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Ocean circulation causes the largest freshening event for 120 years in eastern subpolar North Atlantic

Author

Listed:
  • N. Penny Holliday

    (National Oceanography Centre)

  • Manfred Bersch

    (University of Hamburg)

  • Barbara Berx

    (Marine Scotland Science)

  • Léon Chafik

    (Stockholm University)

  • Stuart Cunningham

    (Scottish Association for Marine Science)

  • Cristian Florindo-López

    (National Oceanography Centre)

  • Hjálmar Hátún

    (Faroe Marine Research Institute)

  • William Johns

    (University of Miami)

  • Simon A. Josey

    (National Oceanography Centre)

  • Karin Margretha H. Larsen

    (Faroe Marine Research Institute)

  • Sandrine Mulet

    (CLS)

  • Marilena Oltmanns

    (GEOMAR Helmholtz Centre for Ocean Research Kiel)

  • Gilles Reverdin

    (Sorbonne Université, CNRS/IRD/MNHN (LOCEAN))

  • Tom Rossby

    (University of Rhode Island)

  • Virginie Thierry

    (Laboratoire d’Océanographie Physique et Spatiale)

  • Hedinn Valdimarsson

    (Marine and Freshwater Research Institute)

  • Igor Yashayaev

    (Bedford Institute of Oceanography)

Abstract

The Atlantic Ocean overturning circulation is important to the climate system because it carries heat and carbon northward, and from the surface to the deep ocean. The high salinity of the subpolar North Atlantic is a prerequisite for overturning circulation, and strong freshening could herald a slowdown. We show that the eastern subpolar North Atlantic underwent extreme freshening during 2012 to 2016, with a magnitude never seen before in 120 years of measurements. The cause was unusual winter wind patterns driving major changes in ocean circulation, including slowing of the North Atlantic Current and diversion of Arctic freshwater from the western boundary into the eastern basins. We find that wind-driven routing of Arctic-origin freshwater intimately links conditions on the North West Atlantic shelf and slope region with the eastern subpolar basins. This reveals the importance of atmospheric forcing of intra-basin circulation in determining the salinity of the subpolar North Atlantic.

Suggested Citation

  • N. Penny Holliday & Manfred Bersch & Barbara Berx & Léon Chafik & Stuart Cunningham & Cristian Florindo-López & Hjálmar Hátún & William Johns & Simon A. Josey & Karin Margretha H. Larsen & Sandrine Mu, 2020. "Ocean circulation causes the largest freshening event for 120 years in eastern subpolar North Atlantic," Nature Communications, Nature, vol. 11(1), pages 1-15, December.
  • Handle: RePEc:nat:natcom:v:11:y:2020:i:1:d:10.1038_s41467-020-14474-y
    DOI: 10.1038/s41467-020-14474-y
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    Cited by:

    1. Mathilde Jutras & Carolina O. Dufour & Alfonso Mucci & Lauryn C. Talbot, 2023. "Large-scale control of the retroflection of the Labrador Current," Nature Communications, Nature, vol. 14(1), pages 1-9, December.

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