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Increase in European summer heatwaves driven by greenhouse gases and amplified by aerosol emission reductions

Abstract:
More frequent heatwaves in Europe are posing considerable risks to human health, infrastructure, and ecosystems. However, the contributions of external forcing factors such as well-mixed greenhouse gases (GHGs) and aerosols remain to be better quantified. Here, using model outputs from the Large Ensemble Single Forcing Model Intercomparison Project (LESFMIP), a recent atmospheric reanalysis and a machine learning method—self-organising maps (SOMs), we attribute European heatwave trends during 1940–2020 to various external forcings. The Europe-averaged heatwave trend during 1940–2020 (0.87 days per decade) is well captured by the multi-model mean (MMM) response with GHGs dominating the trend. The positive heatwave trend in GHGs and ozone is offset by the effects of aerosols during 1940–1979, leading to weak negative heatwave trends. In contrast, the increase in GHGs has driven about half (53 ± 17%; MMM and model-spread) of the strong heatwave trends in 1980–2020 (2.5 days per decade), amplified by the reduction in aerosols (23 ± 15%). This highlights the increasing risk of more frequent heatwaves in Europe if GHG emissions continue to rise without significant mitigation measures. Analysis of atmospheric circulation by SOMs reveals that four major atmospheric circulation patterns, dominated by a blocking high anomaly, are linked to the most spatially-intense European summer heatwaves. A relatively large increase in the occurrence of blocking-like atmospheric circulation has likely exacerbated heatwave trends in Southern and Eastern Europe in 1980–2020. However, this atmospheric circulation trend is much weaker in the model response, and also seems to be outside the internal variability in most of the models. This may partly explain the underestimated heatwave trends in Southern and Eastern Europe. Constraining and further understanding of the thermodynamic and dynamic response in the LESFMIP models is important for attributing and predicting the multi-annual and decadal variability of climate and weather extremes.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1088/1748-9326/ae6d18

Authors

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Institution:
University of Oxford
Role:
Author
ORCID:
0009-0003-9197-8281
More by this author
Institution:
University of Oxford
Role:
Author
ORCID:
0000-0002-9433-8066
More by this author
Institution:
University of Oxford
Role:
Author
ORCID:
0000-0002-8751-1211


Publisher:
IOP Publishing
Journal:
Environmental Research Letters More from this journal
Volume:
21
Issue:
11
Pages:
114008
Article number:
114008
Publication date:
2026-06-04
Acceptance date:
2026-05-13
DOI:
EISSN:
1748-9326
ISSN:
1748-9326


Language:
English
Keywords:
Source identifiers:
4113242
Deposit date:
2026-06-04
ARK identifier:
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