Weather Alerts for Wyoming
1. Freeze Warning for: Cody Foothills; Southwest Bighorn Basin
2. Freeze Warning for: North Bighorn Basin; Southeast Bighorn Basin
3. Freeze Warning for: Wind River Basin; Lander Foothills
4. High Wind Warning for: Ferris/Seminoe/Shirley Mountains; Central Carbon County; North Snowy Range Foothills; Upper North Platte River Basin
5. Winter Storm Warning for: Wind River Mountains West; Wind River Mountains East
6. Winter Storm Warning for: Yellowstone National Park; Absaroka Mountains; Teton and Gros Ventre Mountains
7. Winter Weather Advisory for: Bighorn Mountains West; Bighorn Mountains Southeast
8. Winter Weather Advisory for: Converse County Lower Elevations
9. Winter Weather Advisory for: Ferris/Seminoe/Shirley Mountains; Shirley Basin; Central Carbon County; North Snowy Range Foothills; Southwest Carbon County; Upper North Platte River Basin
10. Winter Weather Advisory for: Green Mountains and Rattlesnake Range; Casper Mountain
11. Winter Weather Advisory for: Natrona County Lower Elevations
12. Winter Weather Advisory for: North Laramie Range
13. Winter Weather Advisory for: Northeast Johnson County; Southeast Johnson County
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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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