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Increased risk of a shutdown of ocean convection posed by warm North Atlantic summers


A shutdown of ocean convection in the subpolar North Atlantic, triggered by enhanced melting over Greenland, is regarded as a potential transition point into a fundamentally different climate regime1,2,3. Noting that a key uncertainty for future convection resides in the relative importance of melting in summer and atmospheric forcing in winter, we investigate the extent to which summer conditions constrain convection with a comprehensive dataset, including hydrographic records that are over a decade in length from the convection regions. We find that warm and fresh summers, characterized by increased sea surface temperatures, freshwater concentrations and melting, are accompanied by reduced heat and buoyancy losses in winter, which entail a longer persistence of the freshwater near the surface and contribute to delaying convection. By shortening the time span for the convective freshwater export, the identified seasonal dynamics introduce a potentially critical threshold that is crossed when substantial amounts of freshwater from one summer are carried over into the next and accumulate. Warm and fresh summers in the Irminger Sea are followed by particularly short convection periods. We estimate that in the winter 2010–2011, after the warmest and freshest Irminger Sea summer on our record, ~40% of the surface freshwater was retained.

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We thank the staff at the NOAA/OAR/ESRL, NCAR and Hadley Centre for providing the SST data, and the staff at Ssalto/Duacs, Aviso and CNES for producing and distributing the altimeter products. We also appreciate the efforts that went into the development and management of the Ocean Observatories Initiative. The research in this study contributes to the projects ‘Blue-Action’ and ‘AtlantOS’ and was funded by the EU Horizon 2020 Programme under grant agreements 727852 and 633211. It was further supported by the German Federal Ministry of Education and Research as part of the ‘Regional Atlantic Circulation and Global Change’ project.

Author information

J.F. and J.K. were involved in planning, acquiring and processing the mooring data. M.O. and J.K. conceived the story. M.O. carried out the data analysis and interpreted the results. All authors contributed to writing the paper.

Competing interests

The authors declare no competing interests.

Correspondence to Marilena Oltmanns.

Supplementary information

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    Supplementary Figures 1–9, Supplementary Table 1 and Supplementary References

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Fig. 1: Labrador Sea, 2010–2011.
Fig. 2: Fresh summers in the Irminger Sea.
Fig. 3: Summer constraints on hydrographic evolution in the Labrador Sea.
Fig. 4: Summer constraints on atmospheric evolution in autumn and winter.
Fig. 5: Trends in the forcing parameters, 1990–2014.