Weather Alerts for Montana
1. Avalanche Warning for: Potomac/Seeley Lake Region
2. High Wind Warning for: Cascade County below 5000ft; Judith Basin County and Judith Gap; Upper Blackfoot and MacDonald Pass; Gates of the Mountains; Little Belt and Highwood Mountains; Helena Valley; Big Belt, Bridger and Castle Mountains
3. High Wind Warning for: Cascade County below 5000ft; Judith Basin County and Judith Gap; Upper Blackfoot and MacDonald Pass; Gates of the Mountains; Little Belt and Highwood Mountains; Helena Valley; Big Belt, Bridger and Castle Mountains
4. High Wind Warning for: Central and Southeast Phillips; Northern Phillips; Southwest Phillips
5. High Wind Warning for: East Glacier Park Region; Northern High Plains; Southern Rocky Mountain Front; Southern High Plains
6. High Wind Warning for: East Glacier Park Region; Northern High Plains; Southern Rocky Mountain Front; Southern High Plains
7. High Wind Warning for: Eastern Glacier, Western Toole, and Central Pondera
8. High Wind Warning for: Eastern Glacier, Western Toole, and Central Pondera
9. High Wind Warning for: Eastern Toole and Liberty; Northern Blaine County; Western and Central Chouteau County; Bears Paw Mountains and Southern Blaine
10. High Wind Warning for: Meagher County Valleys; Elkhorn and Boulder Mountains; Canyon Ferry Area; Missouri Headwaters; Madison River Valley; Gallatin Valley; Beaverhead and Western Madison below 6000ft
11. High Wind Warning for: Northern Stillwater; Golden Valley; Judith Gap; Northern Sweet Grass; Melville Foothills; Southern Wheatland
12. Wind Advisory for: Livingston Area; Beartooth Foothills
13. Winter Storm Warning for: Absaroka/Beartooth Mountains
14. Winter Weather Advisory for: Pryor/Northern Bighorn Mountains; Northeast Bighorn Mountains
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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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