Abstract
The current status of convection-permitting regional climate models is reported. First, the outline of regional climate models is described. Next, the representation of clouds in regional climate models is mentioned. Subsequently, the performance of numerical simulations using convection-permitting regional climate models is presented. In particular, the effects of high-resolution topography on the performance of simulations are discussed. Finally, an example of future climate projections using convection-permitting regional climate models is introduced.
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