Weather Alert in Texas
Flood Warning issued May 9 at 8:55PM CDT by NWS Shreveport LA
AREAS AFFECTED: Angelina, TX; Nacogdoches, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Angelina River Near Lufkin affecting Angelina and Nacogdoches Counties. For the Angelina River...including Alto, Lufkin...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Angelina River near Lufkin. * WHEN...Until further notice. * IMPACTS...At 165.0 feet, Expect flooding to continue for several days with the majority of the gravel access roadway flooded. Boaters and four wheel-operators should use caution traversing both upstream and downstream on the Angelina River as currents can become swift and turbulent. * ADDITIONAL DETAILS... - At 8:30 PM CDT Friday the stage was 165.1 feet. - Bankfull stage is 158.5 feet. - Forecast...The river is expected to remain steady above flood stage at 165.0 feet. - Flood stage is 161.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Saturday evening at 900 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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