The performance of short-range precipitation forecasting with VDRAS analysis is investigated. Results indicate that an anelastic non-hydrostatic model in VDRAS works well for 2-hour nowcasting of the evolution of convections in this study. The limitation of lead times depends on the domain size and computation time. The domain is small (100 km x 100 km) because the outside of Tokyo area is mountainous and the application of VDRAS is favorable to flat areas. Such a small domain is easy affected by the boundary condition with the lapse of time. Basically, VDRAS has much capability in the real-time nowcasting in virtue of introducing Message Passing Interface (MPI). Some small-scale storms, however, need a higher horizontal resolution less than about 2 km, which causes difficulties for the real-time operation. We will also discuss on a framework of assimilating VDRAS analysis into WRF model analysis/forecast as one of remedies to extend the lead times up to around 6 hours. In some storm cases mainly due to the convergence of water vapor flux, the accurate water vapor analysis is crucial for the accurate retrieval. The usefulness of GPS precipitable water data from the Japanese dense GPS receiver network (GEONET) is discussed to modify the first-guess in the pre-processor of VDRAS as a final discussion. The combined use of data from different observing systems is promising to improve quantitativeness of precipitation forecasting.
 - Indicates paper has been withdrawn from meeting
 - Indicates paper has been withdrawn from meeting - Indicates an Award Winner
 - Indicates an Award Winner