Weather Alert in Wisconsin
Ice Storm Warning issued April 2 at 2:21AM CDT until April 3 at 1:00AM CDT by NWS Green Bay WI
AREAS AFFECTED: Oneida; Forest
DESCRIPTION: * WHAT...For the Ice Storm Warning, significant icing expected. Total snow and sleet accumulations up to one inch and ice accumulations between two tenths and one half of an inch. Winds gusting as high as 35 mph. For the Winter Storm Watch, significant icing possible. Total ice accumulations between one quarter and three tenths of an inch possible. * WHERE...Oneida and Forest Counties. * WHEN...For the Ice Storm Warning, from 5 AM early this morning to 1 AM CDT Friday. For the Winter Storm Watch, from Friday evening through Saturday morning. * IMPACTS...Power outages and tree damage are likely due to the ice. Travel could be hazardous due to icy roads. The hazardous conditions will impact the Thursday morning and evening commutes.
INSTRUCTION: Travel is strongly discouraged. If you must travel, keep an extra flashlight, food and water in your vehicle in case of an emergency. Prepare for possible power outages. The latest road conditions can be obtained by calling 5 1 1. For the Winter Storm Watch, monitor the latest forecasts for updates on this situation.
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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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