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 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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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