Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990
The Confluence 3 cruise during February 1990 provides the first hydrographic survey of the Brazil-Malvinas Confluence region ever obtained with such a refined spatial resolution over the continental slope. The closely spaced stations on the slope permit the observation of the branching of the Malvin...
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1995
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Online Access: | https://archimer.ifremer.fr/doc/00481/59318/62077.pdf https://doi.org/10.1029/94JC02864 https://archimer.ifremer.fr/doc/00481/59318/ |
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ftarchimer:oai:archimer.ifremer.fr:59318 2023-05-15T17:13:53+02:00 Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 Provost, Christine Gana, S Garcon, V Maamaatuaiahutapu, K England, Mh 1995-06 application/pdf https://archimer.ifremer.fr/doc/00481/59318/62077.pdf https://doi.org/10.1029/94JC02864 https://archimer.ifremer.fr/doc/00481/59318/ eng eng Amer Geophysical Union https://archimer.ifremer.fr/doc/00481/59318/62077.pdf doi:10.1029/94JC02864 https://archimer.ifremer.fr/doc/00481/59318/ info:eu-repo/semantics/openAccess restricted use Journal Of Geophysical Research-oceans (0148-0227) (Amer Geophysical Union), 1995-06 , Vol. 100 , N. C6 , P. 10655-10678 text Publication info:eu-repo/semantics/article 1995 ftarchimer https://doi.org/10.1029/94JC02864 2021-09-23T20:32:13Z The Confluence 3 cruise during February 1990 provides the first hydrographic survey of the Brazil-Malvinas Confluence region ever obtained with such a refined spatial resolution over the continental slope. The closely spaced stations on the slope permit the observation of the branching of the Malvinas Current near 40 degrees S. The eastern branch returns south, while the eastern one is squeezed along the continental slope, managing to continue northward as far north as 36.3 degrees S. The Brazil-Malvinas (B-M) front has a north-south orientation on the slope and an east-west direction offshore. The B-M front is marked by very strong gradients in temperature and salinity. Fine scale vertical structures and intrusions are numerous in the vicinity of the front and cover a wide range of scales. The largest intrusion observed is a 50-km-wide, 350-m-thick subsurface lense of Thermocline Water present on the Malvinas side of the front. The fine scale vertical structure results in very high temperature and salinity fluxes across the front of the order of 2 x 10(-2)degrees C m(-1) s(-1) and 10(-3) psu m(-1) s(-1). Two types of mode waters are identified as follows: Subtropical Mode Waters north of the front and Subantarctic Mode Waters on both sides of the front. The Subantarctic mode waters (SAMW) appear to recirculate near the western boundary. A young variety of SAMW (lighter, very oxygenated) propagates northward along the continental slope with the Malvinas Current. It detaches from the coast near 37 degrees S and is strongly altered in the frontal region. It is then entrained southward with the Malvinas return flow and Brazil Current extension. The Confluence 3 hydrographic survey provides a good description of the North Atlantic Deep Water (NADW) and Circumpolar Deep Water (CDW) convergence near the western boundary. Strong, fine scale vertical structures are observed in the vicinity of the NADW/CDW front, and the associated temperature and salinity fluxes induced are strong, 5 x 10(-3)degrees cm/s and 2 x 10(-3) psu.m/s, respectively. Article in Journal/Newspaper NADW North Atlantic Deep Water North Atlantic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Austral Journal of Geophysical Research 100 C6 10655 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
The Confluence 3 cruise during February 1990 provides the first hydrographic survey of the Brazil-Malvinas Confluence region ever obtained with such a refined spatial resolution over the continental slope. The closely spaced stations on the slope permit the observation of the branching of the Malvinas Current near 40 degrees S. The eastern branch returns south, while the eastern one is squeezed along the continental slope, managing to continue northward as far north as 36.3 degrees S. The Brazil-Malvinas (B-M) front has a north-south orientation on the slope and an east-west direction offshore. The B-M front is marked by very strong gradients in temperature and salinity. Fine scale vertical structures and intrusions are numerous in the vicinity of the front and cover a wide range of scales. The largest intrusion observed is a 50-km-wide, 350-m-thick subsurface lense of Thermocline Water present on the Malvinas side of the front. The fine scale vertical structure results in very high temperature and salinity fluxes across the front of the order of 2 x 10(-2)degrees C m(-1) s(-1) and 10(-3) psu m(-1) s(-1). Two types of mode waters are identified as follows: Subtropical Mode Waters north of the front and Subantarctic Mode Waters on both sides of the front. The Subantarctic mode waters (SAMW) appear to recirculate near the western boundary. A young variety of SAMW (lighter, very oxygenated) propagates northward along the continental slope with the Malvinas Current. It detaches from the coast near 37 degrees S and is strongly altered in the frontal region. It is then entrained southward with the Malvinas return flow and Brazil Current extension. The Confluence 3 hydrographic survey provides a good description of the North Atlantic Deep Water (NADW) and Circumpolar Deep Water (CDW) convergence near the western boundary. Strong, fine scale vertical structures are observed in the vicinity of the NADW/CDW front, and the associated temperature and salinity fluxes induced are strong, 5 x 10(-3)degrees cm/s and 2 x 10(-3) psu.m/s, respectively. |
format |
Article in Journal/Newspaper |
author |
Provost, Christine Gana, S Garcon, V Maamaatuaiahutapu, K England, Mh |
spellingShingle |
Provost, Christine Gana, S Garcon, V Maamaatuaiahutapu, K England, Mh Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
author_facet |
Provost, Christine Gana, S Garcon, V Maamaatuaiahutapu, K England, Mh |
author_sort |
Provost, Christine |
title |
Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
title_short |
Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
title_full |
Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
title_fullStr |
Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
title_full_unstemmed |
Hydrographic conditions in the Brazil‐Malvinas Confluence during austral summer 1990 |
title_sort |
hydrographic conditions in the brazil‐malvinas confluence during austral summer 1990 |
publisher |
Amer Geophysical Union |
publishDate |
1995 |
url |
https://archimer.ifremer.fr/doc/00481/59318/62077.pdf https://doi.org/10.1029/94JC02864 https://archimer.ifremer.fr/doc/00481/59318/ |
geographic |
Austral |
geographic_facet |
Austral |
genre |
NADW North Atlantic Deep Water North Atlantic |
genre_facet |
NADW North Atlantic Deep Water North Atlantic |
op_source |
Journal Of Geophysical Research-oceans (0148-0227) (Amer Geophysical Union), 1995-06 , Vol. 100 , N. C6 , P. 10655-10678 |
op_relation |
https://archimer.ifremer.fr/doc/00481/59318/62077.pdf doi:10.1029/94JC02864 https://archimer.ifremer.fr/doc/00481/59318/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1029/94JC02864 |
container_title |
Journal of Geophysical Research |
container_volume |
100 |
container_issue |
C6 |
container_start_page |
10655 |
_version_ |
1766071074787688448 |