This document discusses three main types of rainfall: relief, convective, and frontal. Relief rainfall occurs when air is blown over the sea and then forced up over high land, causing the air to cool and condense into rain. Convective rainfall primarily happens in tropical areas where hot air rises, cools, and forms rain, sometimes causing thunderstorms. Frontal rainfall occurs at the boundary of warm and cold air masses, where warm air is forced to rise over cold air, cooling and condensing into rainclouds and precipitation. Diagrams and descriptions of each rainfall type are provided.