Weather Alerts for Wyoming
1. Freeze Warning for: Cody Foothills; Southwest Bighorn Basin
2. Freeze Warning for: North Bighorn Basin; Southeast Bighorn Basin
3. Freeze Warning for: Wind River Basin; Lander Foothills
4. High Wind Warning for: Ferris/Seminoe/Shirley Mountains; Central Carbon County; North Snowy Range Foothills; Upper North Platte River Basin
5. Winter Storm Warning for: Wind River Mountains West; Wind River Mountains East
6. Winter Storm Warning for: Yellowstone National Park; Absaroka Mountains; Teton and Gros Ventre Mountains
7. Winter Weather Advisory for: Bighorn Mountains West; Bighorn Mountains Southeast
8. Winter Weather Advisory for: Converse County Lower Elevations
9. Winter Weather Advisory for: Ferris/Seminoe/Shirley Mountains; Shirley Basin; Central Carbon County; North Snowy Range Foothills; Southwest Carbon County; Upper North Platte River Basin
10. Winter Weather Advisory for: Green Mountains and Rattlesnake Range; Casper Mountain
11. Winter Weather Advisory for: Natrona County Lower Elevations
12. Winter Weather Advisory for: North Laramie Range
13. Winter Weather Advisory for: Northeast Johnson County; Southeast Johnson County
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North America Water Vapor (Moisture)
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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