Weather Alerts for Wyoming
1. High Wind Watch for: South Laramie Range; South Laramie Range Foothills
2. Winter Storm Warning for: Sierra Madre Range
3. Winter Weather Advisory for: Bighorn Mountains West; Bighorn Mountains Southeast
4. Winter Weather Advisory for: Converse County Lower Elevations; Niobrara County; North Laramie Range
5. Winter Weather Advisory for: Green Mountains and Rattlesnake Range; Natrona County Lower Elevations; Casper Mountain
6. Winter Weather Advisory for: Jackson Hole; Star Valley
7. Winter Weather Advisory for: Northeast Johnson County; Southeast Johnson County
8. Winter Weather Advisory for: Snowy Range
9. Winter Weather Advisory for: Southwest Bighorn Basin; Southeast Bighorn Basin; Owl Creek and Bridger Mountains
10. Winter Weather Advisory for: Southwest Wyoming
11. Winter Weather Advisory for: Teton and Gros Ventre Mountains; Wind River Mountains West; Wind River Mountains East; Salt River and Wyoming Ranges
12. Winter Weather Advisory for: Wind River Basin; Lander Foothills
13. Winter Weather Advisory for: Yellowstone National Park
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Current U.S. National Radar--Current
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North America Water Vapor (Moisture)
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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