The Brazil Current is a warm water current that flows south along the Brazilian south coast to the mouth of the Río de la Plata.
Brazil Current in a map of the Atlantic Ocean
Descriptionedit
This current is caused by diversion of a portion of the AtlanticSouth Equatorial Current from where that current meets the South American continent. The Brazil Current begins at about 10–15˚S where the South Equatorial Current (SEC) splits near Cabo de São Roque, Brazil.[1] The current reaches a depth of 700 m and the estimated transport at 12˚S is 2.5 Sv.[2]
The transport increases as the current goes further south with 4 Sv at 15˚S.[1] On the offshore side of the current an anticyclonic recirculation gyre at about 30˚S causes an increase of the Brazil Current’s transport. The estimated southward transport at 27˚S, 31˚S, 34˚S, and 36˚S are 11 Sv, 17 Sv, 22 Sv, and 41 Sv. The total transport can be from 70 to 80 Sv by 36˚S with half of it being in the recirculation gyre.[3] The Brazil Current is a part of the South Atlantic subtropical gyre. The southern side of the gyre consists of the eastward-flowing South Atlantic Current (SAC). The eastern boundary is the Benguela Current System (BCS). The north side consists of the SEC, which flows west and then splits with the north water becoming the North Brazil Current (NBC). The southern-flowing waters become the Brazil Current, which makes up the western boundary.[2] It is a western boundary current like the Gulf Stream, and is its southern counterpart; however, it is considerably shallower and weaker. It flows south from the equator to the west wind drift. It joins the Falkland Current (Malvinas Current) at the Argentine Sea (see Brazil–Falkland Confluence), making it a temperate sea.[4] The Brazil-Falkland Confluence is where the Brazil Current begins to separate from the coast at about 36˚S and is where the saltier subtropical water of the Brazil Current meets the fresher subantarctic water of the Falkland Current.[2][5] The main transport of the current leaves the continental shelf at about 38˚S and the sea surface temperature at that latitude is estimated to be about 16–18˚C,[2][6] although the latitude where the current separates from the coast has been thought to be farther north from July to September than from January to March.[7] If the Falkland Current has low transport then the path of the Brazil Current is dominated by wind stress curl. However, if the Falkland Current transport is increased then the Brazil Current separates from the coast at the observed 38˚S latitude.[8] The range of sea surface temperature and the salinity for the Brazil-Falkland Confluence is 7–18˚C and 33.6–36 psu.[5] The Brazil Current region also contains six major water masses within the system: Upper Circumpolar Water (UCPW), Lower Circumpolar Water (LCPW), Central Water (CW), Antarctic Intermediate Water (AAIW), Antarctic Bottom Water (AABW), and North Atlantic Deep Water (NADW).[3]
Referencesedit
^ abStramma, Lothar; Ikeda, Yoshimine; Peterson, Ray G. (1990). "Geostrophic transport in the Brazil Current region north of 20˚S" (PDF). Deep-Sea Research. 37 (12): 1875–1886. Bibcode:1990DSRA...37.1875S. doi:10.1016/0198-0149(90)90083-8.
^ abcdTalley, Lynne D.; Pickard, George L.; Emery, William J.; Swift, James H. (2011). Descriptive Physical Oceanography: An Introduction (6th ed.). Burlington, MA: Academic Press. p. 555.
^ abZemba, J.C., 1991. "The structure and transport of the Brazil Current between 27˚ and 36˚ South". Ph.D. thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 160 pp.
^Ecorregión Mar Argentino 2013-11-05 at the Wayback Machine(in Spanish)
^ abGordon, Arnold L. (1989). "Brazil-Malvinas Confluence-1984". Deep Sea Research Part A. Oceanographic Research Papers. 36 (3): 359363–361384. Bibcode:1989DSRA...36..359G. doi:10.1016/0198-0149(89)90042-3.
^Chelton, Dudley B.; Wentz, Frank J. (2005). "Global Microwave Satellite Observations of Sea Surface Temperature for Numerical Weather Prediction and Climate Research". Bulletin of the American Meteorological Society. 86 (8): 1097–1115. Bibcode:2005BAMS...86.1097C. doi:10.1175/bams-86-8-1097.
^Olson, Donald B.; Podesta, Guillermo P.; Evans, Robert H.; Brown, Otis B. (1988). "Temporal variations in the separation of Brazil and Malvinas currents". Deep-Sea Research. 35 (12): 1971–1990. Bibcode:1988DSRA...35.1971O. doi:10.1016/0198-0149(88)90120-3.
^Matano, Ricardo P. (1993). "On the separation of the Brazil Current from the coast". Journal of Physical Oceanography. 23 (1): 79–90. Bibcode:1993JPO....23...79M. doi:10.1175/1520-0485(1993)023<0079:otsotb>2.0.co;2.
External linksedit
The Brazil Current
January 19, 2024
brazil, current, warm, water, current, that, flows, south, along, brazilian, south, coast, mouth, río, plata, atlantic, oceandescription, editthis, current, caused, diversion, portion, atlantic, south, equatorial, current, from, where, that, current, meets, so. The Brazil Current is a warm water current that flows south along the Brazilian south coast to the mouth of the Rio de la Plata Brazil Current in a map of the Atlantic OceanDescription editThis current is caused by diversion of a portion of the Atlantic South Equatorial Current from where that current meets the South American continent The Brazil Current begins at about 10 15 S where the South Equatorial Current SEC splits near Cabo de Sao Roque Brazil 1 The current reaches a depth of 700 m and the estimated transport at 12 S is 2 5 Sv 2 The transport increases as the current goes further south with 4 Sv at 15 S 1 On the offshore side of the current an anticyclonic recirculation gyre at about 30 S causes an increase of the Brazil Current s transport The estimated southward transport at 27 S 31 S 34 S and 36 S are 11 Sv 17 Sv 22 Sv and 41 Sv The total transport can be from 70 to 80 Sv by 36 S with half of it being in the recirculation gyre 3 The Brazil Current is a part of the South Atlantic subtropical gyre The southern side of the gyre consists of the eastward flowing South Atlantic Current SAC The eastern boundary is the Benguela Current System BCS The north side consists of the SEC which flows west and then splits with the north water becoming the North Brazil Current NBC The southern flowing waters become the Brazil Current which makes up the western boundary 2 It is a western boundary current like the Gulf Stream and is its southern counterpart however it is considerably shallower and weaker It flows south from the equator to the west wind drift It joins the Falkland Current Malvinas Current at the Argentine Sea see Brazil Falkland Confluence making it a temperate sea 4 The Brazil Falkland Confluence is where the Brazil Current begins to separate from the coast at about 36 S and is where the saltier subtropical water of the Brazil Current meets the fresher subantarctic water of the Falkland Current 2 5 The main transport of the current leaves the continental shelf at about 38 S and the sea surface temperature at that latitude is estimated to be about 16 18 C 2 6 although the latitude where the current separates from the coast has been thought to be farther north from July to September than from January to March 7 If the Falkland Current has low transport then the path of the Brazil Current is dominated by wind stress curl However if the Falkland Current transport is increased then the Brazil Current separates from the coast at the observed 38 S latitude 8 The range of sea surface temperature and the salinity for the Brazil Falkland Confluence is 7 18 C and 33 6 36 psu 5 The Brazil Current region also contains six major water masses within the system Upper Circumpolar Water UCPW Lower Circumpolar Water LCPW Central Water CW Antarctic Intermediate Water AAIW Antarctic Bottom Water AABW and North Atlantic Deep Water NADW 3 References edit a b Stramma Lothar Ikeda Yoshimine Peterson Ray G 1990 Geostrophic transport in the Brazil Current region north of 20 S PDF Deep Sea Research 37 12 1875 1886 Bibcode 1990DSRA 37 1875S doi 10 1016 0198 0149 90 90083 8 a b c d Talley Lynne D Pickard George L Emery William J Swift James H 2011 Descriptive Physical Oceanography An Introduction 6th ed Burlington MA Academic Press p 555 a b Zemba J C 1991 The structure and transport of the Brazil Current between 27 and 36 South Ph D thesis Massachusetts Institute of Technology and Woods Hole Oceanographic Institution 160 pp Ecorregion Mar Argentino Archived 2013 11 05 at the Wayback Machine in Spanish a b Gordon Arnold L 1989 Brazil Malvinas Confluence 1984 Deep Sea Research Part A Oceanographic Research Papers 36 3 359363 361384 Bibcode 1989DSRA 36 359G doi 10 1016 0198 0149 89 90042 3 Chelton Dudley B Wentz Frank J 2005 Global Microwave Satellite Observations of Sea Surface Temperature for Numerical Weather Prediction and Climate Research Bulletin of the American Meteorological Society 86 8 1097 1115 Bibcode 2005BAMS 86 1097C doi 10 1175 bams 86 8 1097 Olson Donald B Podesta Guillermo P Evans Robert H Brown Otis B 1988 Temporal variations in the separation of Brazil and Malvinas currents Deep Sea Research 35 12 1971 1990 Bibcode 1988DSRA 35 1971O doi 10 1016 0198 0149 88 90120 3 Matano Ricardo P 1993 On the separation of the Brazil Current from the coast Journal of Physical Oceanography 23 1 79 90 Bibcode 1993JPO 23 79M doi 10 1175 1520 0485 1993 023 lt 0079 otsotb gt 2 0 co 2 External links editThe Brazil Current Retrieved from https en wikipedia org w index php title Brazil Current amp oldid 1170474050, wikipedia, wiki, book, books, library,
