Weather Alert in Wyoming
Winter Storm Warning issued February 23 at 11:49AM 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 will 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 Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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