Weather Alert in Texas
Flood Warning issued May 4 at 9:37AM CDT by NWS Shreveport LA
AREAS AFFECTED: Anderson, TX; Cherokee, TX; Houston, TX; Trinity, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Neches River Near Alto affecting Anderson, Trinity, Cherokee and Houston Counties. For the Neches River...including Neches, Alto, Diboll...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Neches River near Alto. * WHEN...From this afternoon until further notice. * IMPACTS...At 18.0 feet, Expect flooding of the heavily wooded floodplain. Boat ramps and picnic areas will be completely inundated. * ADDITIONAL DETAILS... - At 9:15 AM CDT Sunday the stage was 15.9 feet. - Bankfull stage is 16.0 feet. - Forecast...The river is expected to rise above flood stage this afternoon and continue rising to a crest of 17.5 feet early Wednesday morning. - Flood stage is 16.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. For more hydrologic information, copy and paste the following website address into your favorite web browser URL bar: https://water.noaa.gov/wfo/SHV The next statement will be issued Monday morning at 945 AM 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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