Weather Alert in Wisconsin
Winter Storm Warning issued April 1 at 1:39AM CDT until April 2 at 12:00PM CDT by NWS La Crosse WI
AREAS AFFECTED: Taylor; Clark
DESCRIPTION: ...LATE WINTER STORM IMPACTS THE AREA FROM TONIGHT THROUGH THURSDAY MORNING... .A late season winter storm will impact areas along and north of Interstate 90 from this evening into Thursday morning. Snow, sleet, and freezing rain will begin late this evening, changing to freezing rain overnight. Ice accumulations are expected and will continue into Thursday morning. Temperatures will warm Thursday afternoon and only rain will be expected. Travel is expected to be impacted. * WHAT...Heavy mixed precipitation expected north central Wisconsin. Total snow and sleet accumulations up to one inch and ice accumulations between two tenths and four tenths of an inch. Winds gusting as high as 35 mph. * WHERE...Clark and Taylor Counties. * WHEN...From midnight tonight to noon CDT Thursday. * IMPACTS...Power outages and tree damage are possible due to the ice. The hazardous conditions could impact the Thursday morning commute.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. 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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