Abstract
To limit global warming to below 2 °C by 2100, CO2 removal from the atmosphere will be necessary. One promising method for achieving CO2 removal at scale is ocean alkalinity enhancement (OAE), but there are challenges with incomplete air–sea CO2 equilibration, which reduces the efficiency of carbon removal. Here, we present global maps of OAE efficiency, and assess the seasonal variation in efficiency. We find that the equilibration kinetics have two characteristic timescales: rapid surface equilibration followed by a slower second phase, which represents the re-emergence of excess alkalinity that was initially subducted. These kinetics vary considerably with latitude and the season of alkalinity release, which are critical factors for determining the placement of potential OAE deployments. Additionally, we quantify the spatial and temporal scales of the induced CO2 uptake, which helps identify the requirements for modelling OAE in regional ocean models.
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Data availability
The data of the CESM2 simulation output (the primary dataset in this study) are archived in analysis-ready cloud-optimized format (https://ieeexplore.ieee.org/abstract/document/9354557) in an open access AWS bucket kindly provided by Source Cooperative, and can be found at https://beta.source.coop/repositories/cworthy/oae-efficiency-atlas/. The CESM2 netCDF output files and a sidecar file of icechunk references are provided, which allow the entire dataset to be accessed via the Zarr protocol. This data availability facilitates the interpretation and extension of the research in this article, via parallel analysis of the entire dataset (∼200 TB of data when uncompressed) by accessing it as a single Xarray dataset (https://openresearchsoftware.metajnl.com/articles/10.5334/jors.148). Instructions for doing so can be found in the README.md file included with the data.
Code availability
The code for simulating OAE in CESM2 and data analysis are available on Zenodo (https://doi.org/10.5281/zenodo.13900162)31.
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Acknowledgements
This material is based on work supported by the National Center for Atmospheric Research, a major facility sponsored by the National Science Foundation under cooperative agreement no. 1755088. Any opinions, findings, conclusions or recommendations expressed in this material do not necessarily reflect the views of the National Science Foundation (NSF). We acknowledge high-performance computing support from Cheyenne (https://doi.org/10.5065/D6RX99HX) provided by the National Center for Atmospheric Research (NCAR) Computational and Information Systems Laboratory, sponsored by the NSF. This research used resources of the National Energy Research Scientific Computing Center, which is supported by the Office of Science of the US Department of Energy under contract no. DE-AC02-05CH11231. [C]Worthy acknowledges support from the Grantham Foundation for the Environment, Founders Pledge, the Chan Zuckerberg Initiative, ClimateWorks Foundation and Stripe. M.Z. acknowledges support from NSF grant no. OCE-1924270 awarded to J. Granger and S. Siedlecki at the University of Connecticut.
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M.C.L., M.Z. and M.D.T. conceptualized the numerical experiments. M.C.L. and M.Z. performed the CESM2 model simulations to generate the underlying data. M.D.T. designed the box model. M.Z. and M.D.T. produced the figures. T.N. made the dataset publicly accessible. All authors contributed to the writing of the text. M.Z. and M.D.T. contributed equally to this work.
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Nature Climate Change thanks the anonymous reviewers for their contribution to the peer review of this work.
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Supplementary information
Supplementary Information
Supplementary Figs. 1–11 and Discussion.
Supplementary Video 1
Evolution of surface pCO2 deficit, OAE efficiency and vertical distribution of excess ALK, for the simulated OAE experiments near Greenland.
Supplementary Video 2
Evolution of surface pCO2 deficit, OAE efficiency and vertical distribution of excess ALK, for the simulated OAE experiments in the Subpolar North Atlantic.
Supplementary Video 3
Evolution of surface pCO2 deficit, OAE efficiency and vertical distribution of excess ALK, for the simulated OAE experiments in the Subtropical North Atlantic.
Supplementary Video 4
Evolution of surface pCO2 deficit, OAE efficiency and vertical distribution of excess ALK, for the simulated OAE experiments in the Equatorial North Atlantic.
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Zhou, M., Tyka, M.D., Ho, D.T. et al. Mapping the global variation in the efficiency of ocean alkalinity enhancement for carbon dioxide removal. Nat. Clim. Chang. 15, 59–65 (2025). https://doi.org/10.1038/s41558-024-02179-9
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DOI: https://doi.org/10.1038/s41558-024-02179-9
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