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Rapid coastal deoxygenation due to ocean circulation shift in the northwest Atlantic

Nature Climate Changevolume 8pages868872 (2018) | Download Citation


Global observations show that the ocean lost approximately 2% of its oxygen inventory over the past five decades1,2,3, with important implications for marine ecosystems4,5. The rate of change varies regionally, with northwest Atlantic coastal waters showing a long-term drop6,7 that vastly outpaces the global and North Atlantic basin mean deoxygenation rates5,8. However, past work has been unable to differentiate the role of large-scale climate forcing from that of local processes. Here, we use hydrographic evidence to show that a Labrador Current retreat is playing a key role in the deoxygenation on the northwest Atlantic shelf. A high-resolution global coupled climate–biogeochemistry model9 reproduces the observed decline of saturation oxygen concentrations in the region, driven by a retreat of the equatorward-flowing Labrador Current and an associated shift towards more oxygen-poor subtropical waters on the shelf. The dynamical changes underlying the shift in shelf water properties are correlated with a slowdown in the simulated Atlantic Meridional Overturning Circulation (AMOC)10. Our results provide strong evidence that a major, centennial-scale change of the Labrador Current is underway, and highlight the potential for ocean dynamics to impact coastal deoxygenation over the coming century.

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The authors thank A. Cogswell and R. Pettipas from Fisheries and Oceans Canada for providing hydrographic data in the central Scotian Shelf and C. E. Brennan for providing the data for the oxygen time series in the central Scotian Shelf. The authors also acknowledge many scientists at NOAA GFDL that configured and ran the climate model, without whose efforts this work would not have been possible. This project has received funding from the European Research Council under the European Union’s Horizon 2020 research and innovation programme (grant no. 682602). E.D.G. acknowledges financial support from the Spanish Ministry of Economy and Competitiveness through the Mara de Maeztu Programme for Centres/Units of Excellence (MDM-2015-0552). The Canadian Foundation for Innovation provided the computing resources for model analysis. D.B. acknowledges support from NOAA grant NA15NOS4780186.

Author information


  1. Joint Institute for the Study of the Atmosphere and the Ocean, Seattle, WA, USA

    • Mariona Claret
  2. University of Washington, Seattle, WA, USA

    • Mariona Claret
  3. Department of Earth and Planetary Sciences, McGill University, Montréal, Quebec, Canada

    • Mariona Claret
    •  & Eric D. Galbraith
  4. Institució Catalana de Recerca i Estudis Avançats (ICREA), Barcelona, Spain

    • Eric D. Galbraith
  5. Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona, Cerdanyola del Vallès, Spain

    • Eric D. Galbraith
  6. Graduate School of Oceanography, University of Rhode Island, Narragansett, RI, USA

    • Jaime B. Palter
  7. Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA, USA

    • Daniele Bianchi
  8. Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada

    • Katja Fennel
  9. Maurice Lamontagne Institute, Fisheries and Oceans Canada, Mont-Joli, Quebec, Canada

    • Denis Gilbert
  10. NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA

    • John P. Dunne


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E.D.G., J.B.P. and D.B. conceived the study. M.C., D.G. and K.F. assembled and analysed the observational data. M.C. and D.B. performed the model output analyses. J.P.D. and E.D.G. participated in the design of the CM2.6-miniBLING experiments. M.C., E.D.G., J.B.P. and D.B. wrote the first draft of the manuscript. All the authors discussed the results and provided input to the manuscript.

Competing interests

The authors declare no competing Interests.

Corresponding author

Correspondence to Mariona Claret.

Supplementary information

  1. Supplementary Information Description: Supplementary figures 1–9, Supplementary Notes, Supplementary References, Supplementary Tables 1–3

    Supplementary figures 1–9, Supplementary Notes, Supplementary References, Supplementary Tables 1–3

  2. Supplementary Video 1

    Time evolution of simulated O2 in the northwest Atlantic on isopycnal σθ = 27.25 kg m−3 over the last twenty model years (from 181 to 200) for preindustrial control (LEFT) and warming (1% annual pCO2 increase until doubled, RIGHT) scenarios. Climate model horizontal resolution is 1/10° and the time period between movie frames is five days. The movie shows that the oxygen supply to slope waters (white shading in Fig. 1) and the Laurentian Channel decreases significantly under warming due to a reduction in transport of ventilated Labrador Current waters west of the Tail of the Grand Banks. Isopycnal outcrop is shown in white

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