Weather Alert in Wisconsin
Winter Storm Warning issued March 13 at 9:26PM CDT until March 16 at 4:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Lincoln; Langlade; Menominee; Door; Marathon; Shawano; Southern Oconto County
DESCRIPTION: * WHAT...Heavy snow expected, briefly mixed with sleet late Saturday night into early Sunday. Total snow accumulations between 18 and 24 inches with local higher amounts possible. Winds gusting as high as 45 mph will result in considerable blowing and drifting snow and possible blizzard conditions late Sunday into Monday. * WHERE...Marathon, Langlade, Lincoln, Door, Menominee, Shawano, and Southern Oconto counties. * WHEN...From 7 PM Saturday to 4 PM CDT Monday. * IMPACTS...Travel could be very difficult to impossible with potential for whiteout conditions. Gusty winds could bring down tree branches and cause power outages. The Monday morning commute will be impacted.
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1. People should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary.
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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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