Those admitted to the SACW
were expected to pay about US$2.
The temperature decreased more sharply when a thermocline was present due to the influence of the SACW
(during spring and summer) when upwelling events were more pronounced, mainly by the prevalence of northeasterly winds (Barth et al.
It was evident the influence of SACW
during spring-summer months in both years, and in autumn (March-April) of the second year (Figure 2).
2014) favor strong vertical homogeneity, the distance of ~86 km of the SACW
from shore, the predominance of the CW and Tropical Water on the SBB, and, eventually, the northward displacement of the low-salinity and nutrient-rich Rio de La Plata plume up to the southern part of the SBB (Ciotti et al.
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Except for coastal upwelling at the extreme limits of the SBB, SACW
has previously been considered to influence mainly the middle and outer continental shelf, detected at distances greater than 30 km from shore (Castro & Miranda 1998).
The similarity of values of female CL and maturity between the regions of Macae and Farol de Sao Tome (northern limit of distribution) strengthens the hypothesis of the influence and importance of the SACW
in the reproductive dynamics of A.
The horizontal distribution of the water temperature at a depth of 50 m showed a flow pattern similar to that of the Brazil Current on the three cruises, and the thermal front of the SACW
of the Cape Sao Tome reached the southern rim of the Abrolhos Bank (Fig.
The presence of these peaks is probably related to SASW or SACW
water masses, because these nitrate peaks can be related to the upwelling events.
When intruding onto the continental shelf, SACW
occupies the bottom layer and mixes with the warmer and fresher Coastal Water (CW).
The combination of these effects results in a strong mechanism capable of carrying cold and nitrate-rich SACW
waters to the coast (Acha et al.
is the water mass responsible for carrying nutrients to the pelagic system mainly in summer (Gaeta & Brandini, 2006).