Stratus
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Cirrus clouds do not typically produce precipitation. They are high-altitude clouds composed of ice crystals and are often thin and wispy in appearance.
The nimbostratus cloud is known to produce drizzle as it is a thick, dark cloud that brings steady and light precipitation. Drizzle is characterized by small water droplets that fall slowly and persistently from a cloud layer.
The type of cloud in a thunderstorm is called a cumulonimbus cloud. These clouds are dense and vertically developed, extending high into the atmosphere where they can produce intense thunderstorms, heavy rainfall, lightning, and sometimes even tornadoes.
Cumulonimbus clouds are the type of clouds that often produce thunderstorms. These clouds are tall, dense, and can extend high into the atmosphere, creating a vertical development that results in the formation of thunder and lightning.
Cumulonimbus clouds can produce a variety of precipitation, including rain, snow, hail, or sleet. The specific type of precipitation that is produced depends on the temperature and atmospheric conditions within the cloud.
The amount of time a water droplet stays in a cloud can vary depending on the size of the droplet and the atmospheric conditions. On average, a water droplet can stay in a cloud for a few minutes to several days before eventually falling as precipitation.