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The amount of precipitation in a given location can vary greatly from year to year and from season to season. Also, the amount of precipitation that falls at one time can vary greatly depending on how close the cloud is to the ground. This means that it is possible for a very small area to receive much more rainfall than a larger area over the same period of time due to local variations in precipitation rates.
A cloud is a large collection of tiny water droplets or ice crystals floating in the atmosphere above Earth's surface. Clouds are formed by rising air and usually contain water vapor as well as minute solid water droplets or ice crystals called cloud condensation nuclei (CCN).
Clouds generally occur in three main types depending on their height and temperature. High-level clouds are those of about 6 miles (10 kilometers) altitude or higher and comprise cirrus, cirrocumulus and cirrostratus types that often produce no precipitation but may reflect sunlight in many directions producing hues from nearly white to pale gray or blue at a distance. Mid-level clouds form at heights between 4 and 6 miles (6 to 10 kilometers) and include altocumulus castellanus and altocumulus lenticularis types that produce little precipitation but may block out light from below when they.