The cumulonimbus clouds is found at high altitudes and form when the wind is strong.
- The mature form of cumulus clouds is a cumulonimbus cloud. They develop when cumulus congestus clouds experience a strong updraft that lifts the tops of the clouds upward until they reach the tropopause at an altitude of 18,000 meters (59,000 feet).
- The dew point and ground temperature are the two main factors that determine the altitude of clouds.
- The dew point is a measurement of the air's relative humidity, but rather than being expressed as a percentage of saturation, it is expressed as the temperature at which the air must be cooled to reach a humidity level of 100 percent.
- At the dew point, the air will become saturated with water vapor. When water reaches 100%, it can start to form dew, rain, clouds, or other types of precipitation. Although the specifics of each atmospheric condition differ, there is a general formula to determine the altitude of clouds.
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