The space-time features of major vorticity disturbances over the western North Pacific during the 1997-98 E1 Ni(?)o ranked as one of the strongest events on record was investigated in this study.We distinguished the different roles that these disturbances had on different timescales in causing the reversal or turnabout of the E1 Ni(?)o event.Remarkable differences in the various disturbances of synoptic,intraseasonal,and interannual timescales were found in the time evolution,propagation,and in their contributions to the changes in near- equatorial zonal flow,which was crucial to the demise of the warm sea surface temperature anomalies in the central-eastern Pacific.It is hypothesized that the westward-traveling synoptic and intraseasonal oscillations in the western North Pacific might be considered as a self-provided negative feedback from the E1 Ni(?)o and played an additional role in its reversal in comparison with other interannual internal and external forcings. In this case,the off-equatorial synoptic and intraseaonal fluctuations served as a stochastic forcing for the tropical ocean and gave rise to the aperiodicity or irregularity of the E1 Ni(?)o-Southern Oscillation. The space-time features of major vorticity disturbances over the western North Pacific during the 1997-98 E1 Ni (?) O ranked as one of the strongest events on record was investigated in this study.We distinguished the different roles that these disturbances had on different timescales in causing the reversal or turnabout of the E1 Ni (?) o event. Mark differential differences in the various disturbances of synoptic, intraseasonal, and interannual timescales were found in the time evolution, propagation, and in their contributions to the changes in near - equatorial zonal flow, which was crucial to the demise of the warm sea surface temperature anomalies in the central-eastern Pacific. It is hypothesized that the westward-traveling synoptic and intraseasonal oscillations in the western North Pacific might be considered as a self-provided negative feedback from the E1 Ni (?) o and played an additional role in its reversal in comparison with other interannual internal and external forcings. In this case, the o ff-equatorial synoptic and intraseaonal counts served as a stochastic forcing for the tropical ocean and gave rise to aperiodicity or irregularity of the E1 Ni (?) o-Southern Oscillation.