First crossings of global warming levels in CMIP6 in light of observed 1.5 °C exceedance

The year 2024 marked the first time global temperatures exceeded 1.5 °C, raising questions about climate projection accuracy and implications for climate goals. We quantify the timing and likelihood of first crossing 1.5 °C and higher global warming levels across CMIP6 models. The observed 2024 crossing occurred 3–7 years earlier than in CMIP6 projections. Models with high present-day warming rates predicted the timing of the 1.5 °C crossing more accurately, while the 2024 timing is likely affected by internal climate variability superimposed on the anthropogenic trend. A pre-mid-century 2 °C crossing is difficult to avoid even under stringent mitigation (75% of models crossing 2 °C under SSP1-2.6). However, while shifting from high (SSP5-8.5) to medium-high (SSP3-7.0) emissions delays a 3 °C crossing by 10 years, low-emission pathways (SSP1-2.6) avoid crossing this threshold in 85% of models. While near-term 2 °C exceedance is a significant risk, immediate mitigation remains critical to enable adaptation and avoid long-term warming.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2026-04-03
DOI
https://doi.org/10.1038/s41612-026-01401-z
Primary Topic
Atmospheric Ozone and Climate
Type
article
Field-Weighted Citation Impact
0.00

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article

First crossings of global warming levels in CMIP6 in light of observed 1.5 °C exceedance

Nora L. S. Fahrenbach, Joonas Merikanto, Antti Lipponen, Kalle Nordling
npj Climate and Atmospheric Science
Atmospheric Ozone and Climate
article

First crossings of global warming levels in CMIP6 in light of observed 1.5 °C exceedance

Nora L. S. Fahrenbach, Joonas Merikanto, Antti Lipponen, Kalle Nordling
article en

Abstract

The year 2024 marked the first time global temperatures exceeded 1.5 °C, raising questions about climate projection accuracy and implications for climate goals. We quantify the timing and likelihood of first crossing 1.5 °C and higher global warming levels across CMIP6 models. The observed 2024 crossing occurred 3–7 years earlier than in CMIP6 projections. Models with high present-day warming rates predicted the timing of the 1.5 °C crossing more accurately, while the 2024 timing is likely affected by internal climate variability superimposed on the anthropogenic trend. A pre-mid-century 2 °C crossing is difficult to avoid even under stringent mitigation (75% of models crossing 2 °C under SSP1-2.6). However, while shifting from high (SSP5-8.5) to medium-high (SSP3-7.0) emissions delays a 3 °C crossing by 10 years, low-emission pathways (SSP1-2.6) avoid crossing this threshold in 85% of models. While near-term 2 °C exceedance is a significant risk, immediate mitigation remains critical to enable adaptation and avoid long-term warming.

npj Climate and Atmospheric Science
Finnish Meteorological Institute (FI), ETH Zurich (CH)
National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Eidgenössische Technische Hochschule Zürich, Emil Aaltosen Säätiö
Climate action
Openalex Percentile: Top 20%
Atmospheric Ozone and Climate
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