Weather Alert in Utah
Winter Weather Advisory issued March 31 at 10:30PM MDT until April 1 at 12:00PM MDT by NWS Salt Lake City UT
AREAS AFFECTED: Wasatch Mountains South of I-80; Western Uinta Mountains; Wasatch Plateau/Book Cliffs; Central Mountains; Southern Mountains
DESCRIPTION: * WHAT...Snow, mainly above 7500 feet across the northern Utah mountains to above 8500 feet in the southern Utah mountains. Snow accumulations of 4 to 8 inches in the northern mountains, with upwards of 10 to 14 inches in the upper Cottonwoods. Snow accumulations of 8 to 14 inches in the central and southern mountains, with upwards of 18 inches in the Tushar Mountains and Brian Head area. * WHERE...Central Mountains, Wasatch Plateau/Book Cliffs, Wasatch Mountains South of I-80, Western Uinta Mountains, and Southern Mountains. * WHEN...Until noon MDT Wednesday. * IMPACTS...Winter driving conditions are expected for elevations above 7,500ft in the northern mountains, 8,000ft in the central mountains, and 8,500ft in the southern mountains. * ADDITIONAL DETAILS...Snow levels will be starting out around 9000 to 9500 feet at the onset of heavier precipitation and will gradually lower through the overnight hours. The lowest snow levels are expected by early to mid-morning on Wednesday as moisture begins to taper off.
INSTRUCTION: Slow down and use caution while traveling. 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 is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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