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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North America Water Vapor (Moisture)
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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