In winter, the region of the stratosphere over the pole cools through radiative heat loss, establishing a strong meridional temperature gradient from equator to pole. This results in strong westerly winds developing around the cold core, a structure known as the stratospheric polar vortex (SPV) (e.g., Waugh et al., 2017). Sudden stratospheric warmings occur when the SPV rapidly breaks down during winter, with a frequency of around six times a decade in the northern hemisphere (Charlton & Polvani, 2007). In the southern hemisphere, only one major sudden stratospheric warming has ever been observed (e.g., Charlton et al., 2005), although the frequency of events in the southern hemisphere has been estimated at once every 25 years (Wang et al., 2020). During a sudden stratospheric warming, polar stratospheric temperatures can increase by up to 40K in a few days (Butler et al., 2015) and the zonal winds weaken, or reverse. The most common definition of major SSWs (hereafter SSW) is when the zonal-mean zonal winds at 10 hPa and 60°N become easterly (e.g., Charlton & Polvani, 2007