Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula

22 pages, 3 tables, 8 figures The hydrographic, chemical and biological conditions observed during spring and summer upwelling events off the NW Iberian Peninsula are compared. Meteorological data showed that northeasterly winds were of similar magnitude during both cruises, whereas the effect of up...

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Published in:Continental Shelf Research
Main Authors: Castro, Carmen G., Pérez, Fiz F., Álvarez-Salgado, Xosé Antón, Fraga, Fernando
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2000
Subjects:
Online Access:http://hdl.handle.net/10261/169655
https://doi.org/10.1016/S0278-4343(99)00071-0
id ftcsic:oai:digital.csic.es:10261/169655
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/169655 2024-02-11T10:06:35+01:00 Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula Castro, Carmen G. Pérez, Fiz F. Álvarez-Salgado, Xosé Antón Fraga, Fernando 2000 http://hdl.handle.net/10261/169655 https://doi.org/10.1016/S0278-4343(99)00071-0 en eng Elsevier https://doi.org/10.1016/S0278-4343(99)00071-0 Sí Continental Shelf Research 20(2): 189-210 (2000) 0278-4343 http://hdl.handle.net/10261/169655 doi:10.1016/S0278-4343(99)00071-0 1873-6955 none Oceanography Chemical and biological Nutrients Coastal upwelling NW Iberian Peninsula artículo http://purl.org/coar/resource_type/c_6501 2000 ftcsic https://doi.org/10.1016/S0278-4343(99)00071-0 2024-01-16T10:32:49Z 22 pages, 3 tables, 8 figures The hydrographic, chemical and biological conditions observed during spring and summer upwelling events off the NW Iberian Peninsula are compared. Meteorological data showed that northeasterly winds were of similar magnitude during both cruises, whereas the effect of upwelling was more intense during the spring than during the summer since stratification was weaker in spring. In the two situations the recurrent upwelling centre off Cape Finisterre (43°N, 9°W) divided the study area into two provinces. The two provinces differ in the occurrence and intensity of winds and in the origin of the upwelled water. Eastern North Atlantic Central Water of subpolar origin (ENACWP) was recorded north of Cape Finisterre during the two events. South of the Cape, ENACWP was observed during the spring situation, whereas ENACW of subtropical origin (ENACWT) prevailed during the summer cruise. Despite the different thermohaline and chemical properties of these two varieties of ENACW, similar nutrient levels were found in the two provinces due to strong remineralisation processes on the southern shelf. In addition, slower horizontal circulation at the southern edge of the upwelling centre and the influence of four large embayments (the Rı́as Baixas) south of Cape Finisterre, favoured chlorophyll accumulation south of the upwelling centre, which has similarly been observed in other upwelling centres around the world This study was supported from EU project No. MAST-CT90-0017. X.A.A.-S. was partially funded by a “Contrato de Incorporación” of the Spanish “Ministerio de Educación y Ciencia” Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Continental Shelf Research 20 2 189 210
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Oceanography
Chemical and biological
Nutrients
Coastal upwelling
NW Iberian Peninsula
spellingShingle Oceanography
Chemical and biological
Nutrients
Coastal upwelling
NW Iberian Peninsula
Castro, Carmen G.
Pérez, Fiz F.
Álvarez-Salgado, Xosé Antón
Fraga, Fernando
Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
topic_facet Oceanography
Chemical and biological
Nutrients
Coastal upwelling
NW Iberian Peninsula
description 22 pages, 3 tables, 8 figures The hydrographic, chemical and biological conditions observed during spring and summer upwelling events off the NW Iberian Peninsula are compared. Meteorological data showed that northeasterly winds were of similar magnitude during both cruises, whereas the effect of upwelling was more intense during the spring than during the summer since stratification was weaker in spring. In the two situations the recurrent upwelling centre off Cape Finisterre (43°N, 9°W) divided the study area into two provinces. The two provinces differ in the occurrence and intensity of winds and in the origin of the upwelled water. Eastern North Atlantic Central Water of subpolar origin (ENACWP) was recorded north of Cape Finisterre during the two events. South of the Cape, ENACWP was observed during the spring situation, whereas ENACW of subtropical origin (ENACWT) prevailed during the summer cruise. Despite the different thermohaline and chemical properties of these two varieties of ENACW, similar nutrient levels were found in the two provinces due to strong remineralisation processes on the southern shelf. In addition, slower horizontal circulation at the southern edge of the upwelling centre and the influence of four large embayments (the Rı́as Baixas) south of Cape Finisterre, favoured chlorophyll accumulation south of the upwelling centre, which has similarly been observed in other upwelling centres around the world This study was supported from EU project No. MAST-CT90-0017. X.A.A.-S. was partially funded by a “Contrato de Incorporación” of the Spanish “Ministerio de Educación y Ciencia” Peer reviewed
format Article in Journal/Newspaper
author Castro, Carmen G.
Pérez, Fiz F.
Álvarez-Salgado, Xosé Antón
Fraga, Fernando
author_facet Castro, Carmen G.
Pérez, Fiz F.
Álvarez-Salgado, Xosé Antón
Fraga, Fernando
author_sort Castro, Carmen G.
title Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
title_short Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
title_full Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
title_fullStr Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
title_full_unstemmed Coupling between thermohaline and chemical fields during two contrasting upwelling events off the NW Iberian Peninsula
title_sort coupling between thermohaline and chemical fields during two contrasting upwelling events off the nw iberian peninsula
publisher Elsevier
publishDate 2000
url http://hdl.handle.net/10261/169655
https://doi.org/10.1016/S0278-4343(99)00071-0
genre North Atlantic
genre_facet North Atlantic
op_relation https://doi.org/10.1016/S0278-4343(99)00071-0

Continental Shelf Research 20(2): 189-210 (2000)
0278-4343
http://hdl.handle.net/10261/169655
doi:10.1016/S0278-4343(99)00071-0
1873-6955
op_rights none
op_doi https://doi.org/10.1016/S0278-4343(99)00071-0
container_title Continental Shelf Research
container_volume 20
container_issue 2
container_start_page 189
op_container_end_page 210
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