Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986

32 pages, 15 figures, 3 tables. The coastal transition zone and adjacent continental shelf of the Iberian upwelling system was studied in September 1986, during the seasonal transition from upwelling-favored to downwelling-favored winds. The most striking features in the coastal transition zone were...

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Published in:Journal of Marine Research
Main Authors: Castro, Carmen G., Álvarez-Salgado, Xosé Antón, Figueiras, F. G., Pérez, Fiz F., Fraga, Fernando
Format: Article in Journal/Newspaper
Language:English
Published: Yale University 1997
Subjects:
Online Access:http://hdl.handle.net/10261/26136
https://doi.org/10.1357/0022240973224436
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spelling ftcsic:oai:digital.csic.es:10261/26136 2024-02-11T10:06:40+01:00 Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986 Castro, Carmen G. Álvarez-Salgado, Xosé Antón Figueiras, F. G. Pérez, Fiz F. Fraga, Fernando 1997-03 1994613 bytes application/pdf http://hdl.handle.net/10261/26136 https://doi.org/10.1357/0022240973224436 en eng Yale University http://dx.doi.org/10.1357/0022240973224436 Journal of Marine Research 55(2): 321-352 (1997) 0022-2402 http://hdl.handle.net/10261/26136 doi:10.1357/0022240973224436 open artículo http://purl.org/coar/resource_type/c_6501 1997 ftcsic https://doi.org/10.1357/0022240973224436 2024-01-16T09:27:37Z 32 pages, 15 figures, 3 tables. The coastal transition zone and adjacent continental shelf of the Iberian upwelling system was studied in September 1986, during the seasonal transition from upwelling-favored to downwelling-favored winds. The most striking features in the coastal transition zone were: (1) a poleward flow of high salinity Eastern North Atlantic Central Water (subtropical) off the Rías Baixas (Galician western coast); and (2) an anticyclonic eddy off Cape Ortegal (Galician northern coast). Chemical and biological similarities between both structures, clearly different from the surrounding oceanic waters, suggest that the eddy was an isolated and aged parcel of water originating from the poleward flow. The continental shelf was characterized by: (1) outwelling of chlorophyll-rich waters from the four large coastal embayments (the “Rías Baixas”) in the western coast and; (2) an upwelling front off the northern coast. The coexistence of opposite hydrographic structures, as the poleward flow and the upwelling front, was the consequence of transitional wind conditions in September–October, and we hypothesized transitional conditions to be crucial for the development of the eddy. Both the poleward flow and the eddy precluded the shelf-edge exchange of microplankton populations developed over the shelf, leading to massive in situ sedimentation and subsequent nutrient mineralization over the shelf. Support for this work came from CICYT Grant No. 84-0068. A fellowship from the Spanish Ministerio de Educación y Ciencia allowed C.G.C. to carry out this work. X.A.A.S. and F.F.P. were also supported for this work by the project EU-MAS2-CT93-65. Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Journal of Marine Research 55 2 321 352
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collection Digital.CSIC (Spanish National Research Council)
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language English
description 32 pages, 15 figures, 3 tables. The coastal transition zone and adjacent continental shelf of the Iberian upwelling system was studied in September 1986, during the seasonal transition from upwelling-favored to downwelling-favored winds. The most striking features in the coastal transition zone were: (1) a poleward flow of high salinity Eastern North Atlantic Central Water (subtropical) off the Rías Baixas (Galician western coast); and (2) an anticyclonic eddy off Cape Ortegal (Galician northern coast). Chemical and biological similarities between both structures, clearly different from the surrounding oceanic waters, suggest that the eddy was an isolated and aged parcel of water originating from the poleward flow. The continental shelf was characterized by: (1) outwelling of chlorophyll-rich waters from the four large coastal embayments (the “Rías Baixas”) in the western coast and; (2) an upwelling front off the northern coast. The coexistence of opposite hydrographic structures, as the poleward flow and the upwelling front, was the consequence of transitional wind conditions in September–October, and we hypothesized transitional conditions to be crucial for the development of the eddy. Both the poleward flow and the eddy precluded the shelf-edge exchange of microplankton populations developed over the shelf, leading to massive in situ sedimentation and subsequent nutrient mineralization over the shelf. Support for this work came from CICYT Grant No. 84-0068. A fellowship from the Spanish Ministerio de Educación y Ciencia allowed C.G.C. to carry out this work. X.A.A.S. and F.F.P. were also supported for this work by the project EU-MAS2-CT93-65. Peer reviewed
format Article in Journal/Newspaper
author Castro, Carmen G.
Álvarez-Salgado, Xosé Antón
Figueiras, F. G.
Pérez, Fiz F.
Fraga, Fernando
spellingShingle Castro, Carmen G.
Álvarez-Salgado, Xosé Antón
Figueiras, F. G.
Pérez, Fiz F.
Fraga, Fernando
Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
author_facet Castro, Carmen G.
Álvarez-Salgado, Xosé Antón
Figueiras, F. G.
Pérez, Fiz F.
Fraga, Fernando
author_sort Castro, Carmen G.
title Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
title_short Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
title_full Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
title_fullStr Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
title_full_unstemmed Transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the Iberian upwelling system (NW Spain) in September 1986
title_sort transient hydrographic and chemical conditions affecting microplankton populations in the coastal transition zone of the iberian upwelling system (nw spain) in september 1986
publisher Yale University
publishDate 1997
url http://hdl.handle.net/10261/26136
https://doi.org/10.1357/0022240973224436
genre North Atlantic
genre_facet North Atlantic
op_relation http://dx.doi.org/10.1357/0022240973224436
Journal of Marine Research 55(2): 321-352 (1997)
0022-2402
http://hdl.handle.net/10261/26136
doi:10.1357/0022240973224436
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container_title Journal of Marine Research
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