Weather Alerts for Utah
1. Avalanche Watch for: Wasatch Mountains I-80 North; Wasatch Mountains South of I-80; Western Uinta Mountains; Wasatch Plateau/Book Cliffs; Central Mountains; Southern Mountains
2. Wind Advisory for: Great Salt Lake Desert and Mountains; Tooele and Rush Valleys; Salt Lake Valley; Western Millard and Juab Counties
3. Winter Storm Warning for: Cache Valley/Utah Portion
4. Winter Storm Warning for: Southern Mountains
5. Winter Storm Warning for: Southwest Utah; Bryce Canyon Country
6. Winter Storm Warning for: Wasatch Back
7. Winter Storm Warning for: Wasatch Mountains I-80 North; Wasatch Mountains South of I-80; Western Uinta Mountains
8. Winter Storm Warning for: Wasatch Plateau/Book Cliffs; Central Mountains
9. Winter Weather Advisory for: Eastern Uinta Mountains
10. Winter Weather Advisory for: La Sal and Abajo Mountains
11. Winter Weather Advisory for: Tavaputs Plateau
12. Winter Weather Advisory for: Tooele and Rush Valleys; Eastern Box Elder County; Northern Wasatch Front; Salt Lake Valley; Utah Valley; Eastern Juab/Millard Counties
13. Winter Weather Advisory for: Zion National Park; Upper Sevier River Valleys; South Central Utah
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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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