Unexpected decline in the ocean carbon sink under record-high sea surface temperatures in 2023

Abstract In 2023, sea surface temperatures (SSTs) reached record highs, partly due to a strong El Niño. Based on historical responses to elevated global mean SSTs, oceanic CO 2 uptake in 2023 should have increased (−0.11 ± 0.04 PgC yr −1 ), driven by reduced outgassing in the tropical Pacific Ocean. However, using observation-based estimates of ocean CO 2 fugacity, we show here that the global non-polar ocean absorbed about 10% less CO 2 than expected (+0.17 ± 0.12 PgC yr −1 ). This weakening was caused by the anomalous outgassing of CO 2 in the subtropical and subpolar regions, especially in the Northern Hemisphere, driven primarily by elevated SSTs reducing the solubility of CO 2 . In most regions, this SST-induced outgassing was mitigated by the depletion of dissolved inorganic carbon in the surface mixed layer. Such negative feedbacks caused an overall muted response of the ocean carbon sink to the record-high SSTs, but this resilience may not persist under long-term warming or more severe SST extremes.

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Publication Details

Journal
Nature Climate Change
Published
2025-09-01
DOI
https://doi.org/10.1038/s41558-025-02380-4
Citations
1
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
1.11

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Unexpected decline in the ocean carbon sink under record-high sea surface temperatures in 2023

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1 citations
Nature Climate Change
Atmospheric and Environmental Gas Dynamics
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article

Unexpected decline in the ocean carbon sink under record-high sea surface temperatures in 2023

Galen A. McKinley, Nicolas Gruber, Marion Gehlen, Luke Gregor, Judith Hauck, Jens Daniel Müller, Dorothée C. E. Bakker, Peter Landschützer, Aline Schneuwly
article en
1 citations

Abstract

Abstract In 2023, sea surface temperatures (SSTs) reached record highs, partly due to a strong El Niño. Based on historical responses to elevated global mean SSTs, oceanic CO 2 uptake in 2023 should have increased (−0.11 ± 0.04 PgC yr −1 ), driven by reduced outgassing in the tropical Pacific Ocean. However, using observation-based estimates of ocean CO 2 fugacity, we show here that the global non-polar ocean absorbed about 10% less CO 2 than expected (+0.17 ± 0.12 PgC yr −1 ). This weakening was caused by the anomalous outgassing of CO 2 in the subtropical and subpolar regions, especially in the Northern Hemisphere, driven primarily by elevated SSTs reducing the solubility of CO 2 . In most regions, this SST-induced outgassing was mitigated by the depletion of dissolved inorganic carbon in the surface mixed layer. Such negative feedbacks caused an overall muted response of the ocean carbon sink to the record-high SSTs, but this resilience may not persist under long-term warming or more severe SST extremes.

Nature Climate ChangeVol. 15(9)
University of East Anglia (GB), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Flanders Marine Institute (BE), Centre National de la Recherche Scientifique (FR), Lamont-Doherty Earth Observatory (US), University of Bremen (DE), Université de Versailles Saint-Quentin-en-Yvelines (FR), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), ETH Zurich (CH), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR), Columbia University (US)
National Science Foundation, Helmholtz Association, National Oceanic and Atmospheric Administration, Horizon 2020 Framework Programme
Openalex Percentile: Top 20%
Atmospheric and Environmental Gas Dynamics
1.11
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