Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season
9 pages, 9 figures, 1 table During the Galicia X cruise, from May to October 1989 an intensive collection of hydrographic data was carried out at a single station on the shelf off the western coast of Galicia. It allows us to follow the response of the water column to the intermittent equatorward wi...
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American Geophysical Union
1993
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Online Access: | http://hdl.handle.net/10261/169631 https://doi.org/10.1029/93JC00458 |
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ftcsic:oai:digital.csic.es:10261/169631 2024-02-11T10:06:24+01:00 Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season Álvarez-Salgado, Xosé Antón Rosón, Gabriel Pérez, Fiz F. Pazos, Yolanda 1993 http://hdl.handle.net/10261/169631 https://doi.org/10.1029/93JC00458 en eng American Geophysical Union Publisher's version https://doi.org/10.1029/93JC00458 Sí Journal of Geophysical Research - Part C - Oceans 98(C8): 14447–14455 (1993) 2169-9291 http://hdl.handle.net/10261/169631 doi:10.1029/93JC00458 open artículo http://purl.org/coar/resource_type/c_6501 1993 ftcsic https://doi.org/10.1029/93JC00458 2024-01-16T10:32:49Z 9 pages, 9 figures, 1 table During the Galicia X cruise, from May to October 1989 an intensive collection of hydrographic data was carried out at a single station on the shelf off the western coast of Galicia. It allows us to follow the response of the water column to the intermittent equatorward wind stress during the upwelling season. Upwelling events occur with biweekly periodicity, bringing Eastern North Atlantic Water (ENAW) to the subsurface layer at our station. A trend of the thermohaline properties of the upwelled water to increase in time was observed. This seems to be mostly due to the southwestward displacement of the origin of this water mass during the year. Although the saltier and warmer ENAW is less nutrient‐rich, nutrient levels increase because of the rapid remineralization of organic matter from the Rías, which takes place in the bottom water on the shelf Support for this work came from CICYT grant MAR88-0245 and Conselleria de Pesca de la Xunta de Galicia. Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Journal of Geophysical Research 98 C8 14447 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
description |
9 pages, 9 figures, 1 table During the Galicia X cruise, from May to October 1989 an intensive collection of hydrographic data was carried out at a single station on the shelf off the western coast of Galicia. It allows us to follow the response of the water column to the intermittent equatorward wind stress during the upwelling season. Upwelling events occur with biweekly periodicity, bringing Eastern North Atlantic Water (ENAW) to the subsurface layer at our station. A trend of the thermohaline properties of the upwelled water to increase in time was observed. This seems to be mostly due to the southwestward displacement of the origin of this water mass during the year. Although the saltier and warmer ENAW is less nutrient‐rich, nutrient levels increase because of the rapid remineralization of organic matter from the Rías, which takes place in the bottom water on the shelf Support for this work came from CICYT grant MAR88-0245 and Conselleria de Pesca de la Xunta de Galicia. Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Álvarez-Salgado, Xosé Antón Rosón, Gabriel Pérez, Fiz F. Pazos, Yolanda |
spellingShingle |
Álvarez-Salgado, Xosé Antón Rosón, Gabriel Pérez, Fiz F. Pazos, Yolanda Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
author_facet |
Álvarez-Salgado, Xosé Antón Rosón, Gabriel Pérez, Fiz F. Pazos, Yolanda |
author_sort |
Álvarez-Salgado, Xosé Antón |
title |
Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
title_short |
Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
title_full |
Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
title_fullStr |
Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
title_full_unstemmed |
Hydrographic variability off the Rias Baixas (NW Spain) during the upwelling season |
title_sort |
hydrographic variability off the rias baixas (nw spain) during the upwelling season |
publisher |
American Geophysical Union |
publishDate |
1993 |
url |
http://hdl.handle.net/10261/169631 https://doi.org/10.1029/93JC00458 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Publisher's version https://doi.org/10.1029/93JC00458 Sí Journal of Geophysical Research - Part C - Oceans 98(C8): 14447–14455 (1993) 2169-9291 http://hdl.handle.net/10261/169631 doi:10.1029/93JC00458 |
op_rights |
open |
op_doi |
https://doi.org/10.1029/93JC00458 |
container_title |
Journal of Geophysical Research |
container_volume |
98 |
container_issue |
C8 |
container_start_page |
14447 |
_version_ |
1790604104040448000 |