The northern North Atlantic Ocean mean circulation in the early 21st Century
The decadal mean circulation in the northern North Atlantic was assessed for the early 21st century from repeated ship-based measurements along the Greenland-Portugal OVIDE line, from satellite altimetry and from earlier reported transports across 59.5°N and at the Greenland-Scotland sills. The rema...
Published in: | Progress in Oceanography |
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Main Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon-elsevier Science Ltd
2016
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00345/45569/45177.pdf https://doi.org/10.1016/j.pocean.2016.06.007 https://archimer.ifremer.fr/doc/00345/45569/ |
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ftarchimer:oai:archimer.ifremer.fr:45569 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
The decadal mean circulation in the northern North Atlantic was assessed for the early 21st century from repeated ship-based measurements along the Greenland-Portugal OVIDE line, from satellite altimetry and from earlier reported transports across 59.5°N and at the Greenland-Scotland sills. The remarkable quantitative agreement between all data sets allowed us to draw circulation pathways with a high level of confidence. The North Atlantic Current (NAC) system is composed of three main branches, referred to as the northern, central and southern branches, which were traced from the Mid-Atlantic Ridge (MAR), to the Irminger Sea, the Greenland-Scotland Ridge and the subtropical gyre. At OVIDE, the northern and central branches of the NAC fill the whole water column and their top-to-bottom integrated transports were estimated at 11.0 ± 3 Sv and 14.2 ± 6.4 Sv (1 Sv = 106 m3 s-1), respectively. Those two branches feed the cyclonic circulation in the Iceland Basin and the flow over the Reykjanes Ridge into the Irminger Sea. This cross-ridge flow was estimated at 11.3 ± 4.2 Sv westward, north of 58.5°N. The southern NAC branch is strongly surface-intensified and most of its top-to-bottom integrated transport, estimated at 16.6 ± 2 Sv, is found in the upper layer. It is composed of two parts: the northern part contributes to the flow over the Rockall Plateau and through the Rockall Trough towards the Iceland-Scotland Ridge; the southern part feeds the anticyclonic circulation towards the subtropical gyre. Summing over the three NAC branches, the top-to-bottom transport of the NAC across OVIDE was estimated at 41.8 ± 3.7 Sv. Because of the surface-intensification of the southern NAC branch, the intermediate water is transported to the northeast Atlantic mostly by the northern and central branches of the NAC (11.9 ± 1.8 Sv eastward). This water circulates cyclonically in the Iceland Basin and anticyclonically in the West European Basin, with similar transport intensities. In the deep layer of the Iceland Basin, Iceland-Scotland Overflow Water (ISOW) spreads southwestward along three pathways on the eastern flank of the Reykjanes Ridge. The associated transport was estimated at 3.2 ± 0.4 Sv. The two shallowest pathways turn around the Reykjanes Ridge towards the Irminger Sea where they head northward. A northeastward transport of deep water is observed in the deep extension of the northern and central branches of the NAC, east of the MAR. In the Irminger Sea our transport estimates for the Irminger Current, Irminger Gyre, East Greenland Irminger Current and Deep Western Boundary Current are in line with previous work. |
format |
Article in Journal/Newspaper |
author |
Daniault, Nathalie Mercier, Herle Lherminier, Pascale Sarafanov, Artem Falina, Anastasia Zunino, Patricia Perezf, Fiz F. Rios, Aida F. Ferron, Bruno Huck, Thierry Thierry, Virginie Gladyshev, Sergey |
spellingShingle |
Daniault, Nathalie Mercier, Herle Lherminier, Pascale Sarafanov, Artem Falina, Anastasia Zunino, Patricia Perezf, Fiz F. Rios, Aida F. Ferron, Bruno Huck, Thierry Thierry, Virginie Gladyshev, Sergey The northern North Atlantic Ocean mean circulation in the early 21st Century |
author_facet |
Daniault, Nathalie Mercier, Herle Lherminier, Pascale Sarafanov, Artem Falina, Anastasia Zunino, Patricia Perezf, Fiz F. Rios, Aida F. Ferron, Bruno Huck, Thierry Thierry, Virginie Gladyshev, Sergey |
author_sort |
Daniault, Nathalie |
title |
The northern North Atlantic Ocean mean circulation in the early 21st Century |
title_short |
The northern North Atlantic Ocean mean circulation in the early 21st Century |
title_full |
The northern North Atlantic Ocean mean circulation in the early 21st Century |
title_fullStr |
The northern North Atlantic Ocean mean circulation in the early 21st Century |
title_full_unstemmed |
The northern North Atlantic Ocean mean circulation in the early 21st Century |
title_sort |
northern north atlantic ocean mean circulation in the early 21st century |
publisher |
Pergamon-elsevier Science Ltd |
publishDate |
2016 |
url |
https://archimer.ifremer.fr/doc/00345/45569/45177.pdf https://doi.org/10.1016/j.pocean.2016.06.007 https://archimer.ifremer.fr/doc/00345/45569/ |
long_lat |
ENVELOPE(-34.041,-34.041,63.054,63.054) ENVELOPE(-22.250,-22.250,65.467,65.467) ENVELOPE(-18.833,-18.833,56.333,56.333) ENVELOPE(-15.036,-15.036,53.825,53.825) ENVELOPE(-28.000,-28.000,52.750,52.750) |
geographic |
Greenland Irminger Sea Mid-Atlantic Ridge Reykjanes Rockall Plateau Rockall Trough West European Basin |
geographic_facet |
Greenland Irminger Sea Mid-Atlantic Ridge Reykjanes Rockall Plateau Rockall Trough West European Basin |
genre |
East Greenland Greenland Greenland-Scotland Ridge Iceland north atlantic current North Atlantic Northeast Atlantic |
genre_facet |
East Greenland Greenland Greenland-Scotland Ridge Iceland north atlantic current North Atlantic Northeast Atlantic |
op_source |
Progress In Oceanography (0079-6611) (Pergamon-elsevier Science Ltd), 2016-08 , Vol. 146 , P. 142-158 |
op_relation |
info:eu-repo/grantAgreement/EC/FP7/264879/EU//CARBOCHANGE https://archimer.ifremer.fr/doc/00345/45569/45177.pdf doi:10.1016/j.pocean.2016.06.007 https://archimer.ifremer.fr/doc/00345/45569/ |
op_rights |
2016 Elsevier Ltd. All rights reserved. info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1016/j.pocean.2016.06.007 |
container_title |
Progress in Oceanography |
container_volume |
146 |
container_start_page |
142 |
op_container_end_page |
158 |
_version_ |
1766399652376084480 |
spelling |
ftarchimer:oai:archimer.ifremer.fr:45569 2023-05-15T16:03:57+02:00 The northern North Atlantic Ocean mean circulation in the early 21st Century Daniault, Nathalie Mercier, Herle Lherminier, Pascale Sarafanov, Artem Falina, Anastasia Zunino, Patricia Perezf, Fiz F. Rios, Aida F. Ferron, Bruno Huck, Thierry Thierry, Virginie Gladyshev, Sergey 2016-08 application/pdf https://archimer.ifremer.fr/doc/00345/45569/45177.pdf https://doi.org/10.1016/j.pocean.2016.06.007 https://archimer.ifremer.fr/doc/00345/45569/ eng eng Pergamon-elsevier Science Ltd info:eu-repo/grantAgreement/EC/FP7/264879/EU//CARBOCHANGE https://archimer.ifremer.fr/doc/00345/45569/45177.pdf doi:10.1016/j.pocean.2016.06.007 https://archimer.ifremer.fr/doc/00345/45569/ 2016 Elsevier Ltd. All rights reserved. info:eu-repo/semantics/openAccess restricted use Progress In Oceanography (0079-6611) (Pergamon-elsevier Science Ltd), 2016-08 , Vol. 146 , P. 142-158 text Publication info:eu-repo/semantics/article 2016 ftarchimer https://doi.org/10.1016/j.pocean.2016.06.007 2021-09-23T20:28:36Z The decadal mean circulation in the northern North Atlantic was assessed for the early 21st century from repeated ship-based measurements along the Greenland-Portugal OVIDE line, from satellite altimetry and from earlier reported transports across 59.5°N and at the Greenland-Scotland sills. The remarkable quantitative agreement between all data sets allowed us to draw circulation pathways with a high level of confidence. The North Atlantic Current (NAC) system is composed of three main branches, referred to as the northern, central and southern branches, which were traced from the Mid-Atlantic Ridge (MAR), to the Irminger Sea, the Greenland-Scotland Ridge and the subtropical gyre. At OVIDE, the northern and central branches of the NAC fill the whole water column and their top-to-bottom integrated transports were estimated at 11.0 ± 3 Sv and 14.2 ± 6.4 Sv (1 Sv = 106 m3 s-1), respectively. Those two branches feed the cyclonic circulation in the Iceland Basin and the flow over the Reykjanes Ridge into the Irminger Sea. This cross-ridge flow was estimated at 11.3 ± 4.2 Sv westward, north of 58.5°N. The southern NAC branch is strongly surface-intensified and most of its top-to-bottom integrated transport, estimated at 16.6 ± 2 Sv, is found in the upper layer. It is composed of two parts: the northern part contributes to the flow over the Rockall Plateau and through the Rockall Trough towards the Iceland-Scotland Ridge; the southern part feeds the anticyclonic circulation towards the subtropical gyre. Summing over the three NAC branches, the top-to-bottom transport of the NAC across OVIDE was estimated at 41.8 ± 3.7 Sv. Because of the surface-intensification of the southern NAC branch, the intermediate water is transported to the northeast Atlantic mostly by the northern and central branches of the NAC (11.9 ± 1.8 Sv eastward). This water circulates cyclonically in the Iceland Basin and anticyclonically in the West European Basin, with similar transport intensities. In the deep layer of the Iceland Basin, Iceland-Scotland Overflow Water (ISOW) spreads southwestward along three pathways on the eastern flank of the Reykjanes Ridge. The associated transport was estimated at 3.2 ± 0.4 Sv. The two shallowest pathways turn around the Reykjanes Ridge towards the Irminger Sea where they head northward. A northeastward transport of deep water is observed in the deep extension of the northern and central branches of the NAC, east of the MAR. In the Irminger Sea our transport estimates for the Irminger Current, Irminger Gyre, East Greenland Irminger Current and Deep Western Boundary Current are in line with previous work. Article in Journal/Newspaper East Greenland Greenland Greenland-Scotland Ridge Iceland north atlantic current North Atlantic Northeast Atlantic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Mid-Atlantic Ridge Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) Rockall Plateau ENVELOPE(-18.833,-18.833,56.333,56.333) Rockall Trough ENVELOPE(-15.036,-15.036,53.825,53.825) West European Basin ENVELOPE(-28.000,-28.000,52.750,52.750) Progress in Oceanography 146 142 158 |