Weather Alert in Texas
Flood Warning issued May 8 at 8:19PM CDT by NWS Shreveport LA
AREAS AFFECTED: Smith, TX; Upshur, TX; Wood, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Sabine River Near Hawkins affecting Smith, Upshur and Wood 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 Hawkins. * WHEN...From Saturday afternoon until further notice. * IMPACTS...At 25.0 feet, Minor lowland flooding of pastures and boatramps. Move livestock and equipment to higher ground. * ADDITIONAL DETAILS... - At 7:45 PM CDT Thursday the stage was 21.4 feet. - Bankfull stage is 22.0 feet. - Forecast...The river is expected to rise above flood stage Saturday afternoon and continue rising to 26.8 feet Tuesday evening. Additional rises are possible thereafter. - Flood stage is 23.0 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 Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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