX XIToward forecasting of heavy rainfall and flood

  4. GAME/HUBEX 1998 &1999 When the area with latent instability is wide enough, a meso-α low is able to develop from convective systems. Latent Heat Organization and Scale-up

  5. Numerical simulation

  6. When the Mei-yu front moves toward the north of Huaihe River The south westerly moist air in the low altitude plays an important role for the development of precipitation systems.

  7. Shanghai Analyzed new data set : CHERES(973) (China) Yangtze-river Heavy rainfall (2001+2002)

  8. Tbb & Radar Reflectivity The convective system: developed rapidly within the observational network passed within the dual-Doppler analysis region

  9. Doppler Radar Range Moist easterly in the low altitudefrom the ocean plays an important role for the formation of convergence and convective cloud systems.

  10. Land surface Cloud & Precipitation New Target Cloud+aerosol Precipitation Moist Boundary Layer Expected New data sets ＊Boundary layer: Prof. Nakamura’s project (in China), Biwa-lake project Wind profiler, 3D-Doppler lidar, Aerosonde, Doppler Sodar, Microwave profiler, Aircraft observation, AWS, Cloud radar ＊ KEOP (Korea) ＊ MRI (Japan): Northern Kyusyu, water vapor transport (2003-2006)

  11. Related Project: CPEA (Coupling Processes in the Equatorial Atmosphere)- FORSGC (Indonesia)

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