Weather Alert in Texas
Severe Thunderstorm Warning issued September 5 at 9:11PM CDT until September 5 at 10:00PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Lamar, TX
DESCRIPTION: At 911 PM CDT, severe thunderstorms were located along a line extending from Boswell to Paris to Sulphur Bluff, moving east at 40 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. These severe storms will be near... Paris, Reno, Camp Maxey, Powderly, Pattonville, Lake Crook, and Pat Mayse Lake around 915 PM CDT. Blossom and Arthur City around 920 PM CDT. Other locations impacted by these severe thunderstorms include Glory, Direct, Midcity, Minter, Forest Hill, Petty, Taylor Town, Globe, Brookston, and Sun Valley.
INSTRUCTION: For your protection stay inside a sturdy structure and keep away from windows. Continuous cloud to ground lightning is occurring with these storms. Move indoors immediately.
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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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