Weather Alert in Wyoming
Winter Storm Watch issued February 22 at 11:42AM MST until February 25 at 11:00AM MST by NWS Riverton WY
AREAS AFFECTED: Teton and Gros Ventre Mountains; Salt River and Wyoming Ranges
DESCRIPTION: * WHAT...Heavy snow possible. Total snow accumulations 12 to 18 inches. Accumulations of 18 to 24 inches possible in the Teton Range. West wind frequently gusting 25 to 35 mph, except gusts up to 45 mph in the Teton Range. * WHERE...Teton and Gros Ventre Mountains and Salt River and Wyoming Ranges. * WHEN...From late Monday night through Wednesday morning. * IMPACTS...Travel could be very difficult. The hazardous conditions could impact the Tuesday evening and Wednesday morning commutes. * ADDITIONAL DETAILS...Snowfall totals toward the southern half of the Salt River Range will range from 4 to 10 inches.
INSTRUCTION: Monitor the latest forecasts for updates on this situation.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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