Sudden stratospheric warmings (SSWs) are extreme cases of stratospheric polar vortex weakening [1].They are termed minor when a reversal of the stratospheric meridional temperature gradient in the subpolar region at 10 hPa and poleward of 60° occurs, or major when this is accompanied by a complete reversal of the stratospheric circumpolar westerly jet [2].Although SSWs occur in both hemispheres, major SSWs are usually observed in the Northern Hemisphere, with a frequency of approximately six per decade.In contrast, only one major SSW has been recorded in the Southern Hemisphere, which occurred in 2002 [3].