 This study examined the effects of mesoscale eddies on air-sea heat and freshwater exchanges in the tropical Atlantic Ocean. The results showed that about 40% of cyclonic eddies contributed to warm SST anomalies, while 40% of anti-cyclonic eddies contributed to cold SST anomalies. These eddies also played a role in the variability of latent heat flux, sensible heat flux, and infrared fluxes as well as precipitation. Additionally, the study found that horizontal advection processes did not significantly affect the overall heat fluxes or precipitation over eddies, but vertical processes did. Finally, the study found that there was a strong correlation between heat fluxes and precipitation underneath the intertropical convergence zone, indicating that eddies may have an important influence on these processes in this area. This article was authored by Habib Michael Ayagweju, Alexis Shainio, Isabel Dodu, and others.