Final answer:
Convectional precipitation occurs in tropical regions where warm air rises and cools, leading to the formation of clouds and heavy rainfall. An example of convectional precipitation is the daily afternoon thunderstorms in tropical rainforests.
Step-by-step explanation:
Convectional precipitation occurs in areas where warm air rises and cools, leading to condensation and the formation of clouds. This type of precipitation is common in tropical regions, where the intense heating of the sun causes the air to rise rapidly. As the air rises, it cools and condenses, resulting in heavy rainfall. An example of convectional precipitation is the daily afternoon thunderstorms often experienced in tropical rainforest areas.