Weather Alert in Michigan
Winter Weather Advisory issued February 5 at 8:52PM EST until February 6 at 10:00AM EST by NWS Marquette MI
AREAS AFFECTED: Keweenaw; Ontonagon; Houghton; Gogebic
DESCRIPTION: * WHAT...Lake effect snow and blowing snow expected. Total snow accumulations up to three inches. Winds gusting as high as 40 mph creating areas of blowing snow. * WHERE...Gogebic, Keweenaw, Northern Houghton, and Ontonagon Counties. * WHEN...From 1 AM EST /midnight CST/ to 10 AM EST /9 AM CST/ Friday. * IMPACTS...Plan on slippery road conditions. Areas of blowing snow will significantly reduce visibilities, particularly near the lakeshore. The hazardous conditions will impact the Friday morning commute.
INSTRUCTION: Slow down and use caution while traveling.
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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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