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Previous studies suggest that the low-frequency background makes an important contribution to the predictability of tropical cyclone (TC) activity on the intraseasonal time scale by providing large-scale conditions favorable for TC formation. Extended numerical experiments were conducted to demonstrate additional low-frequency influence on TC activity, which results from the development of a synoptic-scale wave train. The cyclonic circulation of the wave train provides low-level synoptic-scale disturbances for TC formation. The observed TC formation events over the western North Pacific during 14 August-10 September 2004 were first successfully simulated with the initial and lateral conditions derived from the National Centers for Environmental Prediction (NCEP) Final (FNL) Operational Global Analysis. Then the 27-day extended experiment was repeated only with the initial and lateral boundary conditions derived from the FNL low-frequency (longer than 20 days) background. It is found that the development of the synoptic-scale wave train can be well simulated with TCs forming in the cyclonic circulations of the wave train although the wavelength of the simulated wave train is substantially reduced in the absence of higher-frequency influences with periods shorter than 20 days. Sensitivity experiments indicate that the development of wave trains is sensitive to the initial monsoon trough structure. This study suggests that the synoptic-scale wave train can develop in situ and does not need upstream precursors. [ABSTRACT FROM AUTHOR]