Weather Alert in Utah

Recent Locations: Piedmont, CA   Evans City, PA   Nephi, UT  

Winter Weather Advisory issued February 23 at 10:13PM 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 Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

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

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