from 6500 to 60000 feet
cumulonimbus cloud
A cumulonimbus cloud is not considered a low, middle, or high cloud because it can span multiple vertical layers of the atmosphere. It is a vertically developed cloud that can extend from low to high altitudes, reaching heights of over 50,000 feet. Cumulonimbus clouds are known for their towering structure and are associated with thunderstorms, heavy precipitation, and severe weather.
The Cumulonimbus cloud develops in the lower part of the troposphere, near the Earth's surface, and can reach high into the troposphere. This cloud can be a sign of dangerous storms to come.
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.
What causes a cumulonimbus cloud is the cold and warm fronts that colided.
There is no such thing as a cumulonimbus tornado. A cumulonimbus cloud is a ver large towering cloud. Most thunderstorms are cumulonimbus clouds, and some of the strongest of these storms are what produce tornadoes.
The entire thunderstorm is a cumulonimbus cloud.
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
A cumulonimbus cloud produces rain.
A cumulonimbus cloud produces rain.
A cumulonimbus cloud is a towering cloud that is often associated with thunderstorms. It is characterized by its large vertical development, extending high into the atmosphere, and can produce heavy rain, lightning, thunder, and sometimes even tornadoes. Cumulonimbus clouds have a characteristic anvil shape at the top due to strong upper-level winds.