Such events are rare in the Southern Hemisphere, and can weaken the vortex, while sending ripples across the entire atmospheric system.
Forecast models suggest that within two weeks the strength of the vortex could be cut nearly in half, even without a full reversal of winds, a threshold that typically defines a SSW event.
The anomaly is expected to peak by late September, with temperatures in the stratosphere rising as much as 50°C (90°F) above seasonal norms.
Unusually, this warming is also projected to descend to lower levels of the stratosphere,
At the surface, the South Pole pressure index is forecast to turn negative and stay that way, signaling disrupted polar circulation and the development of high-pressure ridging around Antarctica.
Such blocking patterns are known to push cold polar air outward, raising the risk of sudden cold surges into mid-latitude regions.
In the Southern Hemisphere, the disruption is expected to affect spring weather in South America, Australia, and New Zealand, potentially altering storm activity, rainfall distribution, and seasonal transitions.
“When the Southern Hemisphere’s tropospheric polar vortex is stronger than usual, cold air and powerful winds surrounding Antarctica typically contract towards the south,” said Ben Domasino of Weatherzone.
“The Southern Hemisphere’s polar vortex always weakens during spring as part of its normal seasonal cycle,” Domasino said.
“However, the stratospheric polar vortex has started to weaken faster than usual over the past week due to abnormally warm air entering the polar stratosphere. Some forecast models suggest that further stratospheric warming could occur through the middle of September as well.”
Domensino added that it is difficult to predict how each stratospheric warming episode will impact weather patterns closer to the ground, because such events are rare in the Southern Hemisphere and no two are the same. However, if the tropospheric polar vortex does weaken in the coming weeks, it will increase the likelihood of more frequent and stronger cold fronts over Australia during mid-to-late spring.
The impacts of this stratospheric warming may not be confined to the Southern Hemisphere as the two poles are connected through the Brewer–Dobson circulation, and disturbances in one can propagate into the other.
Extended high-pressure anomalies over the South Pole from August to October have also been associated with colder-than-average winters in the United States during December to February, while Europe often experiences the opposite effect, with warmer conditions than usual." W
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