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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Main Authors: Álvarez, Marta, Bryden, Harry L., Pérez, Fiz F., Ríos, Aida F., Rosón, Gabriel
Format: Article in Journal/Newspaper
Language:English
Published: Yale University 2002
Subjects:
Online Access:http://hdl.handle.net/10261/26056
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spelling 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
institution 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
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