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Antarctic Winter Heats Up Dramatically
25 Apr
Summary
- East Antarctica saw temperatures rise 28°C above average in July/August 2024.
- A weakening polar vortex and atmospheric river fueled the extreme winter heat.
- Antarctic heatwaves contribute to global sea level rise affecting coastlines.

During the Antarctic winter of July and August 2024, extreme warming occurred, with temperatures in East Antarctica rising by as much as 28°C above average for over two weeks. This significant anomaly was not mere weather but a rare atmospheric disturbance amplified by human-caused climate change, offering a preview of future events. The heatwave was initiated by a distortion of the Antarctic polar vortex, allowing stratospheric warming and the subsequent development of a persistent high-pressure system.
This system facilitated the intrusion of a warm, moisture-rich atmospheric river deep into the continent, transporting heat from lower latitudes. Accompanying clouds trapped surface heat, prolonging the event. Unusually warm Southern Ocean temperatures and record low sea ice likely contributed. Computer simulations indicate climate change made this heatwave significantly more probable and intense.
The consequences of such Antarctic heatwaves extend globally. Antarctica's ice sheets store most of the world's freshwater. Warming can affect snowfall, melting, and the stability of ice shelves, which in turn impacts glacier acceleration into the ocean and global sea level rise. These events highlight how climate change is altering extreme weather patterns worldwide.