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Jamshedpur areas of India on 26 May 2010. WRF Model with horizontal decision of nine km and 27 vertical eta degrees is administered for a length of 24 hours the use of NCEP-FNL statistics beginning from 0000 UTC of 26 April 2010 and 0000 UTC of 26 May 2010 as preliminary and boundary situations for the ones instances. YSU Planetary Boundary Layer parameterization scheme for boundary layer option, Rapid Radiative Transfer Model for lengthy wave and Dudhia for brief wave radiation scheme had been applied to run the version. Noah Land Surface Model and Kain-Fritsch cloud scheme also are taken into consideration withinside the Model. An attempt is made to simulate the ones instances via way of means of assimilating SYNOP and Upper Air statistics of Bangladesh and neighbourhood the use of WRF 3DVAR Data Assimilation approach in WRF Model. The simulated rainfalls (convective and non-convective) are as compared with TRMM 3B42RT product and rainfall statistics of Bangladesh Meteorological Department for validation procedure. The version outputs also are as compared with satellite tv for pc and RADAR imageries for validation and applied in explaining the improvement mechanism of the thunderstorms. The WRF Model merchandise like dBZ, rainfall depth, wind float sample, vertical
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