A preliminary result of evaluation of our new mesocyclone detection algorithm (MRI-MDA) using real data will be presented. We applied our algorithm to one-year data taken from four terminal Doppler weather radars in Japan. Although not all detected meso-vortex-signatures were mesocyclones, statistics on meso-vortex-signatures is very useful to know algorithm performance. It is found that meso-vortex-signatures were detected over 30 days in the year. Core diameters, rotational velocities, and depth of rotations showed similar characteristics of those found in mini-supercells in the US. There were four tornadoes within the observation area in the 2004. Mesocyclone were observed prior to two tornadoes, and simultaneously for one tornado, and not observed for one tornado. Lead times of the two tornadoes were 17 and 35 minutes respectively.