EGU26-18069, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-18069
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 11:35–11:45 (CEST)
 
Room 0.31/32
Future intensification of severe multi-hazard supercells in a semi-arid environment of Southern Europe
Carlos Calvo-Sancho1, Juan Jesús González-Alemán2, Amar Halifa-Marín3,4, María Luisa Martín5,6, and Cesar Azorin-Molina1
Carlos Calvo-Sancho et al.
  • 1Centro De Investigaciones sobre Desertificación – CSIC, Moncada (Valencia), Spain (carlos.calvo@csic.es)
  • 2Spanish State Meteorological Agency (AEMET), Department of Science, Spain.
  • 3Instituto Pirenaico de Ecología, Consejo Superior de Investigaciones Científicas (IPE-CSIC), 50059 – Zaragoza, Spain.
  • 4Laboratorio de Climatología y Servicios Climáticos (LCSC), CSIC-Universidad de Zaragoza, Spain
  • 5Department of Applied Mathematics. Faculty of Computer Engineering, Universidad de Valladolid, Spain.
  • 6Interdisciplinary Mathematics Institute. Universidad Complutense de Madrid, Spain.

Severe convective storms capable of producing extreme surface impacts simultaneously (such as large hailstones, strong winds, and heavy rainfall) present a major challenge to numerical weather prediction and risk assessment. On 6 July 2023, the Ebro Valley (Aragon, Spain) was impacted by a series of two high-impact supercells. The first supercell exhibited an extraordinary multi-hazard nature, producing a 50-km swath of giant hail (≥ 10 cm), a tornado, and a downburst with estimated gusts exceeding 200 km/h. The second supercell triggered flash flooding in the city of Zaragoza (population > 700,000) and large hail (> 5 cm) to the south of the city.

This study applies a sub-km-scale pseudo-global warming storyline approach to this compound high-impact event to quantify how anthropogenic climate change will alter its physical drivers and destructive potential. We downscale global climate perspectives to the storm scale by comparing a factual simulation with a future scenario (SSP5-8.5). We perturb initial and boundary conditions using climate change deltas derived from each CMIP6 climate model. We focus on the physical understanding of cascading hazards: specifically, whether future warming enables a transition towards storms that sustain giant hail growth while simultaneously enhancing precipitation efficiency (flash flood risk) and downdraft intensity. Our results aim to demonstrate how event-based storylines can unravel the interactions between thermodynamic changes and storm dynamics, revealing if such unprecedented multi-hazard supercells will become the new reality for extremes in semi-arid regions, thereby amplifying their destructive potential.

How to cite: Calvo-Sancho, C., González-Alemán, J. J., Halifa-Marín, A., Martín, M. L., and Azorin-Molina, C.: Future intensification of severe multi-hazard supercells in a semi-arid environment of Southern Europe, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-18069, https://doi.org/10.5194/egusphere-egu26-18069, 2026.