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Clouds - Coggle Diagram
Clouds
Forming clouds
As the air cools, the amount of water vapor needed for saturation decreases and the relative humidity increases.
When relative humidity reaches 100%, the air is saturated.
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Types of clouds
By shape
Cumulus clouds
Puffy, white clouds that tend to have flat bottoms are called cumulus clouds.
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When these clouds get taller, they produce thunderstorms.
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Stratus clouds
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Usually they stretch across the sky in long, horizontal layers. These clouds are caused by a gentle lifting of a large body of air into the atmosphere.
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Cirrus clouds
Cirrus clouds are thin, feathery, white clouds found at high altutudes.
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Sometimes, they are moved by strong winds at speeds of 100 to 200 miles an hour.
Cirrus clouds are made up entirely of ice crystals and are so thin that at night you can sometimes see the stars shining through them.
If they get thicker, cirrus clouds indicate that a change in weather is coming.
By height
Prefix cirro-
is used to describe clouds that form at high altitudes (above 21,000 feet).
Because of the cold temperatures at high altitude, high clouds are made up of ice crystals. A cumulus cloud that form high in the atmosphere is called a cirrocumulus cloud.
Prefix alto-
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Middle clouds (7,500 to 21,000 feet) can be made up of both water droplets and ice crystals).
Prefix strato-
is used to describe clouds that form at low altitude (below 7,500 feet). Low clouds are made up water droplets.
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Warm vs cold clouds
Clouds are classified as warm if their temperatures throughout is above 32oF and cold if they extend to heights where temperatures are less than 32oF.
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Some cold clouds contain only supercooled water. These clouds are hazardous to aviation because the water, freezing on impact with an airplane, can cause ice to build up on the fuselage and wings.