Weather Alert in Michigan
Blizzard Warning issued March 14 at 8:31PM EDT until March 17 at 8:00AM EDT by NWS Marquette MI
AREAS AFFECTED: Alger; Luce; Delta; Southern Schoolcraft; Northern Schoolcraft
DESCRIPTION: * WHAT...Blizzard conditions expected. Total snow accumulations between 2 and 3 feet, locally higher amounts up to 4 feet possible. Winds gusting as high as 60 mph. * WHERE...Alger, Delta, Luce, Northern Schoolcraft, and Southern Schoolcraft Counties. * WHEN...From 5 AM Sunday to 8 AM EDT Tuesday. * IMPACTS...Travel will be treacherous and potentially life-threatening. Widespread blowing snow and heavy snowfall rates will significantly reduce visibility. Strong winds could cause tree damage and result in power outages. * ADDITIONAL DETAILS...Heavy snowfall rates of 1 to 3 inches per hour are expected much of the day Sunday. Strongest winds late Sunday afternoon into Monday.
INSTRUCTION: Travel should be restricted to emergencies only. If you must travel, have a winter survival kit with you. If you get stranded, stay with your vehicle.
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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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