Weather Alerts for Wyoming
1. Avalanche Warning for: Star Valley; Salt River and Wyoming Ranges
2. High Wind Warning for: Central Laramie County
3. High Wind Warning for: Central Laramie Range and Southwest Platte County
4. High Wind Warning for: East Laramie County
5. High Wind Warning for: East Platte County
6. High Wind Warning for: Ferris/Seminoe/Shirley Mountains; Shirley Basin; Central Carbon County
7. High Wind Warning for: Goshen County
8. High Wind Warning for: Green Mountains and Rattlesnake Range; Natrona County Lower Elevations
9. High Wind Warning for: Laramie Valley
10. High Wind Warning for: North Snowy Range Foothills
11. High Wind Warning for: South Laramie Range; South Laramie Range Foothills
12. High Wind Warning for: South Lincoln County; Rock Springs and Green River; Flaming Gorge; East Sweetwater County
13. High Wind Warning for: Upper North Platte River Basin
14. High Wind Warning for: Wind River Basin
15. High Wind Warning for: Wind River Mountains East; Upper Wind River Basin
16. High Wind Watch for: Absaroka Mountains
17. High Wind Watch for: Cody Foothills
18. Winter Storm Warning for: Sierra Madre Range; Snowy Range
19. Winter Storm Warning for: Teton and Gros Ventre Mountains; Salt River and Wyoming Ranges
20. Winter Storm Warning for: Wind River Mountains West
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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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