Both the observation and simulation reveal the dry soil period (DSP) and wet soil period (WSP) with distinct characters in terms of net surface radiation, Bowen Ratio, PBL height, LCL, LFC, CAPE, CIN, mountain scale convergence and the diurnal evolution of PBL parameters. Results show that the increased soil moisture tends to suppress the PBL depth during the daytime as well as mountain-scale convergence, and a stable PBL makes it more difficult for cumulus convection. But, the moist static energy and CAPE are larger during WSP, which makes the convection to initiate earlier and last longer. The simulation successfully reveals the wet/dry soil periods and their characteristics, but the precipitation and soil moisture related parameters were less well captured in terms of magnitude and duration, which may lead to a different condition for PBL development and convection initiation.