Weather Alert in Michigan
Special Weather Statement issued February 5 at 11:01AM EST by NWS Detroit/Pontiac MI
AREAS AFFECTED: Midland; Bay; Huron; Saginaw; Tuscola; Sanilac; Shiawassee; Genesee; Lapeer; Livingston
DESCRIPTION: Light to briefly moderate intensity snowfall continues to spread southeastward across southern Lower Michigan this morning. Snowfall rates of around a tenth of an inch per hour expected. Visibility reductions below a mile are possible at times. Total new snow accumulations of up to a half inch possible through this evening. Temperatures will hover in the upper teens to lower 20s with southerly winds of 10 to 15 mph. Untreated roadways will become slick and snow covered. Drivers should exercise caution and be prepared for variable road conditions. Obtain the latest road conditions from the MDOT MiDrive Map. If you are going outside, watch your first few steps taken on stairs, sidewalks, and driveways. These surfaces could become snow covered and slippery, increasing your risk of a fall and injury.
INSTRUCTION: N/A
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North America Water Vapor (Moisture)
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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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