230
SOUTH EQUATORIAL.
10° COUNTERCURRENT
I
PERU SUB·
SURFACE
COUNTER·
CURRENT
I
I
J. Tarazona and W. Arntz
®
Fig. 16.l.A Generalized circulation scheme for the eastern South Pacific Ocean with
sites of strong coastal upwelling. B Two-layer coastal upwelling system for the eastern
South Pacific Ocean with the superficial layer constituted by the Peru (Humboldt)
Coastal Current and the subsuperficiallayer constituted by the Peru Subsurface Countercurrent. (After Arntz and Fahrbach 1991)
SOUTH EQUATORIAL.
10° COUNTERCURRENT
I
PERU SUB·
SURFACE
COUNTER·
CURRENT
I
I
J. Tarazona and W. Arntz
®
Fig. 16.l.A Generalized circulation scheme for the eastern South Pacific Ocean with
sites of strong coastal upwelling. B Two-layer coastal upwelling system for the eastern
South Pacific Ocean with the superficial layer constituted by the Peru (Humboldt)
Coastal Current and the subsuperficiallayer constituted by the Peru Subsurface Countercurrent. (After Arntz and Fahrbach 1991)