Sea ice controls net ocean uptake of carbon dioxide by regulating wintertime stratification

Sea-air exchange of carbon dioxide in the Southern Ocean is strongly seasonal, with ocean uptake in summer, which is partly offset by carbon dioxide outgassing in winter. This seasonal balance can shift due to sea ice conditions, inducing interannual variability in the Southern Ocean carbon sink. A decade (2010-2020) of unique, year-round marine carbonate chemistry observations from the Rothera Time Series (West Antarctic Peninsula) reveals that interannual variability in seawater fugacity of carbon dioxide depends on wintertime processes. Sea ice duration controls ocean stratification, which acts as a gateway to the carbon-rich ocean interior. Consequently, years with persistent sea ice cover and high mean winter stratification absorb, on average, 20% more carbon dioxide than years with less sea ice and weaker stratification in winter. Wintertime marine observations are therefore essential to resolve critical processes and reliably quantify interannual variability of the sea-air carbon dioxide flux in seasonally sea ice-covered regions.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-06-18
DOI
https://doi.org/10.1038/s43247-025-02395-x
Citations
1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.30

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article

Sea ice controls net ocean uptake of carbon dioxide by regulating wintertime stratification

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Arctic and Antarctic ice dynamics
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article

Sea ice controls net ocean uptake of carbon dioxide by regulating wintertime stratification

Michael P. Meredith, Giorgio Dall’Olmo, Elise S. Droste, Hugh J. Venables, Bastien Y. Queste, Oliver Legge, Gareth Lee, Mario Hoppema, Elizabeth M. Jones, Dorothée C. E. Bakker
article en
1 citations

Abstract

Sea-air exchange of carbon dioxide in the Southern Ocean is strongly seasonal, with ocean uptake in summer, which is partly offset by carbon dioxide outgassing in winter. This seasonal balance can shift due to sea ice conditions, inducing interannual variability in the Southern Ocean carbon sink. A decade (2010-2020) of unique, year-round marine carbonate chemistry observations from the Rothera Time Series (West Antarctic Peninsula) reveals that interannual variability in seawater fugacity of carbon dioxide depends on wintertime processes. Sea ice duration controls ocean stratification, which acts as a gateway to the carbon-rich ocean interior. Consequently, years with persistent sea ice cover and high mean winter stratification absorb, on average, 20% more carbon dioxide than years with less sea ice and weaker stratification in winter. Wintertime marine observations are therefore essential to resolve critical processes and reliably quantify interannual variability of the sea-air carbon dioxide flux in seasonally sea ice-covered regions.

Communications Earth & EnvironmentVol. 6(1)
University of East Anglia (GB), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), British Antarctic Survey (GB), Norwegian Institute of Marine Research (NO), National Institute of Oceanography and Applied Geophysics (IT), University of Gothenburg (SE)
European Commission, Rijksuniversiteit Groningen, Nederlandse Organisatie voor Wetenschappelijk Onderzoek, Koninklijk Nederlands Instituut voor Onderzoek der Zee, Horizon 2020 Framework Programme, Natural Environment Research Council
Life below water
Openalex Percentile: Top 21%
Arctic and Antarctic ice dynamics
1.30
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