Author
Listed:
- F. Li
(Xiamen University
Georgia Institute of Technology)
- M. S. Lozier
(Georgia Institute of Technology)
- S. Bacon
(National Oceanography Centre)
- A. S. Bower
(Woods Hole Oceanographic Institution)
- S. A. Cunningham
(Scottish Association for Marine Science)
- M. F. Jong
(NIOZ Royal Netherlands Institute for Sea Research)
- B. deYoung
(Memorial University)
- N. Fraser
(Scottish Association for Marine Science)
- N. Fried
(NIOZ Royal Netherlands Institute for Sea Research)
- G. Han
(Institute of Ocean Sciences
Northwest Atlantic Fisheries Centre)
- N. P. Holliday
(National Oceanography Centre)
- J. Holte
(UCSD)
- L. Houpert
(National Oceanography Centre)
- M. E. Inall
(Scottish Association for Marine Science
Edinburgh University)
- W. E. Johns
(University of Miami)
- S. Jones
(Scottish Association for Marine Science)
- C. Johnson
(Scottish Association for Marine Science)
- J. Karstensen
(GEOMAR Helmholtz Centre for Ocean Research Kiel)
- I. A. Le Bras
(Woods Hole Oceanographic Institution
UCSD)
- P. Lherminier
(Laboratoire d’Océanographie Physique et Spatiale)
- X. Lin
(Qingdao National Laboratory for Marine Science and Technology)
- H. Mercier
(Laboratoire d’Océanographie Physique et Spatiale)
- M. Oltmanns
(GEOMAR Helmholtz Centre for Ocean Research Kiel)
- A. Pacini
(Woods Hole Oceanographic Institution)
- T. Petit
(Georgia Institute of Technology)
- R. S. Pickart
(Woods Hole Oceanographic Institution)
- D. Rayner
(National Oceanography Centre)
- F. Straneo
(UCSD)
- V. Thierry
(Laboratoire d’Océanographie Physique et Spatiale)
- M. Visbeck
(GEOMAR Helmholtz Centre for Ocean Research Kiel)
- I. Yashayaev
(Bedford Institute of Oceanography)
- C. Zhou
(Qingdao National Laboratory for Marine Science and Technology)
Abstract
Changes in the Atlantic Meridional Overturning Circulation, which have the potential to drive societally-important climate impacts, have traditionally been linked to the strength of deep water formation in the subpolar North Atlantic. Yet there is neither clear observational evidence nor agreement among models about how changes in deep water formation influence overturning. Here, we use data from a trans-basin mooring array (OSNAP—Overturning in the Subpolar North Atlantic Program) to show that winter convection during 2014–2018 in the interior basin had minimal impact on density changes in the deep western boundary currents in the subpolar basins. Contrary to previous modeling studies, we find no discernable relationship between western boundary changes and subpolar overturning variability over the observational time scales. Our results require a reconsideration of the notion of deep western boundary changes representing overturning characteristics, with implications for constraining the source of overturning variability within and downstream of the subpolar region.
Suggested Citation
F. Li & M. S. Lozier & S. Bacon & A. S. Bower & S. A. Cunningham & M. F. Jong & B. deYoung & N. Fraser & N. Fried & G. Han & N. P. Holliday & J. Holte & L. Houpert & M. E. Inall & W. E. Johns & S. Jon, 2021.
"Subpolar North Atlantic western boundary density anomalies and the Meridional Overturning Circulation,"
Nature Communications, Nature, vol. 12(1), pages 1-9, December.
Handle:
RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-23350-2
DOI: 10.1038/s41467-021-23350-2
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Citations
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Cited by:
- Dipanjan Dey & Robert Marsh & Sybren Drijfhout & Simon A. Josey & Bablu Sinha & Jeremy Grist & Kristofer Döös, 2024.
"Formation of the Atlantic Meridional Overturning Circulation lower limb is critically dependent on Atlantic-Arctic mixing,"
Nature Communications, Nature, vol. 15(1), pages 1-10, December.
- C. W. Böning & P. Wagner & P. Handmann & F. U. Schwarzkopf & K. Getzlaff & A. Biastoch, 2023.
"Decadal changes in Atlantic overturning due to the excessive 1990s Labrador Sea convection,"
Nature Communications, Nature, vol. 14(1), pages 1-10, December.
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