At what altitude do Cirrocumulus clouds typically form?

Cirrocumulus clouds are typically found at higher altitudes, generally forming between 6,000 and 12,000 meters. These clouds consist of ice crystals and are often thin and wispy, contributing to their characteristic appearance in the sky. Their formation at higher altitudes correlates with the colder temperatures that prevail at those heights, which is essential for the development of ice crystal-based clouds.

Understanding the altitude at which specific cloud types form is crucial for meteorological studies and for those involved in aviation and outdoor activities, as it affects weather patterns and visibility. The other choices reflect lower altitudes at which different cloud types such as stratocumulus or cumulus clouds are commonly found, but they do not apply to the cirrocumulus classification. Therefore, recognizing the correct altitude range helps distinguish cirrocumulus clouds from others in meteorological observations.