Cumulonimbus. Thunderstorm clouds are typically very thick and therefore have a high albedo (not very much sunlight penetrates through to the ground, most gets reflected off of the top). Therefore, these clouds appear grey and dark on the bottom.
the storm cloud
Cumulonimbus clouds are responsible for producing thunderstorms. These towering clouds are formed by strong updrafts of warm, moist air that lead to the development of thunder, lightning, and heavy precipitation.
Cumulonimbus Cloud
A cumulonimbus cloud
A cumulonimbus cloud is typically large, dark, and responsible for producing thunderstorms. These clouds are characterized by their towering structure and can lead to heavy rainfall, lightning, thunder, and sometimes hail or strong winds.
Infrared satellite imagery can be used to identify thunderstorms due to their distinctive cold cloud tops. Thunderstorms usually have high cloud tops that are colder than surrounding clouds, making them easily identifiable on infrared satellite images by their brightness and structure.
Cumulonimbus clouds are responsible for creating thunderstorms. These towering clouds develop vertically and can reach high altitudes where they contain a lot of moisture and energy. The updrafts and downdrafts within cumulonimbus clouds cause the air to rise and fall rapidly, leading to the formation of lightning and thunder.
The type of cloud that produces thunderstorms is called a cumulonimbus cloud. These clouds are large, towering clouds that can reach high altitudes and are associated with heavy rainfall, thunder, lightning, and sometimes hail.
A cumulonimbus cloud
easy !! Cumulus Clouds
The clouds that thunderstorms from in are Nimbus clouds. Any type of Nimbus cloud can forms a thunderstorm. p.s. To divine a Nimbus cloud it is ether black or gray. But not every Nimbus cloud forms a thunderstorm only some, but keep that in mined.
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.