Weather Alert in Michigan
Winter Storm Watch issued April 2 at 5:17AM CDT until April 4 at 10:00AM CDT by NWS Marquette MI
AREAS AFFECTED: Luce
DESCRIPTION: * WHAT...For the Winter Weather Advisory, mixed precipitation expected. Total snow and sleet accumulations up to one inch and ice accumulations up to two tenths of an inch. Winds gusting as high as 35 mph. For the Winter Storm Watch, significant icing possible. Total ice accumulations around two tenths of an inch possible. * WHERE...Luce County. * WHEN...For the Winter Weather Advisory, from 11 AM this morning to 11 PM EDT this evening. For the Winter Storm Watch, from late Friday night through Saturday morning. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Thursday evening and Friday morning commutes.
INSTRUCTION: Slow down and use caution while traveling. Monitor the latest forecasts for updates on this situation.
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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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