Weather Alert in Colorado
Severe Thunderstorm Warning issued August 24 at 3:10PM MDT until August 24 at 4:45PM MDT by NWS Goodland KS
AREAS AFFECTED: Cheyenne, CO
DESCRIPTION: SVRGLD The National Weather Service in Goodland has issued a * Severe Thunderstorm Warning for... Western Cheyenne County in east central Colorado... * Until 445 PM MDT. * At 309 PM MDT, a severe thunderstorm was located 12 miles south of Flagler, moving south at 25 mph. HAZARD...Golf ball size hail. SOURCE...Trained weather spotters on I-70. IMPACT...People and animals outdoors will be injured. Expect damage to roofs, siding, windows, and vehicles. * This severe thunderstorm will remain over mainly rural areas of western Cheyenne County in east central Colorado, including the following locations... Wild Horse and Aroya.
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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