Abstract
This project aims to characterize and understand the causes for the variability in the transport of the Deep Western Boundary Current in the South Atlantic. We will use data obtained by currentmeters installed on Pressure Inverted Echo Sounders (PIES) and therefore called CPIES. The PIES array at 34.5°S between 44.5°W and 51.5°W was established by the South Atlantic Meridional Overturning…