Weather Alert in Texas
Flood Warning issued June 13 at 11:11AM CDT by NWS Shreveport LA
AREAS AFFECTED: Gregg, TX; Harrison, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Sabine River At Longview affecting Gregg and Harrison Counties. For the Sabine River near Longview...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Sabine River at Longview. * WHEN...From Sunday afternoon until further notice. * IMPACTS...At 25.0 feet, Expect minor lowland flooding with boat ramps flooded. * ADDITIONAL DETAILS... - At 10:00 AM CDT Friday the stage was 22.2 feet. - Bankfull stage is 25.0 feet. - Forecast...The river is expected to rise above flood stage early Sunday afternoon and continue rising to 25.2 feet Monday morning. Additional rises are possible thereafter. - Flood stage is 25.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. 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 Saturday morning at 1115 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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