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Cross- and long-shelf Ekman transport components were correlated with the variability of zooplankton biomass from 1977 to 1990 off the southern Brazilian coast (27°S to 35°S and 46°W to 54°W). During warm months the dominant cross-shelf Ekman transport was oriented offshore, where an increase in zooplankton biomass occurred with intervals of 2–3 months. The presence of the South Atlantic Central Water (SACW; the water mass that typically upwells at the continental shelf) was confirmed by seasonal temperature–salinity diagrams. The high zooplankton biomass values observed in this study were frequently caused by salps, which play an important ecological role in the pelagic community in upwelling zones that has not been investigated yet.

The Influence of Ekman Transport on Zooplankton Biomass Variability off Southern Brazil