Compensation between meridional flow components of the Atlantic MOC at 26°N
From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26°?N (2004–2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations, transport variations of the Florida Current (FC) and...
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ftsouthampton:oai:eprints.soton.ac.uk:390694 2023-07-30T04:05:06+02:00 Compensation between meridional flow components of the Atlantic MOC at 26°N Frajka-Williams, E. Meinen, C.S. Johns, W.E. Smeed, D.A. Duchez, A. Lawrence, A.J. Cuthbertson, D.A. Mccarthy, G.D. Bryden, H.L. Baringer, M.O. Moat, B.I. Rayner, D. 2016 text https://eprints.soton.ac.uk/390694/ https://eprints.soton.ac.uk/390694/1/os-12-481-2016.pdf en English eng https://eprints.soton.ac.uk/390694/1/os-12-481-2016.pdf Frajka-Williams, E., Meinen, C.S., Johns, W.E., Smeed, D.A., Duchez, A., Lawrence, A.J., Cuthbertson, D.A., Mccarthy, G.D., Bryden, H.L., Baringer, M.O., Moat, B.I. and Rayner, D. (2016) Compensation between meridional flow components of the Atlantic MOC at 26°N. Ocean Science, 12 (2), 481-493. (doi:10.5194/os-12-481-2016 <http://dx.doi.org/10.5194/os-12-481-2016>). cc_by_4 Article PeerReviewed 2016 ftsouthampton https://doi.org/10.5194/os-12-481-2016 2023-07-09T22:05:46Z From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26°?N (2004–2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations, transport variations of the Florida Current (FC) and upper mid-ocean (UMO) transports (top 1000?m east of the Bahamas) are now found to compensate on sub-annual timescales. The observed compensation between the FC and UMO transports is associated with horizontal circulation and means that this part of the correlated variability does not project onto the MOC. A deep baroclinic response to wind-forcing (Ekman transport) is also found in the lower North Atlantic Deep Water (LNADW; 3000–5000?m) transport. In contrast, co-variability between Ekman and the LNADW transports does contribute to overturning. On longer timescales, the southward UMO transport has continued to strengthen, resulting in a continued decline of the MOC. Most of this interannual variability of the MOC can be traced to changes in isopycnal displacements on the western boundary, within the top 1000?m and below 2000?m. Substantial trends are observed in isopycnal displacements in the deep ocean, underscoring the importance of deep boundary measurements to capture the variability of the Atlantic MOC. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic University of Southampton: e-Prints Soton Ocean Science 12 2 481 493 |
institution |
Open Polar |
collection |
University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26°?N (2004–2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations, transport variations of the Florida Current (FC) and upper mid-ocean (UMO) transports (top 1000?m east of the Bahamas) are now found to compensate on sub-annual timescales. The observed compensation between the FC and UMO transports is associated with horizontal circulation and means that this part of the correlated variability does not project onto the MOC. A deep baroclinic response to wind-forcing (Ekman transport) is also found in the lower North Atlantic Deep Water (LNADW; 3000–5000?m) transport. In contrast, co-variability between Ekman and the LNADW transports does contribute to overturning. On longer timescales, the southward UMO transport has continued to strengthen, resulting in a continued decline of the MOC. Most of this interannual variability of the MOC can be traced to changes in isopycnal displacements on the western boundary, within the top 1000?m and below 2000?m. Substantial trends are observed in isopycnal displacements in the deep ocean, underscoring the importance of deep boundary measurements to capture the variability of the Atlantic MOC. |
format |
Article in Journal/Newspaper |
author |
Frajka-Williams, E. Meinen, C.S. Johns, W.E. Smeed, D.A. Duchez, A. Lawrence, A.J. Cuthbertson, D.A. Mccarthy, G.D. Bryden, H.L. Baringer, M.O. Moat, B.I. Rayner, D. |
spellingShingle |
Frajka-Williams, E. Meinen, C.S. Johns, W.E. Smeed, D.A. Duchez, A. Lawrence, A.J. Cuthbertson, D.A. Mccarthy, G.D. Bryden, H.L. Baringer, M.O. Moat, B.I. Rayner, D. Compensation between meridional flow components of the Atlantic MOC at 26°N |
author_facet |
Frajka-Williams, E. Meinen, C.S. Johns, W.E. Smeed, D.A. Duchez, A. Lawrence, A.J. Cuthbertson, D.A. Mccarthy, G.D. Bryden, H.L. Baringer, M.O. Moat, B.I. Rayner, D. |
author_sort |
Frajka-Williams, E. |
title |
Compensation between meridional flow components of the Atlantic MOC at 26°N |
title_short |
Compensation between meridional flow components of the Atlantic MOC at 26°N |
title_full |
Compensation between meridional flow components of the Atlantic MOC at 26°N |
title_fullStr |
Compensation between meridional flow components of the Atlantic MOC at 26°N |
title_full_unstemmed |
Compensation between meridional flow components of the Atlantic MOC at 26°N |
title_sort |
compensation between meridional flow components of the atlantic moc at 26°n |
publishDate |
2016 |
url |
https://eprints.soton.ac.uk/390694/ https://eprints.soton.ac.uk/390694/1/os-12-481-2016.pdf |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_relation |
https://eprints.soton.ac.uk/390694/1/os-12-481-2016.pdf Frajka-Williams, E., Meinen, C.S., Johns, W.E., Smeed, D.A., Duchez, A., Lawrence, A.J., Cuthbertson, D.A., Mccarthy, G.D., Bryden, H.L., Baringer, M.O., Moat, B.I. and Rayner, D. (2016) Compensation between meridional flow components of the Atlantic MOC at 26°N. Ocean Science, 12 (2), 481-493. (doi:10.5194/os-12-481-2016 <http://dx.doi.org/10.5194/os-12-481-2016>). |
op_rights |
cc_by_4 |
op_doi |
https://doi.org/10.5194/os-12-481-2016 |
container_title |
Ocean Science |
container_volume |
12 |
container_issue |
2 |
container_start_page |
481 |
op_container_end_page |
493 |
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1772816813779845120 |