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Reservoir CO2 and CH4 emissions and their climate impact over the period 1900–2060

Nature Geoscience volume 15, pages 700–705 (2022)Cite this article

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Abstract

Reservoirs are essential for human populations, but their global carbon footprint is substantial (0.73–2.41 PgCO2-equivalent yr−1). Yet the temporal evolution of reservoir carbon emissions and their contribution to anthropogenic radiative forcing remains unresolved. Here we quantify the long-term historical and future evolution (1900–2060) of cumulative global reservoir area, carbon dioxide and methane emissions and the resulting radiative forcing. We show that global reservoir carbon emissions peaked in 1987 (4.4 TmolC yr−1) and have been declining since, due largely to decreasing carbon dioxide emissions as reservoirs age. However, reservoir-induced radiative forcing continues to rise due to ongoing increases in reservoir methane emissions, which accounted for 5.2% of global anthropogenic methane emissions in 2020. We estimate that, in the future, methane ebullition and degassing flux will make up >75% of the reservoir-induced radiative forcing, making these flux pathways key targets for improved understanding and mitigation.

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Fig. 1: Evolution of reservoir area.
Fig. 2: Reservoir emissions through time.
Fig. 3: Relative contribution of reservoirs to anthropogenic carbon emissions.
Fig. 4: Evolution of reservoir-induced RF.
Fig. 5: Relative contribution of RF of each reservoir flux pathway compared with global anthropogenic RF of combined C-GHGs, CO2 and CH4.

Data availability

Data and modelling tools used in this study are available through the following sources: GRanD v.1.3 database38, Zarfl, Lumsdon et al. (2015)15, G-res tool10, MAGICC626, SSP public database v.2.036. A year-by-year dataset of reservoir area and emissions is also available in Supplementary Data 1.

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Acknowledgements

This study was funded by the UNESCO Chair in Global Environmental Change held by Y.T.P. through which C.S., S.M.-B. and Y.T.P. were funded. J.A.H. was funded by an NSF INFEWS grant (NSF EAR 1639458), an NSF DEB Grant (no. 135211), a GRIL Fellowship Grant and a Stanford University Cox Visiting Professorship.

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Authors and Affiliations

  1. UNESCO Chair in Global Environmental Change, Department of Biological Sciences, University of Quebec at Montreal (UQAM), Montréal, Québec, Canada

    Cynthia Soued, Sara Mercier-Blais & Yves T. Prairie

  2. School of the Environment, Washington State University, Vancouver, Vancouver, WA, USA

    John A. Harrison

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Contributions

All authors contributed to conceptualization and data analysis. S.M.-B. performed data curation. J.A.H. and Y.T.P. acquired funding. C.S. wrote the original draft, and all authors reviewed and edited the manuscript.

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Correspondence to Cynthia Soued.

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Nature Geoscience thanks Xingchen Yan, Lluís Gómez-Gener, Ronny Lauerwald and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Thomas Richardson, in collaboration with the Nature Geoscience team.

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Soued, C., Harrison, J.A., Mercier-Blais, S. et al. Reservoir CO2 and CH4 emissions and their climate impact over the period 1900–2060. Nat. Geosci. 15, 700–705 (2022). https://doi.org/10.1038/s41561-022-01004-2

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