Articles | Volume 6, issue 4
https://doi.org/10.5194/wcd-6-1107-2025
https://doi.org/10.5194/wcd-6-1107-2025
Research article
 | 
20 Oct 2025
Research article |  | 20 Oct 2025

Asymmetric response of Northern Hemisphere near-surface wind speed to CO2 removal

Zhi-Bo Li, Chao Liu, Cesar Azorin-Molina, Soon-Il An, Yang Zhao, Yang Xu, Jongsoo Shin, Deliang Chen, and Cheng Shen

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Cited articles

An, S.-I., Shin, J., Yeh, S.-W., Son, S.-W., Kug, J.-S., Min, S.-K., and Kim, H.-J.: Global cooling hiatus driven by an AMOC overshoot in a carbon dioxide removal scenario, Earths Future, 9, e2021EF002165, https://doi.org/10.1029/2021EF002165, 2021. 
Bichet, A., Wild, M., Folini, D., and Schär, C.: Causes for decadal variations of wind speed over land: Sensitivity studies with a global climate model, Geophysical Research Letters, 39, https://doi.org/10.1029/2012GL051685, 2012. 
Boucher, O., Halloran, P. R., Burke, E. J., Doutriaux-Boucher, M., Jones, C. D., Lowe, J., Ringer, M. A., Robertson, E., and Wu, P.: Reversibility in an Earth System model in response to CO2 concentration changes, Environmental Research Letters, 7, 024013, https://doi.org/10.1088/1748-9326/7/2/024013, 2012. 
Cao, L., Bala, G., and Caldeira, K.: Why is there a short-term increase in global precipitation in response to diminished CO2 forcing?, Geophysical Research Letters, 38, L06703, https://doi.org/10.1029/2011GL046713, 2011. 
Chemke, R., Zanna, L., and Polvani, L. M.: Identifying a human signal in the North Atlantic warming hole, Nature Communications, 11, 1–7, https://doi.org/10.1038/s41467-020-15285-x, 2020. 
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Our research explores how Northern Hemisphere near-surface wind speeds respond to the removal of CO2 from the atmosphere. Using advanced CESM (Community Earth System Model) simulations, we discovered that wind speeds react differently during periods of increased and decreased carbon dioxide levels. Different responses are attributed to changes in global surface temperature and AMOC (Atlantic Meridional Overturning Circulation). This study not only advances our understanding of climate dynamics but also aids in optimizing strategies for wind energy.
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