Weather Alert in Minnesota
Special Weather Statement issued September 4 at 6:09PM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Sibley; Brown; Nicollet; Le Sueur; Watonwan; Blue Earth; Martin; Faribault
DESCRIPTION: At 609 PM CDT, Doppler radar was tracking an area of strong thunderstorms extending from over Gibbon to over Comfrey, or extending from 15 miles north of New Ulm to 28 miles southwest of New Ulm, moving southeast at 55 mph. HAZARD...Wind gusts of 50 to 55 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Mankato, New Ulm, North Mankato, St. Peter, St. James, Sleepy Eye, Lake Crystal, Eagle Lake, Madelia, Truman, Nicollet, Kasota, Courtland, Butterfield, Good Thunder, Amboy, Lafayette, Hanska, Comfrey and Vernon Center.
INSTRUCTION: Monitor the weather situation closely and be alert for threatening weather conditions.
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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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