What is it about?
About 180 million years ago (the early Jurassic), there was a hyperthermal event due to rapidly increasing CO2. Geological evidence shows a large amount of strong-wind caused deposits at the coast of the Tethys ocean. Our climate simulations show that there were indeed super-hurricanes over the Tethys ocean as CO2 is 4 times of the present level.
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Why is it important?
The consistency between geological records and climate simulations indicates that hurricanes were intensified for CO2-induced warm world.
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This page is a summary of: Elevated atmospheric CO
2
drove an increase in tropical cyclone intensity during the early Toarcian hyperthermal, Proceedings of the National Academy of Sciences, July 2023, Proceedings of the National Academy of Sciences,
DOI: 10.1073/pnas.2301018120.
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