In this study, we investigated the future changes in tropical cyclone (TC) activities using regional climate models (RCMs) forced by multi-global climate models (GCMs). The simulation experiments were conducted at a 25-km horizontal resolution over the Coordinated Regional Climate Downscaling Experiment (CORDEX)-East Asia (EA) domain. The ensemble mean method was applied to reduce the uncertainty of each single RCM. During the historical period (1981-2005), the ensemble mean of RCMs captured TC frequency comparable to observation data but simulated their intensity weakly. When comparing the near future (2026-2050) and far future (2076-2100) periods under the high emission scenario to the historical period, the RCMs exhibited a consistent feature: the core region of TC genesis migrated northward. As the genesis region shifted, the TC activities also moved northward to the mid-latitude. In addition, the extreme intensity of landfalling TCs had increased above 25 degrees N compared to the historical period. These results are related to environmental fields; increasing relative vorticity and specific humidity of 850 hPa and weakening of vertical wind shear over the mid-latitude due to higher sea surface temperature compared to the historical period.