Irreversible glacier change and trough water for centuries after overshooting 1.5 °C

Exceeding 1.5 °C of global warming above pre-industrial levels has become a distinct possibility, yet the consequences of such an overshoot for mountain glaciers and their contribution to raising sea levels and impacting water availability are not well understood. Here we show that exceeding and then returning to below 1.5 °C will have irreversible consequences for glacier mass and runoff over centuries. Global climate and glacier simulations project that a 3.0 °C peak-and-decline scenario will lead to 11% more global glacier mass loss by 2500 compared with limiting warming to 1.5 °C without overshooting. In basins where glaciers regrow after peak temperature, glacier runoff reduces further than if the glaciers stabilize, a phenomenon we call 'trough water'. Half the studied glaciated basins show reduced glacier runoff with overshoot compared with without for decades to centuries after peak warming. These findings underscore the urgency of near-term emissions reductions and limiting temperature overshoot.

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Publication Details

Journal
Nature Climate Change
Published
2025-05-19
DOI
https://doi.org/10.1038/s41558-025-02318-w
Citations
9
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
11.71

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article

Irreversible glacier change and trough water for centuries after overshooting 1.5 °C

Fabrice Lacroix, Carl‐Friedrich Schleussner, Patrick Schmitt, David R. Rounce et al.
9 citations
Nature Climate Change
Cryospheric studies and observations
11.71
article

Irreversible glacier change and trough water for centuries after overshooting 1.5 °C

Fabrice Lacroix, Carl‐Friedrich Schleussner, Patrick Schmitt, David R. Rounce, Thomas Lukas Frölicher, Lilian Schuster, Lizz Ultee, Fabien Maussion
article en
9 citations

Abstract

Exceeding 1.5 °C of global warming above pre-industrial levels has become a distinct possibility, yet the consequences of such an overshoot for mountain glaciers and their contribution to raising sea levels and impacting water availability are not well understood. Here we show that exceeding and then returning to below 1.5 °C will have irreversible consequences for glacier mass and runoff over centuries. Global climate and glacier simulations project that a 3.0 °C peak-and-decline scenario will lead to 11% more global glacier mass loss by 2500 compared with limiting warming to 1.5 °C without overshooting. In basins where glaciers regrow after peak temperature, glacier runoff reduces further than if the glaciers stabilize, a phenomenon we call 'trough water'. Half the studied glaciated basins show reduced glacier runoff with overshoot compared with without for decades to centuries after peak warming. These findings underscore the urgency of near-term emissions reductions and limiting temperature overshoot.

Nature Climate ChangeVol. 15(6)
University of Bern (CH), Oeschger Centre for Climate Change Research (CH), Goddard Space Flight Center (US), Bern University of Applied Sciences (CH), International Institute for Applied Systems Analysis (AT), Universität Innsbruck (AT), At Bristol (GB), University of Bristol (GB), Humboldt-Universität zu Berlin (DE), Carnegie Mellon University (US), Morgan State University (US)
National Science Foundation, National Aeronautics and Space Administration, European Commission, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Österreichischen Akademie der Wissenschaften, Nuclear Safety and Security Commission, Medizinische Universität Innsbruck, Universität Innsbruck, Horizon 2020 Framework Programme
Life below water
Openalex Percentile: Top 1%
Cryospheric studies and observations
11.71
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