Preprints
https://doi.org/10.5194/egusphere-2025-4976
https://doi.org/10.5194/egusphere-2025-4976
27 Oct 2025
 | 27 Oct 2025
Status: this preprint is open for discussion and under review for Weather and Climate Dynamics (WCD).

A combined storyline-statistical approach for conditional extreme event attribution

Dalena León-FonFay, Alexander Lemburg, Andreas H. Fink, Joaquim G. Pinto, and Frauke Feser

Abstract. Quantifying the influence of anthropogenic global warming on extreme events requires both physical and statistical understanding. We present a framework combining two complementary conditional attribution methods: spectrally nudged storylines and flow-analogues. Applied to the 2018 Central European heatwave, storylines project an area-mean intensification of 1.7 °C per degree of global warming. Despite no detected changes in atmospheric blocking, the flow-analogue approach further indicates that heatwaves exceeding the storyline-projected intensities become far less rare at their corresponding warming levels than the factual 2018 event was under present conditions. Specifically, the 2018 heatwave, with an intensity of 2.2 °C and a return period of 1-in-277-years today, becomes a 6.6 °C event with a 1-in-26-year probability in a +4 K world. We conclude that this combined framework is promising for climate change attribution of individual extreme events, offering both a physical assessment of anthropogenic warming and its associated likelihood while accounting for potential shifts in atmospheric dynamics.

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Dalena León-FonFay, Alexander Lemburg, Andreas H. Fink, Joaquim G. Pinto, and Frauke Feser

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Dalena León-FonFay, Alexander Lemburg, Andreas H. Fink, Joaquim G. Pinto, and Frauke Feser
Dalena León-FonFay, Alexander Lemburg, Andreas H. Fink, Joaquim G. Pinto, and Frauke Feser

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Short summary
We combine physical (spectrally nudged storylines) and statistical (flow-analogue) methods to show how global warming affects the intensity and likelihood of historical extreme events. By conditioning on the circulation pattern, we minimize uncertainties linked to atmospheric dynamics. Using the 2018 Central European heatwave, we find that while the weather pattern remains equally likely, its intensity and frequency rise sharply with warming, making such events far more common in the future.
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