Weather Alert in Texas
Flood Warning issued May 8 at 8:24PM CDT until May 11 at 6:20AM CDT by NWS Shreveport LA
AREAS AFFECTED: Franklin, TX; Morris, TX; Red River, TX; Titus, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Sulphur River Near Talco affecting Red River, Titus, Morris and Franklin Counties. For the Sulphur River...including Talco...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Sulphur River near Talco. * WHEN...Until Sunday morning. * IMPACTS...At 25.0 feet, Expect minor flooding of lowland areas with a few secondary roadways closed. All cattle and equipment nearby the river should be moved to higher ground. * ADDITIONAL DETAILS... - At 7:45 PM CDT Thursday the stage was 23.8 feet. - Bankfull stage is 20.0 feet. - Forecast...The river is expected to fall below flood stage early Saturday afternoon and continue falling to 14.9 feet Tuesday evening. - Flood stage is 20.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Friday evening at 830 PM CDT.
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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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