Weather Alert in Wisconsin
Winter Storm Watch issued March 31 at 8:49PM CDT until April 2 at 1:00PM CDT by NWS Green Bay WI
AREAS AFFECTED: Lincoln; Langlade; Menominee; Northern Oconto County; Marathon; Shawano; Southern Marinette County; Southern Oconto County
DESCRIPTION: * WHAT...Heavy sleet and freezing rain possible. Total snow and sleet accumulations of 1 to 2 inches and ice accumulations between 1/4 and 1/2 inch possible. * WHERE...Marathon, Langlade, Lincoln, Menominee, Northern Oconto County, Shawano, Southern Marinette County, and Southern Oconto counties. * WHEN...From late Wednesday night through Thursday afternoon. * IMPACTS...Significant ice accumulation on power lines and tree limbs may cause tree damage and power outages. Travel could be nearly impossible. The hazardous conditions will likely impact the Thursday morning commute.
INSTRUCTION: Monitor the latest forecasts for updates on this situation. People should consider delaying all travel. If travel is absolutely necessary, drive with extreme caution. Consider taking a winter storm kit along with you, including such items as tire chains, booster cables, flashlight, shovel, blankets and extra clothing. Also take water, a first aid kit, and anything else that would help you survive in case you become stranded.
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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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