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This study analyzes the bifurcation of the Western Boundary Current (WBC) system in the South Atlantic Ocean using two high-resolution ocean models, HYCOM and OCCAM. It identifies key bifurcation latitudes for different water masses, revealing that the South Equatorial Current bifurcates at 13°-15° S and the Antarctic Intermediate Water at 28°-30° S, contributing to the complex flow dynamics in the region. The findings enhance understanding of the WBC
- Author
- Janini Pereira
- Language
- EN