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Cloud Types 18.3 Brain Pop: Clouds.

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Presentation on theme: "Cloud Types 18.3 Brain Pop: Clouds."— Presentation transcript:

1 Cloud Types 18.3 Brain Pop: Clouds

2 18.3 Types of Clouds Clouds are classified based on how they formed and their height 3 basic forms…

3 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

4 Cumulus: (= a pile) Rounded, thick, puffy masses
Formed by vertically rising air currents Usually mean fair weather

5 Layered, gray, and smooth
Stratus: (= a layer) Layered, gray, and smooth Form in sheets at low altitudes Block out sunlight - associated with rain

6 3 levels of height  can have seasonal and latitudinal variation

7 Cirrostratus halo around the sun
Cirrus cirrocumulus High Clouds: (above 6000 meters) Cirrostratus halo around the sun cirrostratus

8 altocumulus Middle Clouds: ( meters) altostratus

9 Low Clouds: (below 2000 meters)
Stratus stratocumulus Low Clouds: (below 2000 meters) nimbostratus

10 Clouds of vertical development: (start at 2000 meters – mid/high)
cumulonimbus Clouds of vertical development: (start at 2000 meters – mid/high)

11 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.

12 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

13 OR fog forms over land as air temperature near the ground drops overnight and reaches the dew point in the early morning

14 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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