Weather Alert in Wisconsin
Winter Weather Advisory issued February 17 at 11:08PM CST until February 19 at 6:00PM CST by NWS Duluth MN
AREAS AFFECTED: Ashland; Iron
DESCRIPTION: * WHAT...Mixed precipitation. Additional snow accumulations between 1 and 3 inches and ice accumulations around a light glaze. Winds gusting as high as 35 mph. * WHERE...Ashland and Iron Counties. This includes the Tribal Lands of the Bad River Reservation and the northwestern area of the Lac du Flambeau Band. Other locations including Madeline Island. * WHEN...Until 6 PM CST Thursday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Wednesday morning and evening commutes. * ADDITIONAL DETAILS...Snow is favored for the northern half of each County, while ice is more likely for the southern half.
INSTRUCTION: Slow down and use caution while traveling. Call 511 or visit www.511wi.gov for Wisconsin road information.
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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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