<p>Swells are critical concerns regarding safety, marine transportation, and coastal engineering construction of coastal countries along the Gulf of Guinea and have been scientific problems due to the lack of systematic theoretical, numerical, and observational research. In this study, a double nesting numerical model was constructed and validated from the Atlantic Ocean to the Gulf of Guinea based on simulating waves nearshore (SWAN) to explore the swell characteristics and source tracing in the Gulf of Guinea in winter and summer seasons from 2020 to 2021. Simulation results reveal that swells are stronger and deflect more to the west in winter than summer, even though they dominate in both seasons in the Gulf of Guinea in the S-SW directional range. Simulated two-dimensional (2D) wave spectral patterns not only clarify wave composition, variation, and propagation properties from the central South Atlantic Ocean to the Gulf of Guinea, but also distinguish swell strength and directional range in winter and summer. The NW wind events induce swells which spread toward the SSE-ESE direction from the North Atlantic Ocean, big wind source generates sustained and stable S-SW swells from the South Atlantic Ocean, and corresponding swell-influenced areas are discussed. The strongest swell event in the Gulf of Guinea during the simulation was used as a case study to trace its source. A strong clockwise wind vortex within the Roaring Forties induced these large swells in the Gulf of Guinea approximately 5.5 days later, and swell propagation formed a regular isoline of peak period distribution from the South Atlantic Ocean to the Gulf of Guinea in the SSW-SW direction.</p>