Weather Alert in Texas
Special Weather Statement issued September 5 at 4:35PM CDT by NWS San Angelo TX
AREAS AFFECTED: Runnels; Jones; Shackelford; Taylor; Callahan; Coleman
DESCRIPTION: At 434 PM CDT, Doppler radar was tracking a strong thunderstorms from Ballinger to Abilene, moving northeast at 35 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... Abilene, Clyde, Winters, Baird, Tye, Tuscola, Buffalo Gap, Lawn, Dudley, Bradshaw, Caps, Dyess Afb, Eula, Potosi, View, Wingate, Happy Valley, Hamby, Nugent, and Coronados Camp. People attending West Texas Fair and Rodeo should seek safe shelter immediately! This includes Interstate 20 between Mile Markers 277 and 313.
INSTRUCTION: If outdoors, consider seeking shelter inside 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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