Weather Alert in Utah
Winter Storm Warning issued February 16 at 2:10PM MST until February 18 at 5:00PM MST by NWS Salt Lake City UT
AREAS AFFECTED: Southern Mountains
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 8 and 18 inches with locally higher accumulations up to 2 to 3 feet near Brian Head and in the Tushar Mountains. Winds gusting as high as 60 mph through Monday night. * WHERE...Southern Mountains. * WHEN...From 5 PM this afternoon to 5 PM MST Wednesday. * IMPACTS...Winter driving conditions can be expected on all mountain routes. Traction restrictions are likely. * ADDITIONAL DETAILS...A period of heavy snow is expected Monday night, with snowfall continuing into Tuesday afternoon. A brief lull is expected Tuesday afternoon before ramping up again Tuesday evening. Another round of heavy snow is expected Wednesday. Very strong winds, peaking Monday evening, will persist through at least Wednesday.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. For winter road conditions from the Utah Department of Transportation, visit http://www.udottraffic.utah.gov. For graphical depictions of the snowfall forecast, including Official NWS Forecast, High End Amount, and Low End Amount, visit weather.gov/slc/winter.
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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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