Weather Alert in Wyoming
Winter Storm Warning issued February 23 at 1:12AM MST until February 25 at 5:00PM MST by NWS Riverton WY
AREAS AFFECTED: Absaroka Mountains
DESCRIPTION: * WHAT...Heavy snow possible. Total snow accumulations 15 to 25 inches over the western half of the Absaroka Range, with 4 to 10 inches over the eastern half. West wind frequently gusting 35 to 45 mph. West winds gusting 60 to 70 mph will occur Wednesday, with the stronger gusts occurring on the east side of the range. * WHERE...Absaroka Mountains. * WHEN...From 5 AM Tuesday to 5 PM MST Wednesday. * IMPACTS...Travel could be very difficult. * ADDITIONAL DETAILS...A High Wind Warning is also in effect for the Absaroka Mountains through Tuesday morning due to stronger wind speeds expected in areas where snowfall will be not as heavy.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. For graphical depictions of the snowfall forecast, including the official NWS forecast, high end amounts, and low end amounts, visit https://weather.gov/riw/winter . For winter road conditions from the Wyoming Department of Transportation, visit https://wyoroad.info .
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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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