The North Brazil Current (NBC) rings are a key mechanism for interhemispheric water transport, facilitating the exchange between the South Atlantic Ocean and the North Atlantic. However, significant uncertainties persist regarding the total volume transported by these structures and the properties of the water masses they advect. In this study, we integrate high-resolution in situ observations from the EUREC4A-OA field experiment with satellite altimetry to address these knowledge gaps. Using a novel methodology, we estimate that surface NBC rings transport approximately 1.5 Sv while subsurface eddies contribute between 0.4 Sv and 9.7 Sv underscoring their critical role in the regional total transport. Combined, these transports, may significantly contribute to closing the Atlantic Meridional Overturning Circulation transport at low latitudes. Surface NBC rings predominantly advect Salinity Maximum Waters and fresh waters from the Amazon River, whereas subsurface NBC rings play a critical role in transporting Eastern South Atlantic Central Waters, Western South Atlantic Central Waters, and Antarctic Intermediate Waters northward. We also found that the heat transports by surface and subsurface NBC rings are here evaluated at 5.8 TW and 0.3 TW which is much less than previous estimation. Overall, these findings underscore the pivotal role of subsurface NBC rings as conduits for South Atlantic Waters across the equator and the Tropical North Atlantic. This study confirms the intricate dynamics of NBC rings and their essential role into interhemispheric water transport.