Subtropical Shelf Front off eastern South America
Historical hydrographic data from the continental shelf off eastern South America are used to examine the thermohaline properties of the water masses in the region between 20°S and 40°S. The continental shelf water masses are originated by dilution of open ocean waters of the western boundary curren...
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ftconicet:oai:ri.conicet.gov.ar:11336/71691 2023-10-09T21:55:56+02:00 Subtropical Shelf Front off eastern South America Piola, Alberto Ricardo Campos, Edmo Möller, Osmar O. Charo, Marcela Martinez, Carlos application/pdf http://hdl.handle.net/11336/71691 eng eng American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/1999JC000300 info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999JC000300 http://hdl.handle.net/11336/71691 Piola, Alberto Ricardo; Campos, Edmo; Möller, Osmar O.; Charo, Marcela; Martinez, Carlos; Subtropical Shelf Front off eastern South America; American Geophysical Union; Journal of Geophysical Research; 105; C3; 3-2000; 6565-6578 0148-0227 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1029/1999JC000300 2023-09-24T20:04:21Z Historical hydrographic data from the continental shelf off eastern South America are used to examine the thermohaline properties of the water masses in the region between 20°S and 40°S. The continental shelf water masses are originated by dilution of open ocean waters of the western boundary currents of the South Atlantic Ocean. On the basis of temperature‐salinity relation, two distinct water masses are identified, namely, the Subantarctic Shelf Water and the Subtropical Shelf Water. Subantarctic Shelf Water originates by dilution of Subantarctic Water, primarily in the southeast Pacific, due to excess precipitation and continental runoff and enters the continental shelf near 55°S. The Subtropical Shelf Water is modified South Atlantic Central Water diluted by continental runoff from the coast of Brazil. In addition, substantial dilution of the upper shelf waters takes place at the mouth of Río de la Plata (approximately located at 36°S) and, in a lesser extent, at the Patos‐Mirim Lagoon (at 32°S). The Río de la Plata and the Patos outflows form a low‐salinity tongue that caps the shelf water leading to a salinity decrease to values <30. The low‐salinity tongue extends northward over the shelf penetrating farther north in winter than in summer. The extent of the low‐salinity water has a strong impact on the vertical stratification and acts to limit winter convection to the layer above the halocline. There is little or no indication of mixing between Subantarctic Shelf Water and Subtropical Shelf Water. An intense temperature, salinity, and nutrient front separates these water masses. The front is oriented along the north‐south direction, located on average near the 50 m isobath at 32°S and extends southward toward the shelf break near 36°S. Between 32° and 34°S the Subtropical Shelf Front follows the 100 to 200 m isobaths and separates Subantarctic Shelf Water from the oceanic South Atlantic Central Water. On the basis of the temperature and salinity distributions, beneath the low‐salinity surface layer, ... Article in Journal/Newspaper South Atlantic Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Pacific Journal of Geophysical Research: Oceans 105 C3 6565 6578 |
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Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
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https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Piola, Alberto Ricardo Campos, Edmo Möller, Osmar O. Charo, Marcela Martinez, Carlos Subtropical Shelf Front off eastern South America |
topic_facet |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
Historical hydrographic data from the continental shelf off eastern South America are used to examine the thermohaline properties of the water masses in the region between 20°S and 40°S. The continental shelf water masses are originated by dilution of open ocean waters of the western boundary currents of the South Atlantic Ocean. On the basis of temperature‐salinity relation, two distinct water masses are identified, namely, the Subantarctic Shelf Water and the Subtropical Shelf Water. Subantarctic Shelf Water originates by dilution of Subantarctic Water, primarily in the southeast Pacific, due to excess precipitation and continental runoff and enters the continental shelf near 55°S. The Subtropical Shelf Water is modified South Atlantic Central Water diluted by continental runoff from the coast of Brazil. In addition, substantial dilution of the upper shelf waters takes place at the mouth of Río de la Plata (approximately located at 36°S) and, in a lesser extent, at the Patos‐Mirim Lagoon (at 32°S). The Río de la Plata and the Patos outflows form a low‐salinity tongue that caps the shelf water leading to a salinity decrease to values <30. The low‐salinity tongue extends northward over the shelf penetrating farther north in winter than in summer. The extent of the low‐salinity water has a strong impact on the vertical stratification and acts to limit winter convection to the layer above the halocline. There is little or no indication of mixing between Subantarctic Shelf Water and Subtropical Shelf Water. An intense temperature, salinity, and nutrient front separates these water masses. The front is oriented along the north‐south direction, located on average near the 50 m isobath at 32°S and extends southward toward the shelf break near 36°S. Between 32° and 34°S the Subtropical Shelf Front follows the 100 to 200 m isobaths and separates Subantarctic Shelf Water from the oceanic South Atlantic Central Water. On the basis of the temperature and salinity distributions, beneath the low‐salinity surface layer, ... |
format |
Article in Journal/Newspaper |
author |
Piola, Alberto Ricardo Campos, Edmo Möller, Osmar O. Charo, Marcela Martinez, Carlos |
author_facet |
Piola, Alberto Ricardo Campos, Edmo Möller, Osmar O. Charo, Marcela Martinez, Carlos |
author_sort |
Piola, Alberto Ricardo |
title |
Subtropical Shelf Front off eastern South America |
title_short |
Subtropical Shelf Front off eastern South America |
title_full |
Subtropical Shelf Front off eastern South America |
title_fullStr |
Subtropical Shelf Front off eastern South America |
title_full_unstemmed |
Subtropical Shelf Front off eastern South America |
title_sort |
subtropical shelf front off eastern south america |
publisher |
American Geophysical Union |
url |
http://hdl.handle.net/11336/71691 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/1999JC000300 info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999JC000300 http://hdl.handle.net/11336/71691 Piola, Alberto Ricardo; Campos, Edmo; Möller, Osmar O.; Charo, Marcela; Martinez, Carlos; Subtropical Shelf Front off eastern South America; American Geophysical Union; Journal of Geophysical Research; 105; C3; 3-2000; 6565-6578 0148-0227 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1029/1999JC000300 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
105 |
container_issue |
C3 |
container_start_page |
6565 |
op_container_end_page |
6578 |
_version_ |
1779320205159170048 |