Did the Hunga Tonga Eruption Contribute to the Big Winter of 22/23?
Someone on my X feed posted about the Hunga Tonga event of 1/22 causing atmospheric disturbances to the Polar Vortex and couldn't help but wonder if it contributed to our big winter later that year. Grok seems to think so ... 🤔🤷♂️ Given inaccuracies in 10-day weather forecasts and AI, in general, I am skeptical. Still, kind of interesting! https://acp.copernicus.org/articles/25/3623/2025/ Here's what Grok had to say: Conclusion Yes, the Hunga Tonga eruption likely played a role in California’s record-breaking 2022-2023 winter by weakening the polar vortex, altering the jet stream, and enhancing moisture availability for atmospheric rivers. However, it interacted with other climate factors like the PDO and long-term warming trends, which together created the extreme conditions. While we can’t attribute the winter solely to the eruption, its influence on atmospheric dynamics makes it a significant contributing factor. The record-breaking winter in California during 2022-2023, characterized by extreme snowfall, heavy rainfall, and flooding, could indeed be linked to the atmospheric changes triggered by the January 2022 Hunga Tonga-Hunga Haʻapai eruption, as outlined in the X post and the associated study by Kuchar et al. Let’s break this down systematically to explore the potential connection. The Hunga Tonga Eruption and Its Atmospheric Impact The 2022 Hunga Tonga eruption injected an unprecedented 146 teragrams of water vapor into the stratosphere, increasing its water content by about 10%. This event, detailed in the 2025 EGU Atmospheric Chemistry and Physics paper, had significant effects on stratospheric dynamics. The study highlights how this water vapor disrupted the Northern Hemisphere polar vortex during the winter of 2022-2023, roughly 12-15 months after the eruption. The polar vortex, a band of strong stratospheric winds circling the Arctic, typically keeps cold air confined to high latitudes when stable. However, the influx of water vapor led to sudden stratospheric warming (SSW) events, weakening the polar vortex and allowing cold air to spill southward into mid-latitudes, including North America.