EGU26-14729, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-14729
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 04 May, 09:20–09:30 (CEST)
 
Room D2
Attributing consecutive hot and dry compound events to climate change
Cristina Deidda1, Clair Barnes2, Carlo De Michele3, Patrick Willems4, Jakob Zscheischler5, and Wim Thiery1
Cristina Deidda et al.
  • 1Vrije Universiteit Brussel, Vrije Universiteit Brussel, Hydrology and Hydraulic Engineering, Bruxelles, Belgium
  • 2Grantham Institute, Imperial College London, London, United Kingdom
  • 3Politecnico di Milano, Department of Civil and Environmental Engineering, Milano, Italy
  • 4Hydraulics and Geotechnics Section, Department of Civil Engineering, KU Leuven, Leuven , Belgium
  • 5Helmholtz Centre for Environmental Research—UFZ, Department of Compound Environmental Risks, Leipzig, Germany

In recent years, an increasing frequency of heatwaves and drought events have been experienced, with growing socioeconomic and environmental impacts, particularly in the agricultural sector.  The occurrence of these compound extremes in consecutive years amplifies their effects, leading to greater economic losses. Consecutive droughts can significantly affect vegetation growth and place additional stress on agricultural systems. When hot and dry compound extremes occur over multiple years, their impacts become even more pronounced, as they hinder the recovery of crops and strongly affect agricultural productivity.

In this study, we explore the use of univariate, bivariate and temporal compound attribution to show how climate change is influencing the probability of single, compound, and consecutive extreme events. In particular, we propose a case study in Belgium to investigate how the probability of consecutive extremes is changing in a warmer climate. The aim of the study is to highlight the urgency of increasing attention on both the impact of the single events and the larger impacts that can be caused by the more frequent consecutive extremes and consecutive co-occurrent extremes. Finally, we discuss some of possible implications of these findings for policymakers and practitioners involved in climate adaptation and risk management.

How to cite: Deidda, C., Barnes, C., De Michele, C., Willems, P., Zscheischler, J., and Thiery, W.: Attributing consecutive hot and dry compound events to climate change, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-14729, https://doi.org/10.5194/egusphere-egu26-14729, 2026.