Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud
Autor(a) principal: | |
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Data de Publicação: | 1966 |
Tipo de documento: | Artigo |
Idioma: | spa |
Título da fonte: | Boletim do Instituto Oceanográfico |
Texto Completo: | https://www.revistas.usp.br/biocean/article/view/27781 |
Resumo: | The distribution of oxygen in an area of the South Atlantic Ocean has been studied. The area is limited by the Argentinian continental slope and the 45º W meridian and from 35º S to 47º S. The distribution of oxygen in studied in relation with the salinity distribution in seven horizontal levels and one vertical profile. The oxygen distribution in the area of the Subtropical Convergence has a characteristic pattern that seems to be very useful in the determination of the Convergence. The Subtropical Convergence was situated between the oceanographic station where was found the maximum salinity and the maximum oxygen (negative) horizontal gradients. The maximum fluctuation of the Subtropical Convergence area is situated immediately East of Malvinas Current, where its desplacement N-S between winter and spring is, at least, 200 nautical miles. The water sunk at the Subtropical Convergence can be followed by its oxygen content. The intermediate maximum of oxygen is not coincident with the depth of salinity minimum characteristic of the núcleos of S. A. waters. A hipothesis to explain this is given. |
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Boletim do Instituto Oceanográfico |
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Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud The distribution of oxygen in an area of the South Atlantic Ocean has been studied. The area is limited by the Argentinian continental slope and the 45º W meridian and from 35º S to 47º S. The distribution of oxygen in studied in relation with the salinity distribution in seven horizontal levels and one vertical profile. The oxygen distribution in the area of the Subtropical Convergence has a characteristic pattern that seems to be very useful in the determination of the Convergence. The Subtropical Convergence was situated between the oceanographic station where was found the maximum salinity and the maximum oxygen (negative) horizontal gradients. The maximum fluctuation of the Subtropical Convergence area is situated immediately East of Malvinas Current, where its desplacement N-S between winter and spring is, at least, 200 nautical miles. The water sunk at the Subtropical Convergence can be followed by its oxygen content. The intermediate maximum of oxygen is not coincident with the depth of salinity minimum characteristic of the núcleos of S. A. waters. A hipothesis to explain this is given. Universidade de São Paulo. Instituto Oceanográfico1966-12-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://www.revistas.usp.br/biocean/article/view/2778110.1590/S0373-55241967000100006Boletim do Instituto Oceanográfico; v. 16 n. 1 (1967); 67-85 Boletim do Instituto Oceanografico; Vol. 16 No. 1 (1967); 67-85 Boletim do Instituto Oceanográfico; Vol. 16 Núm. 1 (1967); 67-85 2316-89510373-5524reponame:Boletim do Instituto Oceanográficoinstname:Instituto Oceanográfico da Universidade de São Paulo (IOUSP)instacron:USPspahttps://www.revistas.usp.br/biocean/article/view/27781/29553Pizarro, Mariano Javierinfo:eu-repo/semantics/openAccess2012-06-24T14:50:50Zoai:revistas.usp.br:article/27781Revistahttps://www.revistas.usp.br/bioceanPUBhttps://www.revistas.usp.br/biocean/oaiamspires@usp.br0373-55240373-5524opendoar:2012-06-24T14:50:50Boletim do Instituto Oceanográfico - Instituto Oceanográfico da Universidade de São Paulo (IOUSP)false |
dc.title.none.fl_str_mv |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
title |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
spellingShingle |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud Pizarro, Mariano Javier |
title_short |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
title_full |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
title_fullStr |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
title_full_unstemmed |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
title_sort |
Distribución del oxígeno disuelto en la zona oeste de la Convergencia Subtropical del Atlantico Sud |
author |
Pizarro, Mariano Javier |
author_facet |
Pizarro, Mariano Javier |
author_role |
author |
dc.contributor.author.fl_str_mv |
Pizarro, Mariano Javier |
description |
The distribution of oxygen in an area of the South Atlantic Ocean has been studied. The area is limited by the Argentinian continental slope and the 45º W meridian and from 35º S to 47º S. The distribution of oxygen in studied in relation with the salinity distribution in seven horizontal levels and one vertical profile. The oxygen distribution in the area of the Subtropical Convergence has a characteristic pattern that seems to be very useful in the determination of the Convergence. The Subtropical Convergence was situated between the oceanographic station where was found the maximum salinity and the maximum oxygen (negative) horizontal gradients. The maximum fluctuation of the Subtropical Convergence area is situated immediately East of Malvinas Current, where its desplacement N-S between winter and spring is, at least, 200 nautical miles. The water sunk at the Subtropical Convergence can be followed by its oxygen content. The intermediate maximum of oxygen is not coincident with the depth of salinity minimum characteristic of the núcleos of S. A. waters. A hipothesis to explain this is given. |
publishDate |
1966 |
dc.date.none.fl_str_mv |
1966-12-31 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://www.revistas.usp.br/biocean/article/view/27781 10.1590/S0373-55241967000100006 |
url |
https://www.revistas.usp.br/biocean/article/view/27781 |
identifier_str_mv |
10.1590/S0373-55241967000100006 |
dc.language.iso.fl_str_mv |
spa |
language |
spa |
dc.relation.none.fl_str_mv |
https://www.revistas.usp.br/biocean/article/view/27781/29553 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade de São Paulo. Instituto Oceanográfico |
publisher.none.fl_str_mv |
Universidade de São Paulo. Instituto Oceanográfico |
dc.source.none.fl_str_mv |
Boletim do Instituto Oceanográfico; v. 16 n. 1 (1967); 67-85 Boletim do Instituto Oceanografico; Vol. 16 No. 1 (1967); 67-85 Boletim do Instituto Oceanográfico; Vol. 16 Núm. 1 (1967); 67-85 2316-8951 0373-5524 reponame:Boletim do Instituto Oceanográfico instname:Instituto Oceanográfico da Universidade de São Paulo (IOUSP) instacron:USP |
instname_str |
Instituto Oceanográfico da Universidade de São Paulo (IOUSP) |
instacron_str |
USP |
institution |
USP |
reponame_str |
Boletim do Instituto Oceanográfico |
collection |
Boletim do Instituto Oceanográfico |
repository.name.fl_str_mv |
Boletim do Instituto Oceanográfico - Instituto Oceanográfico da Universidade de São Paulo (IOUSP) |
repository.mail.fl_str_mv |
amspires@usp.br |
_version_ |
1797049930215325696 |