Articles | Volume 12, issue 2
https://doi.org/10.5194/os-12-481-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-481-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
01 Apr 2016
Research article |
| 01 Apr 2016
Compensation between meridional flow components of the Atlantic MOC at 26° N
E. Frajka-Williams
CORRESPONDING AUTHOR
Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, SO14 3ZH, UK
C. S. Meinen
Atlantic Oceanographic and Meteorological Laboratory, Physical Oceanography Division, 4301 Rickenbacker Causeway, Miami, FL 33149, USA
W. E. Johns
University of Miami, Rosentiel School of Marine and Atmospheric Science, 4600 Rickenbacker Causeway, Miami, FL, USA
D. A. Smeed
National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
A. Duchez
National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
A. J. Lawrence
Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, SO14 3ZH, UK
D. A. Cuthbertson
Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, SO14 3ZH, UK
G. D. McCarthy
National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
H. L. Bryden
Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, SO14 3ZH, UK
M. O. Baringer
Atlantic Oceanographic and Meteorological Laboratory, Physical Oceanography Division, 4301 Rickenbacker Causeway, Miami, FL 33149, USA
B. I. Moat
National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
D. Rayner
National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
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Bogi Hansen, Karin Margretha Húsgarð Larsen, Hjálmar Hátún, and Svein Østerhus
Ocean Sci., 12, 1205–1220, https://doi.org/10.5194/os-12-1205-2016, https://doi.org/10.5194/os-12-1205-2016, 2016
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T. J. Sherwin, D. Aleynik, E. Dumont, and M. E. Inall
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C. P. Atkinson, H. L. Bryden, S. A. Cunningham, and B. A. King
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C. P. Atkinson, H. L. Bryden, J. J-M. Hirschi, and T. Kanzow
Ocean Sci., 6, 837–859, https://doi.org/10.5194/os-6-837-2010, https://doi.org/10.5194/os-6-837-2010, 2010
M. P. Chidichimo, T. Kanzow, S. A. Cunningham, W. E. Johns, and J. Marotzke
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Short summary
The ocean meridional overturning circulation (MOC) is predicted by climate models to slow down in this century, resulting in reduced transport of heat northward to mid-latitudes. At 26° N, the Atlantic MOC has been measured continuously for the past decade (2004–2014). In this paper, we discuss the 10-year record of variability, identify the origins of the continued weakening of the circulation, and discuss high-frequency (subannual) compensation between transport components.
The ocean meridional overturning circulation (MOC) is predicted by climate models to slow down...
