@InProceedings{ViannaMene:2002:CuSeLe,
author = "Vianna, Marcio L. and Menezes, Viviane V. de",
title = "Currents and sea level off the Northeast Brazilian coast",
year = "2002",
organization = "Simp{\'o}sio Brasileiro de Oceanografia, 1.",
keywords = "OCEANOGRAFIA.",
abstract = "The region of the North Brazil Current (NBC)Retroflection in the
northern hemisphere has been studied since the 80{\"{\i}}s by
Johns and collaborators (Johns et al., 1998), who disclosed the
importance of the annual cycle, the 25-40 day and 60-90 day
oscillations in relation to NBC ring shedding. Upstream, with no
rings in the NBC, near Fortaleza, no long-term data was ever
published to date. This work describes our effort to study sea
level and currents over the NE Brazil shelf in the last 8 years.
We deployed and maintained 3 Tide Gauges (TG)at Fortaleza and
TERMISA over the northern shelf (3S-4S)and at Tamandar{\'e} (8S),
and two ADCP bottom moorings, and obtained some time series data
kindly given to us by INPH and Petrobr{\'a}s. There are presently
three current meter time series records available: two ADCP
moorings (July 2000-March 2001, 20m and 30m depths, 037W)at the
mid and outer shelf, and one standard current meter mooring off
Paracur{\'u} (August 1995-March 1996, 40m isobath, 039W, surface
data). Hourly wind station data sets from two stations were also
made available to us, one at the coast and one at the offshore
site off Paracur{\'u}. The ADCP data were studied by EOF
analysis, which confirmed the well-known barotropic nature of the
observed currents on the continental shelf. The principal
component time series were analyzed by Multichannel Singular
Spectrum Analysis (MSSA). After removal of tidal signals, the
low-frequency signal vector spectra show a dominant spectral peak
at 57 day period at both ADCP sites, with currents strongly
polarized in the longshore direction. The Paracuru currents, and
the contemporaneous TG data, present the same spectral bands as
the Johns current meter data. These oscillations are shown to be
wind-forced by a complex EOF-MSSA analysis. We also used ERS wind
scatterometer data to extend this analysis to the NBC
Retroflection area, and obtained similar correlation. The annual
and interannual variability study was done by use of the TG data,
which was shown to be consistent with our altimeter data described
in another work in this Symposium. The study shows that while the
annual cycle may be absent south of 4S, which is dominated by a
biennial cycle, but it is present north of 4S, with a interannual
modulation. This is interpreted as a consequence of the fact that
the NBC-NBUC south of 4S has a negligible annual cycle, while the
C-SEC has a strong one. It is also shown that large phase
differences (time scale of a week)between the annual cycle on
sites at relative distances of 200 km may be a consequence of
interference patterns of incident and scattered
equatorially-trapped Rossby waves by the NE coast.",
conference-location = "S{\~a}o Paulo",
conference-year = "26-30 ago. 2002",
label = "11377",
language = "Pt",
urlaccessdate = "03 maio 2024"
}