Plinius Conference Abstracts
Vol. 18, Plinius18-3, 2024, updated on 11 Jul 2024
https://doi.org/10.5194/egusphere-plinius18-3
18th Plinius Conference on Mediterranean Risks
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 02 Oct, 12:00–12:15 (CEST)| Lecture room

Attribution of the destructive Mediterranean derecho in 2022 to anthropogenic warming

Juan Jesus González-Alemán1, Damián Insua-Costa2,3, Eric Bazile4, Sergi González-Herrero5, Mario Marcello Miglietta6,7, Pieter Groenemeijer8, and Markus G. Donat9
Juan Jesus González-Alemán et al.
  • 1Department of Development and Applications, Spanish State Meteorological Agency, Madrid, Spain
  • 2Hydro-Climate Extremes Lab (H-CEL), Ghent University
  • 3CRETUS, Non-linear Physics Group, Universidade de Santiago de Compostela, Galicia, Spain
  • 4CNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France
  • 5WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland
  • 6University of Bari, Department of Earth and Geoenvironmental Sciences, Bari, Italy (m.miglietta@isac.cnr.it)
  • 7CNR-ISAC, Padua, Italy
  • 8European Severe Storms Laboratory, Wessling, Germany
  • 9Barcelona Supercomputing Center, and Institució Catalana de Recerca i Estudis Avançats, Barcelona, Spain

An extremely intense and organized convective storm, classified as a “derecho”, developed over the western Mediterranean Sea on August 18, 2022. The system affected Corsica, northern Italy, and Austria, with wind gusts up to 62 m/s and giant hailstones (diameter of around 11 cm), being responsible for 12 fatalities and 106 injured people.

The derecho developed over an extreme and persisting marine heatwave over the western Mediterranean. Therefore, the hypothesis of a relationship between the atmospheric event and the marine heatwave rapidly arose, suggesting a possible link with anthropogenic climate change.

By performing model simulations with both the Model for Prediction Across Scales (MPAS) and the nonhydrostatic operational AROME model and using the pseudo-global warming approach, we find a relationship between the marine heatwave, the actual anthropogenic climate change conditions, and the development of this extremely rare and severe convective event. These results suggest the increase of probability of development of similar events with respect to the past associated to climate change, and illustrate how climate change effects can cascade through a chain of extreme weather and climate events.

 

How to cite: González-Alemán, J. J., Insua-Costa, D., Bazile, E., González-Herrero, S., Miglietta, M. M., Groenemeijer, P., and Donat, M. G.: Attribution of the destructive Mediterranean derecho in 2022 to anthropogenic warming, 18th Plinius Conference on Mediterranean Risks, Chania, Greece, 30 Sep–3 Oct 2024, Plinius18-3, https://doi.org/10.5194/egusphere-plinius18-3, 2024.