Observations reveal that the wintertime southern hemisphere stratospheric polar vortex is modulated by the phase of the equatorial quasi-biennial oscillation (QBO). The high-latitude southern stratosphere is shown to be slightly colder throughout the winter, and the final warming occurs later, when the QBO is in its west phase. During May--October, the modulation of winds by the QBO is confined to midlatitudes, at the edge of the polar vortex. The difference between west and east phase composites of zonal mean wind during November, at the time of the final warming in the southern hemisphere, exceeded 14 ms-1. This difference is very similar to that in January in the northern hemisphere. While northern hemisphere QBO effects are optimized using equatorial winds near 40 hPa, southern hemisphere effects are best seen using ~25 hPa winds. ¿ 1998 American Geophysical Union