The type of rainfall characterized by torrential downpour in the tropics or during summers in the temperature interiors is called

The type of rainfall characterized by torrential downpour in the tropics or during summers in the temperature interiors is called "convectional rainfall." This type of rainfall occurs due to the heating of the Earth's surface, which causes the air to rise, cool, and condense into clouds. As the clouds continue to rise, they become saturated and precipitation occurs in the form of heavy rain, often accompanied by thunder and lightning. Convectional rainfall is common in areas with high temperatures and humidity, such as tropical regions, and is usually of short duration but high intensity.