Weather Alerts for Wyoming
1. High Wind Watch for: South Laramie Range; South Laramie Range Foothills
2. Winter Storm Warning for: Sierra Madre Range
3. Winter Weather Advisory for: Bighorn Mountains West; Bighorn Mountains Southeast
4. Winter Weather Advisory for: Converse County Lower Elevations; Niobrara County; North Laramie Range
5. Winter Weather Advisory for: Green Mountains and Rattlesnake Range; Natrona County Lower Elevations; Casper Mountain
6. Winter Weather Advisory for: Jackson Hole; Star Valley
7. Winter Weather Advisory for: Northeast Johnson County; Southeast Johnson County
8. Winter Weather Advisory for: Northern Campbell; Southern Campbell; Western Crook; Weston County Plains; Newcastle
9. Winter Weather Advisory for: Snowy Range
10. Winter Weather Advisory for: Southwest Bighorn Basin; Southeast Bighorn Basin; Owl Creek and Bridger Mountains
11. Winter Weather Advisory for: Southwest Wyoming
12. Winter Weather Advisory for: Teton and Gros Ventre Mountains; Wind River Mountains West; Wind River Mountains East; Salt River and Wyoming Ranges
13. Winter Weather Advisory for: Wind River Basin; Lander Foothills
14. Winter Weather Advisory for: Yellowstone National Park
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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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