Weather Alert in Texas
Flash Flood Warning issued August 29 at 11:51AM CDT until August 29 at 1:30PM CDT by NWS Shreveport LA
AREAS AFFECTED: Gregg, TX; Harrison, TX; Marion, TX; Upshur, TX
DESCRIPTION: FFWSHV The National Weather Service in Shreveport has extended the * Flash Flood Warning for... Gregg County in northeastern Texas... Harrison County in northeastern Texas... Western Marion County in northeastern Texas... Upshur County in northeastern Texas... * Until 130 PM CDT. * At 1151 AM CDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar indicated. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. * Some locations that will experience flash flooding include... Longview, Marshall, Kilgore, White Oak, Gladewater, Gilmer, Hallsville, Ore City, Clarksville City, East Mountain, Harleton, Diana, Cedar Springs, West Mountain, Woodlawn, Liberty City, Elysian Fields, Lakeport, Scottsville and Union Grove.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads.
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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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