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Cloud Types 18.3 Brain Pop: Clouds
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18.3 Types of Clouds Clouds are classified based on how they formed and their height 3 basic forms…
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Cirrus: (= a curl of hair) Thin, white, wispy, feathery
Made from ice crystals at high altitudes Seen in fair weather, but can mean rain or snow is coming
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Cumulus: (= a pile) Rounded, thick, puffy masses
Formed by vertically rising air currents Usually mean fair weather
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Layered, gray, and smooth
Stratus: (= a layer) Layered, gray, and smooth Form in sheets at low altitudes Block out sunlight - associated with rain
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3 levels of height can have seasonal and latitudinal variation
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Cirrostratus halo around the sun
Cirrus cirrocumulus High Clouds: (above 6000 meters) Cirrostratus halo around the sun cirrostratus
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altocumulus Middle Clouds: ( meters) altostratus
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Low Clouds: (below 2000 meters)
Stratus stratocumulus Low Clouds: (below 2000 meters) nimbostratus
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Clouds of vertical development: (start at 2000 meters – mid/high)
cumulonimbus Clouds of vertical development: (start at 2000 meters – mid/high)
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Fog: A cloud with its base at or very near the ground
The only difference between clouds and fog is their method and place of formation.
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Fogs caused by cooling Ex: coastal California
Fog forms when warm oceanic air moves over a cold water current, then wind blows it over land Ex: coastal California
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OR fog forms over land as air temperature near the ground drops overnight and reaches the dew point in the early morning
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Fogs caused by evaporation
Fog forms over water when water temperatures are still warm, but air temperatures have fallen rapidly Fall and early winter
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