Here an idealized atmospheric circulation model is used to simulate SFW events, focusing on the mechanisms for stratosphere-troposphere coupling during spring onset. When the radiative equilibrium temperature in the stratosphere is gradually changed from a winter to a spring state, while the radiative forcing of the troposphere is held fixed, the model generates realistic SFW events. Composites of the model SFWs are generated, as well as anomalies from these composites. The simulated spring onset date and zonal wind transition pattern of our preliminary results without topography are consistent with the SH observations. The zonal wind anomaly transition, however, is somewhat similar to NH observations in that a relatively weak but statistically significant zonal wind anomaly extends downward into the lower troposphere, even the surface. Eliassen-Palm flux analysis of model SFWs shows the presence of strong wave activity near the onset date, similar to the NH and SH observations. Additional dynamical analyses of these model SFWs will be presented, and their implications for understanding the observed downward influence of SFWs will be discussed.