Cyclonic rainfall is a type of precipitation that occurs when warm, moist air masses meet cold, dry air masses. This collision of contrasting air masses leads to the formation of cyclones or low-pressure systems, which, in turn, result in rainfall. Cyclonic rainfall is closely associated with the formation of cyclones, which are large-scale systems characterized by rotating winds that circulate counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. Several factors contribute to the formation of cyclonic rainfall, including the Coriolis effect, the convergence of moist air towards a low-pressure center, and the collision of warm, moist air masses with cold, dry air masses. Cyclonic rainfall contributes to the overall climate patterns, affecting long-term weather trends and atmospheric conditions.