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