Weather Alert in Wisconsin
Winter Weather Advisory issued April 1 at 3:11AM CDT until April 2 at 12:00PM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Polk; Barron; Rusk
DESCRIPTION: ...MESSY SPRING SYSTEM BRINGS FREEZING RAIN, SLEET, AND SNOWTO PORTIONS OF MINNESOTA AND WISCONSIN TONIGHT THROUGH THURSDAY... .A strong spring system brings a variety of precipitation types to the region tonight through Thursday. While there is still some uncertainty in the exact track of the low, mainly snow & sleet is expected across central Minnesota, while a mix of freezing rain, sleet, & snow is expected for southern Minnesota, the Twin Cities metro, & western Wisconsin. The greatest travel impacts are expected across eastern Minnesota & west-central Wisconsin where icing amounts around 0.25" are likely, along with sleet & snow at times. This will lead to very slick roads, as well as the possibility of some downed tree branches & power outages. Elsewhere, freezing rain accumulations around 0.1" along with an inch or two of sleet & snow will lead to slick roads late Wednesday night through Thursday morning. * WHAT...Mixed precipitation expected. Total snow accumulations up to one inch, sleet accumulations around 1 inch, and ice accumulations between one tenth and two tenths of an inch. * WHERE...Barron, Polk, and Rusk Counties. * WHEN...From midnight tonight to noon CDT Thursday. * IMPACTS...Roads, and especially bridges and overpasses, will likely become slick and hazardous. Plan on slippery road conditions. The hazardous conditions will impact the Wednesday evening and Thursday morning commutes.
INSTRUCTION: Slow down and use caution while traveling. Call 5 1 1 or visit 511wi.gov for road conditions.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - 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
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