Storm events are the primary mechanisms for generating overwash along the shoreline. This process occurs when wave runup exceeds the elevation of sandy features, often forming washover deposits. In retrograding barriers, overwash is the main driver of landward migration. Extreme wave energy events can lead to rapid changes in the morphology of these environments. On urbanized coastlines, storm impacts can be catastrophic and result in high reconstruction costs. Understanding the characteristics of storm events and the local morphological characteristics of these sandy features is crucial for risk assessments, hazard mitigation, and coastal area adaptations in the scenario of increasing storm events. The main objective of this study is to analyze the role of overwash processes in the retrogradation of the Quissamã barrier, located in the southern sector of the Paraíba do Sul River Delta Complex (PSRDC), on the coast of Rio de Janeiro. Using data from the global Wave Watch III model, sea warnings issued by the Brazilian Navy, atmospheric pressure charts, and astronomical tides, we identified storm events and mapped the washover fans formed after specific storm events. The washover fans were identified using PlanetScope images. The identified storm events were characterized by waves from the SE-S directions with high peak periods, and mostly occurred during spring tides or transitioning to neap tides. Additionally, the atmospheric pattern for most events was associated with the migration of cold fronts from high to low latitudes, leading to the development of extratropical cyclones. The geometry of the barrier also proved to be an essential morphological pattern. Considering the relative sea level along part of the Brazilian coast has been decreasing over the last 5500 years, storm events and associated processes are crucial for the retrogradation of barriers, maintaining the retrogradational characteristics of this coastal barrier.