Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic
36 pages, 7 figures, 4 tables, 1 appendix. A transoceanic hydrographic section across the North Atlantic Subpolar gyre from Vigo (northwestern Iberian Peninsula) to Cape Farewell (south of Greenland) was sampled in summer 1997 as part of the World Ocean Circulation Experiment program (WOCE A25, 4x c...
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ftcsic:oai:digital.csic.es:10261/26056 2024-02-11T10:02:50+01:00 Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic Álvarez, Marta Bryden, Harry L. Pérez, Fiz F. Ríos, Aida F. Rosón, Gabriel 2002-03 789682 bytes application/pdf http://hdl.handle.net/10261/26056 en eng Yale University http://jmr.publisher.ingentaconnect.com/content/jmr/jmr/2002/00000060/00000002/art00001 Journal of Marine Research 60(2): 191-226 (2002) 0022-2402 http://hdl.handle.net/10261/26056 open artículo http://purl.org/coar/resource_type/c_6501 2002 ftcsic 2024-01-16T09:27:35Z 36 pages, 7 figures, 4 tables, 1 appendix. A transoceanic hydrographic section across the North Atlantic Subpolar gyre from Vigo (northwestern Iberian Peninsula) to Cape Farewell (south of Greenland) was sampled in summer 1997 as part of the World Ocean Circulation Experiment program (WOCE A25, 4x cruise). The circulation pattern across the 4x section is diagnosed using inverse methods. The flow is constrained with measured mass transports at specific sites, while conserving mass and salt for the region north of the section and forcing the silicate flux to a reasonable value. The fluxes of physical (heat and freshwater) and chemical (nutrients and oxygen) properties are estimated and decomposed into barotropic, baroclinic and horizontal components. The heat transport amounts to 0.65 ± 0.1 PW poleward, with 54% and 45% of the flux due to the baroclinic (or overturning) and horizontal circulation, respectively. From the salt conservation, an equatorward freshwater transport of-0.4 ± 1.5 Sv is estimated, resulting from net precipitation plus runoff over the North Atlantic Ocean north of the section. The Subpolar gyre exports nutrients and oxygen southward toward the Subtropical ocean at rates of -50 ± 19, -6 ± 2, -26 ± 15 and -1992 ± 440 kmol s-1 for nitrate, phosphate, silicate and oxygen, respectively. The main mechanism responsible for the nutrient transport is the overturning cell, whereas oxygen is mainly transported southward due to the large-scale horizontal circulation. Combining our fluxes with those from the 36N section (Rintoul and Wunsch, 1991) allows us to examine budgets of physical (heat and freshwater) and chemical (nitrogen and oxygen) properties for an enclosed area of the Subpolar and Temperate North Atlantic. The tentative nitrogen budget for the box between the 4x and the 36N sections suggests that the Temperate North Atlantic is exporting organic nitrogen toward the Subtropical and the Subpolar provinces, which is consistent with indirect evidence. The cruise was primarily supported by the ... Article in Journal/Newspaper Cape Farewell Greenland North Atlantic Digital.CSIC (Spanish National Research Council) Greenland |
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Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
description |
36 pages, 7 figures, 4 tables, 1 appendix. A transoceanic hydrographic section across the North Atlantic Subpolar gyre from Vigo (northwestern Iberian Peninsula) to Cape Farewell (south of Greenland) was sampled in summer 1997 as part of the World Ocean Circulation Experiment program (WOCE A25, 4x cruise). The circulation pattern across the 4x section is diagnosed using inverse methods. The flow is constrained with measured mass transports at specific sites, while conserving mass and salt for the region north of the section and forcing the silicate flux to a reasonable value. The fluxes of physical (heat and freshwater) and chemical (nutrients and oxygen) properties are estimated and decomposed into barotropic, baroclinic and horizontal components. The heat transport amounts to 0.65 ± 0.1 PW poleward, with 54% and 45% of the flux due to the baroclinic (or overturning) and horizontal circulation, respectively. From the salt conservation, an equatorward freshwater transport of-0.4 ± 1.5 Sv is estimated, resulting from net precipitation plus runoff over the North Atlantic Ocean north of the section. The Subpolar gyre exports nutrients and oxygen southward toward the Subtropical ocean at rates of -50 ± 19, -6 ± 2, -26 ± 15 and -1992 ± 440 kmol s-1 for nitrate, phosphate, silicate and oxygen, respectively. The main mechanism responsible for the nutrient transport is the overturning cell, whereas oxygen is mainly transported southward due to the large-scale horizontal circulation. Combining our fluxes with those from the 36N section (Rintoul and Wunsch, 1991) allows us to examine budgets of physical (heat and freshwater) and chemical (nitrogen and oxygen) properties for an enclosed area of the Subpolar and Temperate North Atlantic. The tentative nitrogen budget for the box between the 4x and the 36N sections suggests that the Temperate North Atlantic is exporting organic nitrogen toward the Subtropical and the Subpolar provinces, which is consistent with indirect evidence. The cruise was primarily supported by the ... |
format |
Article in Journal/Newspaper |
author |
Álvarez, Marta Bryden, Harry L. Pérez, Fiz F. Ríos, Aida F. Rosón, Gabriel |
spellingShingle |
Álvarez, Marta Bryden, Harry L. Pérez, Fiz F. Ríos, Aida F. Rosón, Gabriel Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
author_facet |
Álvarez, Marta Bryden, Harry L. Pérez, Fiz F. Ríos, Aida F. Rosón, Gabriel |
author_sort |
Álvarez, Marta |
title |
Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
title_short |
Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
title_full |
Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
title_fullStr |
Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
title_full_unstemmed |
Physical and biogeochemical fluxes and net budgets in the subpolar and temperate North Atlantic |
title_sort |
physical and biogeochemical fluxes and net budgets in the subpolar and temperate north atlantic |
publisher |
Yale University |
publishDate |
2002 |
url |
http://hdl.handle.net/10261/26056 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Cape Farewell Greenland North Atlantic |
genre_facet |
Cape Farewell Greenland North Atlantic |
op_relation |
http://jmr.publisher.ingentaconnect.com/content/jmr/jmr/2002/00000060/00000002/art00001 Journal of Marine Research 60(2): 191-226 (2002) 0022-2402 http://hdl.handle.net/10261/26056 |
op_rights |
open |
_version_ |
1790598915042574336 |