CONVECTIONAL RAINFALL
Convectional rainfall is a type of precipitation that occurs when warm, moist air rises and cools, leading to the formation of clouds and eventually rain. This type of precipitation is common in tropical and subtropical regions and is often associated with thunderstorms. Some characteristics of convectional rainfall include:
- It is often accompanied by strong winds, lightning, and thunder.
- It tends to be heavy and of relatively short duration, as it is caused by the rapid rising and cooling of air.
- It is most common during the afternoon and early evening, when the sun has had time to heat the ground and warm the air near the surface.
- It can lead to flash flooding in areas with poor drainage.
- It is a key factor in the water cycle and is important for maintaining the Earth's temperature balance.
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