Weather Alert in Wyoming
High Wind Watch issued February 22 at 11:23AM MST until February 24 at 5:00PM MST by NWS Riverton WY
AREAS AFFECTED: Wind River Mountains East; Upper Wind River Basin
DESCRIPTION: * WHAT...West winds 30 to 40 mph with gusts around 60 mph possible. Gusts around Red Canyon and the east slope of the central and southern Wind River Range could climb to around 75 mph. * WHERE...Upper Wind River Basin and Wind River Mountains East. * WHEN...From Monday evening through Tuesday afternoon. * IMPACTS...Travel could be difficult, especially for high profile vehicles traveling Wyoming Highway 28 around Red Canyon. * ADDITIONAL DETAILS...Wind gusts 50 to 60 mph are possible in Dubois and the surrounding valley, while gusts around Red Canyon near South Pass could see gusts around 75 mph.
INSTRUCTION: Monitor the latest forecasts and warnings for updates.
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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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