Seasonal variability of the Atlantic meridional overturning circulation at 26.5°N
Seasonal variability of the Atlantic meridional overturning circulation at 26.5°N
The Atlantic meridional overturning circulation (AMOC) makes the strongest oceanic contribution to the meridional redistribution of heat. Here, an observation-based, 48-month-long time series of the vertical structure and strength of the AMOC at 26.5°N is presented. From April 2004 to April 2008, the AMOC had a mean strength of 18.7 ± 2.1 Sv (1 Sv ? 106 m3 s?1) with fluctuations of 4.8 Sv rms. The best guess of the peak-to-peak amplitude of the AMOC seasonal cycle is 6.7 Sv, with a maximum strength in autumn and a minimum in spring. While seasonality in the AMOC was commonly thought to be dominated by the northward Ekman transport, this study reveals that fluctuations of the geostrophic midocean and Gulf Stream transports of 2.2 and 1.7 Sv rms, respectively, are substantially larger than those of the Ekman component (1.2 Sv rms). A simple model based on linear dynamics suggests that the seasonal cycle is dominated by wind stress curl forcing at the eastern boundary of the Atlantic. Seasonal geostrophic AMOC anomalies might represent an important and previously underestimated component of meridional transport and storage of heat in the subtropical North Atlantic. There is evidence that the seasonal cycle observed here is representative of much longer intervals. Previously, hydrographic snapshot estimates between 1957 and 2004 had suggested a long-term decline of the AMOC by 8 Sv. This study suggests that aliasing of seasonal AMOC anomalies might have accounted for a large part of the inferred slowdown.
5678-5698
Kanzow, T.
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Cunningham, S.A.
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Johns, W.E.
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Hirschi, J.J-M.
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Marotzke, J.
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Baringer, M.O.
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Meinen, C.S.
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Chidichimo, M.P.
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Atkinson, C.
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Beal, L.M.
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Bryden, H.L.
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Collins, J.
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1 November 2010
Kanzow, T.
ede4d92e-c4b2-48d0-83bf-a03f881aa819
Cunningham, S.A.
07f1bd78-d92f-478b-a016-b92f530142c3
Johns, W.E.
e69b0088-c832-4ed8-94f6-9c5e9e6f62af
Hirschi, J.J-M.
c8a45006-a6e3-4319-b5f5-648e8ef98906
Marotzke, J.
6047bfd1-68a3-4abe-95ce-e1df9a56ce76
Baringer, M.O.
b8dab4b9-918b-4bc9-a033-dcbeb03f5730
Meinen, C.S.
e1d8f782-ccdf-4f81-98c4-cc1c7701165c
Chidichimo, M.P.
eb692475-d4b9-4a3d-af65-ac8ff566bd54
Atkinson, C.
760a87ea-b947-437e-a511-5a3afcf36fa4
Beal, L.M.
3939723a-86f3-4691-bd09-bf1ab2657c76
Bryden, H.L.
7f823946-34e8-48a3-8bd4-a72d2d749184
Collins, J.
3b902164-96cf-4fb2-a9e2-23f08f64c5fd
Kanzow, T., Cunningham, S.A., Johns, W.E., Hirschi, J.J-M., Marotzke, J., Baringer, M.O., Meinen, C.S., Chidichimo, M.P., Atkinson, C., Beal, L.M., Bryden, H.L. and Collins, J.
(2010)
Seasonal variability of the Atlantic meridional overturning circulation at 26.5°N.
Journal of Climate, 23 (21), .
(doi:10.1175/2010JCLI3389.1).
Abstract
The Atlantic meridional overturning circulation (AMOC) makes the strongest oceanic contribution to the meridional redistribution of heat. Here, an observation-based, 48-month-long time series of the vertical structure and strength of the AMOC at 26.5°N is presented. From April 2004 to April 2008, the AMOC had a mean strength of 18.7 ± 2.1 Sv (1 Sv ? 106 m3 s?1) with fluctuations of 4.8 Sv rms. The best guess of the peak-to-peak amplitude of the AMOC seasonal cycle is 6.7 Sv, with a maximum strength in autumn and a minimum in spring. While seasonality in the AMOC was commonly thought to be dominated by the northward Ekman transport, this study reveals that fluctuations of the geostrophic midocean and Gulf Stream transports of 2.2 and 1.7 Sv rms, respectively, are substantially larger than those of the Ekman component (1.2 Sv rms). A simple model based on linear dynamics suggests that the seasonal cycle is dominated by wind stress curl forcing at the eastern boundary of the Atlantic. Seasonal geostrophic AMOC anomalies might represent an important and previously underestimated component of meridional transport and storage of heat in the subtropical North Atlantic. There is evidence that the seasonal cycle observed here is representative of much longer intervals. Previously, hydrographic snapshot estimates between 1957 and 2004 had suggested a long-term decline of the AMOC by 8 Sv. This study suggests that aliasing of seasonal AMOC anomalies might have accounted for a large part of the inferred slowdown.
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Published date: 1 November 2010
Organisations:
Ocean and Earth Science, National Oceanography Centre,Southampton, Marine Physics and Ocean Climate
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Local EPrints ID: 168897
URI: http://eprints.soton.ac.uk/id/eprint/168897
ISSN: 0894-8755
PURE UUID: 1433603f-09e9-4438-9f9c-61ecfd7ac1be
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Date deposited: 06 Dec 2010 17:02
Last modified: 14 Mar 2024 02:39
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Contributors
Author:
T. Kanzow
Author:
S.A. Cunningham
Author:
W.E. Johns
Author:
J.J-M. Hirschi
Author:
J. Marotzke
Author:
M.O. Baringer
Author:
C.S. Meinen
Author:
M.P. Chidichimo
Author:
C. Atkinson
Author:
L.M. Beal
Author:
J. Collins
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