Simulations of the thermally induced breeze involved with a relatively narrow, elongated water body is presented in conjunction with evaluations of sensible heat fluxes in a stable marine atmospheric surface layer. The effect of the water surface temperature and of the large-scale synoptic winds on the development of surface flows over the water is examined. As implied by the sensible heat flux patterns, the simulation results reveal the following trends: (1) When the synoptic flow is absent or light, the induced surface breeze is not affected noticeably by a reduction of the water surface temperature; (2) for stronger synoptic flow, the resultant surface flow may be significantly affected by the water surface temperature.