Weather Alerts for Montana
1. High Wind Warning for: Madison River Valley; Beaverhead and Western Madison below 6000ft
2. Winter Storm Warning for: Absaroka/Beartooth Mountains
3. Winter Storm Warning for: Crazy Mountains
4. Winter Storm Watch for: Gallatin and Madison County Mountains and Centennial Mountains
5. Winter Storm Watch for: Gallatin Valley
6. Winter Weather Advisory for: Bitterroot/Sapphire Mountains
7. Winter Weather Advisory for: Butte/Blackfoot Region
8. Winter Weather Advisory for: East Glacier Park Region
9. Winter Weather Advisory for: Lower Clark Fork Region
10. Winter Weather Advisory for: Northwest Beaverhead County
11. Winter Weather Advisory for: Potomac/Seeley Lake Region
12. Winter Weather Advisory for: Southern Rocky Mountain Front; Little Belt and Highwood Mountains; Big Belt, Bridger and Castle Mountains
13. Winter Weather Advisory for: West Glacier Region
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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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