ANNUAL CYCLE AND VARIABILITY OF THE NORTH BRAZIL CURRENT

Citation
We. Johns et al., ANNUAL CYCLE AND VARIABILITY OF THE NORTH BRAZIL CURRENT, Journal of physical oceanography, 28(1), 1998, pp. 103-128
Citations number
66
Categorie Soggetti
Oceanografhy
ISSN journal
00223670
Volume
28
Issue
1
Year of publication
1998
Pages
103 - 128
Database
ISI
SICI code
0022-3670(1998)28:1<103:ACAVOT>2.0.ZU;2-E
Abstract
Current meter observations from an array of three subsurface moorings located on the Brazil continental slope near 4 degrees N are used to d escribe the annual cycle and low-frequency variability of the North Br azil Current (NBC). The moored array was deployed from September 1989 to January 1991, with further extension of the shallowest mooring, loc ated over the 500-m isobath near the axis of the NBC, through Septembe r 1991. Moored current measurements were also obtained over the adjace nt shelf for a limited time between February and May 1990. The NBC has a large annual cycle at this latitude, ranging from a maximum transpo rt of 36 Sv (Sv = 10(6) m(3) s(-1)) in July-August to a minimum of 13 Sv in April-May, with an annual mean transport of approximately 26 Sv. The mean transport is dominated by how in the upper 150 m, and the se asonal cycle is contained almost entirely in the top 300 m. Transport over the continental shelf is 3-5 Sv and appears to be fairly constant throughout the year, based on the available current meter records and shipboard ADCP surveys. The NBC transport cycle is in good agreement with linear wind-driven models and appears to be in near-equilibrium w ith remote wind stress curl forcing across the tropical Atlantic for m uch of the year. However, the mean transport of the NBC is 15 Sv large r than can be explained by wind forcing alone, indicating a strong the rmohaline component. Mesoscale variability in the region is dominated by fluctuations with periods near 25-40 days and 60-90 days. The 25-40 -day fluctuations are strongly surface trapped and are most energetic in early summer during the acceleration phase of the NBC. The lower-fr equency fluctuations have a deeper reaching baroclinic structure, are present year-round, and are associated with the propagation of large a nticyclonic eddies northwestward along the coast. It is hypothesized t hat these features may serve as a catalyst for the eddy shedding proce ss seen in the NBC retroflection in earlier observations.