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In this study, the effect of soil moisture on convective precipitation in humid region is investigated by numerical simulations. Based on the observed soil moisture within the Lake Biwa basin, two numerical simulations are carried out in mountainous region around the Lake Biwa on 15th Aug. 2001 (during the intensified observation period of the Lake Biwa Project). One of them has the wettest initial condition of soil moisture and the other has the driest initial condition of soil moisture in Aug. 2001. It is found that realistic difference of initial condition of soil moisture can affect convective precipitation in humid region significantly and the drier condition of soil moisture causes the larger amount of precipitation.

THE EFFECT OF SOIL MOISTURE ON CONVECTIVE PRECIPITATION OVER THE MOUNTAINOUS REGION IN JAPAN DURING THE SUMMER SEASON