Weather Alert in Wisconsin
Winter Storm Warning issued March 14 at 2:06AM CDT until March 16 at 4:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Vilas; Oneida; Forest; Florence; Northern Marinette County; Northern Oconto County; Southern Marinette County
DESCRIPTION: * WHAT...Heavy snow expected. Total snow accumulations between 18 and 24 inches, with locally higher amounts to 30 inches possible. Winds gusting as high as 45 mph may result in considerable blowing and drifting snow and near blizzard conditions late Sunday into Monday. * WHERE...Oneida, Vilas, Florence, Forest, Northern Marinette County, Northern Oconto County, and Southern Marinette counties. * WHEN...From 1 AM Sunday 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 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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