Weather Alert in Wisconsin
Severe Thunderstorm Warning issued March 30 at 11:26PM CDT until March 31 at 12:15AM CDT by NWS Green Bay WI
AREAS AFFECTED: Brown, WI; Calumet, WI; Kewaunee, WI; Manitowoc, WI
DESCRIPTION: SVRGRB The National Weather Service in Green Bay has issued a * Severe Thunderstorm Warning for... Southern Brown County in northeastern Wisconsin... Kewaunee County in northeastern Wisconsin... Northeastern Calumet County in east central Wisconsin... Manitowoc County in east central Wisconsin... * Until 1215 AM CDT. * At 1126 PM CDT, severe thunderstorms were located along a line extending from near Brillion to Valders to near Cleveland, moving east at 60 mph. HAZARD...Quarter size hail. SOURCE...Radar indicated. IMPACT...Damage to vehicles is expected. * Severe thunderstorms will be near... Manitowoc and Brillion around 1130 PM CDT. Two Creeks around 1150 PM CDT. Other locations impacted by these severe thunderstorms include Krok, Maribel, Larrabee, Slovan, Gregorville, Curran, Wayside, Morrison, Rankin, and Humboldt.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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