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 Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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