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 curr...

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Guardado en:
Detalles Bibliográficos
Publicado: 2000
Materias:
salinity
temperature
thermohaline structure
water mass
South America
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_21699291_v105_nC3_p6565_Piola
http://hdl.handle.net/20.500.12110/paper_21699291_v105_nC3_p6565_Piola
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_21699291_v105_nC3_p6565_Piola
record_format dspace
spelling paper:paper_21699291_v105_nC3_p6565_Piola2025-07-30T19:10:18Z Subtropical shelf front off eastern South America salinity temperature thermohaline structure water mass 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 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 Rio 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, the Subtropical Shelf Front appears as an extension of the Brazil-Malvinas Confluence over the continental shelf of South America. Thus the location of the Subtropical Shelf Front may be linked to the migrations of the separation point of the Brazil-Malvinas Confluence from the continental slope. Copyright 2000 by the American Geophysical Union. 2000 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_21699291_v105_nC3_p6565_Piola http://hdl.handle.net/20.500.12110/paper_21699291_v105_nC3_p6565_Piola
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic salinity
temperature
thermohaline structure
water mass
South America
spellingShingle salinity
temperature
thermohaline structure
water mass
South America
Subtropical shelf front off eastern South America
topic_facet salinity
temperature
thermohaline structure
water mass
South America
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 Rio 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, the Subtropical Shelf Front appears as an extension of the Brazil-Malvinas Confluence over the continental shelf of South America. Thus the location of the Subtropical Shelf Front may be linked to the migrations of the separation point of the Brazil-Malvinas Confluence from the continental slope. Copyright 2000 by the American Geophysical Union.
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
publishDate 2000
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_21699291_v105_nC3_p6565_Piola
http://hdl.handle.net/20.500.12110/paper_21699291_v105_nC3_p6565_Piola
_version_ 1840324205677117440

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