Zero emissions commitment depends on warming level

Abstract When anthropogenic CO 2 emissions cease, global temperature does not stabilize immediately. The resulting global temperature change, the zero emissions commitment, is central to carbon budget assessments and understanding reversibility of global warming, yet its dependence on prior warming levels remains unclear. Here we show, using zero-emission simulations with the UK Earth System Model (UKESM1.2) across global warming levels of 1.5–5 K, that the zero emissions commitment stays near zero up to 2 K but becomes positive at higher warming levels, reaching 0.4–0.6 K after ~ 150 years. This dependence indicates that stabilizing or reversing warming becomes progressively more difficult as peak temperature rises. We identify the mechanism behind this behaviour: stronger warming from higher radiative disequilibrium and weakening carbon sinks, driven by saturated land carbon uptake and the reduced radiative impact of CO 2 drawdown at higher background CO 2 concentrations. Higher peak warming therefore commits the planet to additional warming, limiting temperature-overshoot reversibility.

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Publication Details

Journal
Nature Climate Change
Published
2026-11-03
DOI
https://doi.org/10.1038/s41558-026-02776-w
Citations
2
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
4.80

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article

Zero emissions commitment depends on warming level

Ranjini Swaminathan, Timothy Andrews, CHRIS D. JONES, Jeremy P. R. B. Walton et al.
2 citations
Nature Climate Change
Climate variability and models
4.80
article

Zero emissions commitment depends on warming level

Ranjini Swaminathan, Timothy Andrews, CHRIS D. JONES, Jeremy P. R. B. Walton, Andrew J. Wiltshire, Robin S. Smith, Richard G. Williams, Andrea J. Dittus, L. de Mora, S. T. Rumbold, Eddy Robertson, Paulo Ceppi, Colin Jones, Laura Gibbs, Spencer Liddicoat
article en
2 citations

Abstract

Abstract When anthropogenic CO 2 emissions cease, global temperature does not stabilize immediately. The resulting global temperature change, the zero emissions commitment, is central to carbon budget assessments and understanding reversibility of global warming, yet its dependence on prior warming levels remains unclear. Here we show, using zero-emission simulations with the UK Earth System Model (UKESM1.2) across global warming levels of 1.5–5 K, that the zero emissions commitment stays near zero up to 2 K but becomes positive at higher warming levels, reaching 0.4–0.6 K after ~ 150 years. This dependence indicates that stabilizing or reversing warming becomes progressively more difficult as peak temperature rises. We identify the mechanism behind this behaviour: stronger warming from higher radiative disequilibrium and weakening carbon sinks, driven by saturated land carbon uptake and the reduced radiative impact of CO 2 drawdown at higher background CO 2 concentrations. Higher peak warming therefore commits the planet to additional warming, limiting temperature-overshoot reversibility.

Nature Climate Change
Met Office (GB), University of Leeds (GB), University of Liverpool (GB), University of Exeter (GB), Plymouth Marine Laboratory (GB), University of Bristol (GB), National Centre for Atmospheric Science (GB), National Centre for Earth Observation (GB), Imperial College London (GB), University of Reading (GB)
Government of the United Kingdom, UK Research and Innovation, European Commission, Met Office, HORIZON EUROPE Framework Programme, Natural Environment Research Council
Climate action
Openalex Percentile: Top 8%
Climate variability and models
4.80
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