Weather Alert in Wisconsin
Winter Storm Warning issued March 13 at 1:40PM CDT until March 16 at 4:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Lincoln; Langlade; Menominee; Door; Marathon; Shawano; Wood; Portage; Waupaca; Outagamie; Brown; Kewaunee; Waushara; Winnebago; Calumet; Manitowoc; Southern Oconto County
DESCRIPTION: * WHAT...Heavy mixed precipitation expected. Total snow accumulations 12 and 18 inches with localized higher amounts and ice accumulations around a light glaze. Winds gusting as high as 45 mph may result in blizzard conditions late Sunday into Monday. * WHERE...Portions of central, east central, north central, and northeast Wisconsin. * WHEN...From 7 PM Saturday to 4 PM CDT Monday. * IMPACTS...Travel could be very difficult to impossible with potential for whiteout conditions. Gusty winds could bring down tree branches and cause power outages. The Monday morning commute will be impacted.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1. People should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary.
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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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