Atlantic transport variability at 25° N in six hydrographic sections
In January and February 2010, a sixth transatlantic hydrographic section was completed across 25° N, extending the hydrographic record at this latitude to over half a century. In combination with continuous transport measurements made since 2004 at 26.5° N by the Rapid-WATCH project, we reassess tra...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:81c649fed51a41f5a41d1240fdd0e514 2023-05-15T17:25:25+02:00 Atlantic transport variability at 25° N in six hydrographic sections C. P. Atkinson H. L. Bryden S. A. Cunningham B. A. King 2012-07-01 https://doi.org/10.5194/os-8-497-2012 http://www.ocean-sci.net/8/497/2012/os-8-497-2012.pdf https://doaj.org/article/81c649fed51a41f5a41d1240fdd0e514 en eng Copernicus Publications doi:10.5194/os-8-497-2012 1812-0784 1812-0792 http://www.ocean-sci.net/8/497/2012/os-8-497-2012.pdf https://doaj.org/article/81c649fed51a41f5a41d1240fdd0e514 undefined Ocean Science, Vol 8, Iss 4, Pp 497-523 (2012) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2012 fttriple https://doi.org/10.5194/os-8-497-2012 2023-01-22T17:50:35Z In January and February 2010, a sixth transatlantic hydrographic section was completed across 25° N, extending the hydrographic record at this latitude to over half a century. In combination with continuous transport measurements made since 2004 at 26.5° N by the Rapid-WATCH project, we reassess transport variability in the 25° N hydrographic record. Past studies of transport variability at this latitude have assumed transport estimates from each hydrographic section to represent annual average conditions. In this study the uncertainty in this assumption is assessed through use of Rapid-WATCH observations to quantify sub-seasonal and seasonal transport variability. Whilst in the upper-ocean no significant interannual or decadal transport variability are identified in the hydrographic record, in the deep ocean transport variability in both depth and potential temperature classes suggests some interannual or decadal variability may have occurred. This is particularly striking in the lower North Atlantic Deep Water where southward transports prior to 1998 were greater than recent transports by several Sverdrups. Whilst a cooling and freshening of Denmark Straits Overflow Water has occurred which is coincident with these transport changes, these water mass changes appear to be density compensated. Transport changes are the result of changing velocity shear in the vicinity of the Deep Western Boundary Current. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Unknown Ocean Science 8 4 497 523 |
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envir geo C. P. Atkinson H. L. Bryden S. A. Cunningham B. A. King Atlantic transport variability at 25° N in six hydrographic sections |
topic_facet |
envir geo |
description |
In January and February 2010, a sixth transatlantic hydrographic section was completed across 25° N, extending the hydrographic record at this latitude to over half a century. In combination with continuous transport measurements made since 2004 at 26.5° N by the Rapid-WATCH project, we reassess transport variability in the 25° N hydrographic record. Past studies of transport variability at this latitude have assumed transport estimates from each hydrographic section to represent annual average conditions. In this study the uncertainty in this assumption is assessed through use of Rapid-WATCH observations to quantify sub-seasonal and seasonal transport variability. Whilst in the upper-ocean no significant interannual or decadal transport variability are identified in the hydrographic record, in the deep ocean transport variability in both depth and potential temperature classes suggests some interannual or decadal variability may have occurred. This is particularly striking in the lower North Atlantic Deep Water where southward transports prior to 1998 were greater than recent transports by several Sverdrups. Whilst a cooling and freshening of Denmark Straits Overflow Water has occurred which is coincident with these transport changes, these water mass changes appear to be density compensated. Transport changes are the result of changing velocity shear in the vicinity of the Deep Western Boundary Current. |
format |
Article in Journal/Newspaper |
author |
C. P. Atkinson H. L. Bryden S. A. Cunningham B. A. King |
author_facet |
C. P. Atkinson H. L. Bryden S. A. Cunningham B. A. King |
author_sort |
C. P. Atkinson |
title |
Atlantic transport variability at 25° N in six hydrographic sections |
title_short |
Atlantic transport variability at 25° N in six hydrographic sections |
title_full |
Atlantic transport variability at 25° N in six hydrographic sections |
title_fullStr |
Atlantic transport variability at 25° N in six hydrographic sections |
title_full_unstemmed |
Atlantic transport variability at 25° N in six hydrographic sections |
title_sort |
atlantic transport variability at 25° n in six hydrographic sections |
publisher |
Copernicus Publications |
publishDate |
2012 |
url |
https://doi.org/10.5194/os-8-497-2012 http://www.ocean-sci.net/8/497/2012/os-8-497-2012.pdf https://doaj.org/article/81c649fed51a41f5a41d1240fdd0e514 |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_source |
Ocean Science, Vol 8, Iss 4, Pp 497-523 (2012) |
op_relation |
doi:10.5194/os-8-497-2012 1812-0784 1812-0792 http://www.ocean-sci.net/8/497/2012/os-8-497-2012.pdf https://doaj.org/article/81c649fed51a41f5a41d1240fdd0e514 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/os-8-497-2012 |
container_title |
Ocean Science |
container_volume |
8 |
container_issue |
4 |
container_start_page |
497 |
op_container_end_page |
523 |
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1766116846935736320 |