Extreme climate issues might still happen even under 2ºC warming

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Originally, climate scientists believed some of the more extreme climate hazards were only likely to happen if we blew past the 1.5ºC limit and ended up in the 3ºC or 4ºC window. Here, new research from European scientists suggests that these big issues, such as severe drought, fires and intense rainfall might still happen, even under the moderate increase of 2ºC. The team say past assessments would look at global averages to predict the future of our climate, but in this study the team instead looked at how the temperature change can affect specific systems, such as our cities, forests or crop growing regions. They say that heavy rainfall in populated areas could increase by 4–15%, with their worst‑case 2ºC predictions, as well as a quarter of their models suggesting we would see drought conditions in major crop-producing regions that would actually surpass the average projections for 4ºC of warming.

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From: Springer Nature

Extreme global climate outcomes possible under moderate warming

Extreme climate hazards may occur under moderate 2 ºC warming at levels predicted for higher degrees of warming, a study in Nature finds. The research shows that severe drought, fire‑weather conditions and intense rainfall could threaten food production, forests and densely populated urban areas even exceeding the average projections typically associated with 3 ºC or 4 ºC of warming. The findings underscore the need for governments and institutions to prepare for plausible worst‑case scenarios, even under ’moderate’ levels of warming.

Climate assessments often rely on global and multimodel averages to communicate the most likely future climate. However, these averages do not capture how climate change affects specific systems, such as cities, forests or crop‑growing regions, and may mask large differences between individual climate models. This variability obscures the possibility that extreme rainfall, widespread drought, or dangerous fire‑weather conditions could arise under lower warming than projected. As warming approaches 1.5 ºC, understanding these credible worst‑case futures is essential for effective risk management and climate‑mitigation planning.

To provide a clearer picture of these risks, Emanuele Bevacqua and colleagues focus on climate hazards in some of the real‑world systems most vulnerable to change. They examine complete model simulations for specific climate‑sensitive areas; heavy rainfall in populated regions, drought across global breadbaskets, and fire‑weather conditions in forests. The authors find that individual climate models at 2 ºC project outcomes that are more extreme than the multimodel‑mean projections at 3 ºC or even 4 ºC. Under sector-specific analysis, heavy rainfall in populated areas could be projected to increase by 4–15%, with the worst‑case 2 ºC model exceeding the average outcome at 3 ºC. Additionally, 10 out of 42 models show drought conditions in major crop‑producing regions that surpass the average projections for 4 ºC, with drought frequency potentially rising by more than 50%.

These findings suggest that relying solely on multimodel averages could lead to the underestimating of the severity and timing of climate impacts across globally critical systems. As policymakers refine mitigation plans and organizations prepare for future climate risk, understanding and stress‑testing against these realistic worst‑case scenarios will be crucial.

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Nature
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Organisation/s: Helmholtz Centre for Environmental Research - UFZ, Germany
Funder: Open access funding provided by Helmholtz-Zentrum für Umweltforschung GmbH - UFZ. E.B. received funding from the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) via the Emmy Noether Programme (grant ID 524780515). This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement number 101003469. J.Z. acknowledges the Helmholtz Initiative and Networking Fund (Young Investigator Group COMPOUNDX, Grant Agreement VH-NG-1537). We acknowledge A. Bastos and M. Anand for support with the re-gridding of the European Space Agency Land Cover dataset via the LC-CCI user tool, and F. Gaupp for making available the crop-region definitions. We acknowledge the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP6, and thank the climate modelling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies that support CMIP and the ESGF. Analyses were carried out on the high-performance computing cluster EVE, a joint effort of both the Helmholtz Centre for Environmental Research - UFZ and the German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig.
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