Since the beginning of the satellite era, the only documented tropical cyclone over the western South Atlantic Ocean (SAO) has been Catarina, which occurred in March 2004. However, this system resulted from a tropical transition (TT), when a dipole blocking-pattern at the middle-upper levels of the atmosphere contributed to decreasing the vertical wind shear over an extratropical cyclone (McTaggart-Cowan et al., 2006; Pezza & Simmonds, 2005). Fifteen years after Catarina, in March 2019, the Brazilian Navy registered Iba, the first pure tropical cyclogenesis over tropical western SAO (∼16.5°S). Iba is an indigenous name previously established by the Brazilian Navy (NORMAN, 2018). As this system has not yet been described in the literature, it is the purpose of this study. The low frequency of tropical systems over the SAO has been explained by the unfavorable climate conditions for tropical cyclogenesis such as environmental vertical wind shear stronger than 10 m s −1 in the 850-200 hPa layer and sea surface temperature (SST) colder than 26°C (Gray, 1968; Pezza & Simmonds, 2005). On the other hand, the combination of the main environmental predictors for tropical cyclogenesis (absolute vorticity at 850 hPa, relative humidity at 700 hPa, potential intensity in terms of maximum wind speed, and the vertical wind shear at 850-200 hPa layer) in the Genesis Potential Index (GPI; K. A. Emanuel & Nolan, 2004) show some favorable conditions for tropical cyclogenesis near southeastern Brazil (Walsh et al., 2013). McTaggart-Cowan et al. (2013, 2015) also suggest that the SAO climate conditions are most likely to favor weak and strong TT than pure tropical cyclogenesis. The definition of weak and strong TT was introduced by Davis and Bosart (2003, 2004). The weak TT occurs in an environment with a weak upper-level disturbance and moderate lower-level thermal gradients, while the strong TT takes place in the presence of strong upper-level disturbance and strong lower-level thermal gradients (McTaggart-Cowan et al., 2013). Hodges et al. (2017), comparing six reanalysis datasets and IBTrACS (observed data) from 1979 to 2012, showed one tropical cyclone per year over the SAO in the observations and ∼7 cyclones per year in each