Weather Alert in Wisconsin
Winter Weather Advisory issued March 14 at 11:04PM CDT until March 15 at 4:00PM CDT by NWS Milwaukee/Sullivan WI
AREAS AFFECTED: Sheboygan; Dodge
DESCRIPTION: * WHAT...For the Winter Weather Advisory, mixed precipitation. Additional snow accumulations one to two inches and ice accumulations around one tenth of an inch. Winds gusting as high as 40 MPH. For the Winter Storm Warning, heavy snow and some mixed precipitation expected. Total snow accumulations between 5 and 8 inches and ice accumulations around a light glaze. Winds gusting as high as 45 MPH leading to blowing to drifting snow. Near blizzard conditions are possible later Sunday night into early Monday morning. * WHERE...Sheboygan and Dodge Counties. * WHEN...For the Winter Weather Advisory, until 4 PM CDT Sunday. For the Winter Storm Warning, from 7 PM Sunday to 4 PM CDT Monday. * IMPACTS...Roads, and especially bridges and overpasses, will likely become slick and hazardous. Visibilities may drop below 1/4 mile due to falling and blowing snow. The strong winds and weight of snow on tree limbs may down power lines and could cause sporadic power outages. Travel could be very difficult. Widespread blowing snow could significantly reduce visibility. The hazardous conditions could impact the Monday morning and evening commutes. Gusty winds could bring down tree branches.
INSTRUCTION: Persons are urged to stay indoors until conditions improve. If you must go outside, dress in layers. Several layers of clothes will keep you warmer than a single heavy coat. Cover exposed skin to reduce your risk of frostbite or hypothermia. Gloves, a scarf, and a hat will keep you from losing your body heat. Persons should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary. The latest road conditions can be obtained by calling 5 1 1.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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