Articles | Volume 21, issue 5
https://doi.org/10.5194/os-21-1849-2025
https://doi.org/10.5194/os-21-1849-2025
Research article
 | 
01 Sep 2025
Research article |  | 01 Sep 2025

Mesoscale dynamics and transport in the North Brazil Current as revealed by the EUREC4A-OA experiment

Yan Barabinot, Sabrina Speich, Xavier Carton, Pierre L'Hégaret, Corentin Subirade, Rémi Laxenaire, and Johannes Karstensen

Data sets

The new CNES-CLS18 global mean dynamic topography (https://resources.marine.copernicus.eu) S. Mulet et al. https://doi.org/10.5194/os-17-789-2021

TOEddies Global Atlas R. Laxenaire et al. https://doi.org/10.17882/102877

Argos floats from Coriolis Global Data Assembly Centre (GDAC) Argo https://doi.org/10.17882/42182

DUACS DT2018: 25 years of reprocessed sea level altimetry products (https://resources.marine.copernicus.eu) G. Taburet et al. https://doi.org/10.5194/os-15-1207-2019

Concatenated Temperature, Salinity, and Velocity measurements from EUREC4A_OA/ATOMIC P. L’Hégaret et al. https://doi.org/10.17882/92071

Download
Short summary
Mesoscale eddies are rotating oceanic currents key to ocean variability. Off Brazil’s northeast coast, the North Brazil Current generates on average 4.5 eddies per year, which drift towards the West Indies, transporting waters from the Southern Hemisphere. Using data collected at sea by the EUREC4A-OA cruise, this study reveals that deep eddies transport 5 times more water than surface ones, reshaping our understanding of the regional water transport.
Share