title: Equatorial Undercurrent and Related Currents off Brazil in March and April 1963.
abstract: In 1963, the source of the Equatorial Undercurrent appeared to be near 38 degrees W. This undercurrent was an equatorial extension of a narrow saline current setting east-southeast at the surface near 2 degrees N 42 degrees W. Near 380 degrees W, a retroverse branch of the Guiana Current also joined the Equatorial Undercurrent. Surface flow was easterly along all of the east-southeast current and the undercurrent observed. The subsurface-velocity maximum of the undercurrent was higher at 35 degrees W than at 38 degrees W.
authors.forename: J D
authors.initials: JD
authors.lastname: Cochrane