1996
DOI: 10.1029/96eo00177
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Experiment studies circulation in the western South Atlantic

Abstract: Observations in the Brazil Current region between 20° and 30°S are revealing many interesting oceanographic features. In the austral winter of 1993, what appears to be an anomalous northward penetration of waters from the Brazil/Malvinas confluence region into the South Brazil Bight was observed (Figure 1).

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Cited by 70 publications
(65 citation statements)
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“…Segundo Campos et al (1996), a penetração deáguas frias oriundas da região da Confluência Subtropical na plataforma continental brasileira alcança limites setentrionais médios em torno de 28 • S, próximo ao Cabo de Santa Marta. Somente em condições anômalas a CCC alcançaria menores latitudes.…”
Section: Discussionunclassified
See 1 more Smart Citation
“…Segundo Campos et al (1996), a penetração deáguas frias oriundas da região da Confluência Subtropical na plataforma continental brasileira alcança limites setentrionais médios em torno de 28 • S, próximo ao Cabo de Santa Marta. Somente em condições anômalas a CCC alcançaria menores latitudes.…”
Section: Discussionunclassified
“…Apresentam contornos delimitados por intensos gradientes de propriedades físicas em superfície e em subsuperfície, em geral ocorrem associados a correntes instáveis (Olson, 1991). Campos et al (1996) afirmam que os vórtices na Bacia de Santos, tanto ciclônicos como anticiclônicos, são formados em lados opostos ao eixo da CB e aparentemente não se desprendem da corrente.…”
unclassified
“…Satellite-derived sea surface temperatures reveal that the coldest water tongue over the shelf (17øC) extends northward to 26øS [Campos et al, 1996a]. An additional drifter deployed at the Brazil Current in late April 1993 near 30øS also drifted onshore and followed a similar path and temperature trend, suggesting that the northward recirculation was indeed a large scale feature at the time.…”
Section: Campos Et Al [1996a] Andmentioning
confidence: 99%
“…Due to the confluence of both currents between latitudes 25°S and 45°S of the western South Atlantic observed in certain periods of the year, there is the formation of water masses like the South Atlantic Central Water (SACW; T < 20ºC, S < 36.4), accounting for part of the convergence of the subtropical gyre and giving rise to the Cabo Frio upwelling, which extends between 23 o S and 29 o S (Castro-Filho et al, 1987;Campos et al, 1996Campos et al, , 2000Silveira et al, 2000;Acha et al, 2004). This upwelling is enhanced by coastal winds and by the break in the continental shelf (approximately 50 km from the coast) driven by the meandering pattern and eddy of the Brazil Current (Castro & Miranda, 1998;Campos et al, 2000).…”
Section: Introductionmentioning
confidence: 99%