Weather Alert in Texas
Flash Flood Warning issued August 12 at 6:17AM CDT until August 12 at 9:00AM CDT by NWS Fort Worth TX
AREAS AFFECTED: Palo Pinto, TX; Parker, TX
DESCRIPTION: FFWFWD The National Weather Service in Fort Worth has issued a * Flash Flood Warning for... Eastern Palo Pinto County in north central Texas... Western Parker County in north central Texas... * Until 900 AM CDT. * At 617 AM CDT, Doppler radar indicated thunderstorms producing heavy rain across northern Palo Pinto and Parker counties. The storms are slowly moving south-southeast, producing radar estimated rainfall rates up to 2 inches of rain per hour. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar. IMPACT...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... Mineral Wells, Brock, Graford, Cool, Lake Mineral Wells, Millsap, Adell, Advance, New Salem, Salesville, Bennett, Garner, Peadenville, Brazos, Brock Junction, Authon, Oran, Whitt, Santo and Dennis. High water flows and lowland flooding is expected along Keechi Creek, particularly along the east fork.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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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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