Articles | Volume 17, issue 5
https://doi.org/10.5194/esd-17-1573-2026
https://doi.org/10.5194/esd-17-1573-2026
Research article
 | 
23 Oct 2026
Research article |  | 23 Oct 2026

Unexpected land-surface warming following a relatively limited-forcing hypothetical nuclear war

Anson Ka Hei Cheung, Paul J. Kushner, Francesco S. R. Pausata, Zhihong Zhuo, and Marguerite L. Brown

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Cited articles

Bardeen, C. G., Kinnison, D. E., Toon, O. B., Mills, M. J., Vitt, F., Xia, L., Jägermeyr, J., Lovenduski, N. S., Scherrer, K. J. N., Clyne, M., and Robock, A.: Extreme ozone loss following nuclear war results in enhanced surface ultraviolet radiation, J. Geophys. Res.-Atmos., 126, https://doi.org/10.1029/2021JD035079, 2021. 
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Byrne, B., Liu, J., Bowman, K. W., Pascolini-Campbell, M., Chatterjee, A., Pandey, S., Miyazaki, K., van der Werf, G. R., Wunch, D., Wennberg, P. O., Roehl, C. M., and Sinha, S.: Carbon emissions from the 2023 Canadian wildfires, Nature, 633, 835–839, https://doi.org/10.1038/s41586-024-07878-z, 2024. 
Cheung, A.: Dataset for “Unexpected land-surface warming following a relatively limited-forcing hypothetical nuclear war”, Borealis, V3 [data set], https://doi.org/10.5683/SP3/UG2598, 2025. 
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If a nuclear war happened, firestorms induced by nuclear detonations in urban areas could inject black carbon (BC) into the upper atmosphere, disrupting global climate. We simulated the climate impacts of relatively limited-forcing scenarios using an Earth system model. In all scenarios, BC blocks sunlight, causes global cooling, and decreases precipitation for more than a decade. However, a drastic global warming emerges midway through the first year and lasts until the year's end.
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