Weather Alerts for Montana
1. High Wind Warning for: Madison River Valley; Beaverhead and Western Madison below 6000ft
2. Lake Wind Advisory for: Central and Southeast Phillips; Central and Southern Valley; Petroleum; Garfield; McCone; Southwest Phillips
3. Special Weather Statement for: Missoula/Bitterroot Valleys; Bitterroot/Sapphire Mountains; Potomac/Seeley Lake Region
4. Wind Advisory for: Livingston Area; Beartooth Foothills
5. Winter Storm Warning for: Absaroka/Beartooth Mountains; Crazy Mountains
6. Winter Storm Warning for: Gallatin and Madison County Mountains and Centennial Mountains
7. Winter Weather Advisory for: Bitterroot/Sapphire Mountains
8. Winter Weather Advisory for: Butte/Blackfoot Region
9. Winter Weather Advisory for: East Glacier Park Region
10. Winter Weather Advisory for: Gallatin Valley
11. Winter Weather Advisory for: Lower Clark Fork Region
12. Winter Weather Advisory for: Madison River Valley
13. Winter Weather Advisory for: Northwest Beaverhead County
14. Winter Weather Advisory for: Potomac/Seeley Lake Region
15. Winter Weather Advisory for: Pryor/Northern Bighorn Mountains; Northeast Bighorn Mountains
16. Winter Weather Advisory for: Red Lodge Foothills; Paradise Valley; Livingston Area; Beartooth Foothills
17. Winter Weather Advisory for: Southern Big Horn; Sheridan Foothills
18. Winter Weather Advisory for: Southern Rocky Mountain Front; Little Belt and Highwood Mountains; Big Belt, Bridger and Castle Mountains
19. Winter Weather Advisory for: West Glacier Region
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North America Water Vapor (Moisture)
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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