Weather Alert in Michigan
Special Weather Statement issued March 21 at 11:07AM EDT by NWS Gaylord MI
AREAS AFFECTED: Western Chippewa; Central Chippewa; Southeast Chippewa; Western Mackinac; Eastern Mackinac; Mackinac Island/Bois Blanc Island
DESCRIPTION: A wet, slushy snow is set to fall this afternoon into the evening across eastern upper Michigan. Reductions in visibility will be possible during periods of heavier snow, and roads may become slushy / slippery. A general 1 to 3 inches of snowfall is anticipated through sunset, heaviest toward the M-28 corridor and points north, including Sault Ste. Marie. In the wake of this snowfall, drizzly precipitation is set to linger through the evening into tonight. With temperatures hovering right around 32, a glaze of ice is possible on top of the snow that falls. While hazardous travel is not anticipated to prevail, wintry driving conditions will be possible this afternoon through tonight across eastern upper Michigan, including the Mackinac Bridge. Be cognizant of road conditions and give yourself some extra distance between yourself and the vehicle in front of you.
INSTRUCTION: N/A
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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