Dm. Fratantoni et Pl. Richardson, SOFAR float observations of an intermediate-depth eastern boundary currentand mesoscale variability in the eastern tropical Atlantic Ocean, J PHYS OCEA, 29(6), 1999, pp. 1265-1278
Two neutrally buoyant SOFAR floats vigorously looped and meandered at depth
s of 950-1150 m in the eastern tropical Atlantic Ocean. The float trajector
ies illustrate a poleward how along the tropical eastern boundary and signi
ficant intermediate-depth mesoscale variability in the low-latitude eastern
basin. One float, caught within an energetic cyclonic eddy near the easter
n boundary, looped cyclonically 14 times while translating 600 km northward
parallel to the African coastline. A second float. launched near the Mid-A
tlantic Ridge, meandered eastward with a Lagrangian zonal wavelength of 400
km and meridional amplitude exceeding 200 km. Satellite infrared imagery i
ndicates that horizontal shear associated with the system of near-surface z
onal equatorial currents may contribute to the observed intermediate-depth
variability.