Weather Alert in Texas
Flood Warning issued May 10 at 8:43PM CDT by NWS Shreveport LA
AREAS AFFECTED: Gregg, TX; Smith, TX; Upshur, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Sabine River Near Gladewater affecting Smith, Gregg and Upshur Counties. For the Sabine River...including Mineola, Hawkins, Gladewater, Longview, Beckville, Logansport...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Sabine River near Gladewater. * WHEN...Until further notice. * IMPACTS...At 32.0 feet, Lowland flooding will continue to slowly decrease over the next several days. * ADDITIONAL DETAILS... - At 8:15 PM CDT Saturday the stage was 25.8 feet. - Bankfull stage is 25.0 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight and continue rising to a crest of 30.9 feet Thursday morning. - Flood stage is 26.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Sunday evening at 845 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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