Abstract: This paper discusses application of an inlay-mesh model to the Meiliang Lake Area's wind-driven currents in the cases of various wind regimes.The results showed that the water of Taihu Lake flows into Meiliang Lake in the case of the windS,the water of Meiliang Lake flows into Taihu Lake in the case of the wind Nduring the early period of wind forcing,and that stable wind-driven current is the clockwise cyclic gyres in the case of Sand E wind direction,and the counterclock-wise cyclic gyres in the N and W wind direction.The water exchange between Meiliang Lake and Zhushang Lake is separated by the reclamation of Mashang area,influencing the winddriven current types of Meiliang Lake,and causing water renewing to be decelerated.