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.