Biblioteca

The Equatorial Undercurrent (EUC) encounters the Galápagos Archipelago on the equator as it flows eastward across the Pacific. The impact of the Galápagos Archipelago on the EUC in the eastern equatorial Pacific remains largely unknown. In this study, the path of the EUC as it reaches the Galápagos Archipelago is measured directly using high-resolution observations obtained by autonomous underwater gliders.Gliders were deployed along three lines that define a closed region with the Galápagos Archipelago as the eastern boundary and 938W from 28S to 28N as the western boundary. Twelve transects were simultaneously occupied along the three lines during 52 days in April–May 2016. Analysis of individual glider transects and average sections along each line show that the EUC splits around the Galápagos Archipelago. Velocity normal to the transects is used to estimate net horizontal volume transport into the volume. Downward integration of the net horizontal transport profile provides an estimate of the time- and areal-averaged vertical velocity profile over the 52-day time period. Localmaxima in vertical velocity occur at depths of 25 and 280m with magnitudes of (1.7 6 0.6) 3 1025ms21 and (8.0 6 1.6) 3 1025ms21, respectively. Volume transport as a function of salinity indicates that...