The different types of clouds can be broken down into three categories: low level, mid level and high level. The lowest level types of clouds in the atmosphere are stratus, cumulus and stratocumulus. Mid level clouds are altocumulus and altostratus. The highest clouds in the atmosphere (ones that are all the way at the at the top of the atmosphere) are cirrus, cirrostratus and cirrocumulus. Cumulonimbus clouds (thunderstorm clouds) can also grow to high heights in the atmosphere.
Clouds that form in the lowest level of the atmosphere are the stratus, cumulus and stratocumulus clouds. The stratus clouds are often gray in color and can sometimes take up the entire sky. Often times on a chilly winter or fall day stratus clouds will develop and sometimes produce drizzle or very light flurries/snow.
Cumulus clouds are my favorite! Those are the types of clouds that look like puffy cotton balls in the sky. Cumulus clouds that form on a quiet afternoon are referred to as 'fair-weather' cumulus clouds. One common thing you'll notice with cumulus clouds is that their bases are all flat and form at the same height. When enough instability is present in the atmosphere, the cumulus cloud can build into what we call a cumulonimbus cloud and produce thunderstorms.
Stratocumulus clouds are actually the type of clouds we had earlier in the week behind departing low pressure. These clouds look like cumulus clouds, but they are lower and form in rows. Often times you can see the sun in between the rows of clouds. This type of cloud doesn't usually produce any precipitation. It just forms when there is cooler air aloft in the atmosphere.
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