Weather Alert in Utah
Winter Weather Advisory issued February 23 at 2:32PM MST until February 25 at 5:00PM MST by NWS Salt Lake City UT
AREAS AFFECTED: Wasatch Mountains I-80 North; Wasatch Mountains South of I-80; Western Uinta Mountains
DESCRIPTION: * WHAT...Snow expected above 8000 feet. Above 8000 feet, 2 to 8 inches expected. Above 9000 feet, 6 to 16 inches expected. Locally higher amounts to 18 inches possible for the Bear River Range and Upper Cottonwoods. Winds gusting as high as 80 mph across exposed mountain ridgelines. * WHERE...The Wasatch Mountains, and Western Uinta Mountains. * WHEN...From 8 AM Tuesday to 5 PM MST Wednesday. * IMPACTS...Travel could be difficult at times along high elevation routes like Logan Summit, the Upper Cottonwoods, and Wolf Creek Pass. Traction law restrictions may be enacted. Gusty winds could bring down tree branches. * ADDITIONAL DETAILS...Snow levels begin around 6500 feet at the onset of precipitation, but quickly rise to around 8000 feet by Tuesday afternoon. Snow levels may rise as high as 10000 feet overnight under heavy precipitation. Snow character will be heavy and wet given the warm nature of this storm.
INSTRUCTION: Dangerous conditions already exist in the backcountry, per the Utah Avalanche Center. Heavy, wet snow is expected, so backcountry users should exercise extra caution and consult utahavalanchecenter.org for avalanche forecasts. 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 Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
Weather Topic: What are Hole Punch Clouds?
Home - Education - Cloud Types - Hole Punch Clouds
Next Topic: Mammatus Clouds
A hole punch cloud is an unusual occurrence when a disk-shaped
hole appears in a cirrostratus, cirrocumulus, or altocumulus cloud.
When part of the cloud forms ice crystals, water droplets in the surrounding area
of the cloud evaporate. The effect of this process produces a large elliptical
gap in the cloud. The hole punch cloud formation is rare, but it is not specific
to any geographic area.
Other names which have been used to describe this phenomena include fallstreak hole,
skypunch, and cloud hole.
Next Topic: Mammatus Clouds
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