Weather Alert in Texas
Flood Warning issued April 29 at 2:04PM CDT by NWS Norman OK
AREAS AFFECTED: Wichita, TX; Wilbarger, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Beaver Creek near Electra affecting Wilbarger and Wichita Counties. * WHAT...Major flooding is forecast. * WHERE...Beaver Creek near Electra. * WHEN...From late tonight until further notice. * IMPACTS...At 29.0 feet, Widespread flood levels up to 5 feet in depth cover farm and range lands... and may inundate some oil and gas facilities... along and near the creek in southern Wilbarger County and southwestern Wichita County. * ADDITIONAL DETAILS... - At 1:00 PM CDT Tuesday the stage was 12.4 feet. - Bankfull stage is 24.0 feet. - Forecast...The river will rise above flood stage late tonight to 29.0 feet early Thursday afternoon. - Flood stage is 24.0 feet. - Flood History...This crest compares to a previous crest of 29.0 feet on 04/20/1990. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Additional information is available at www.weather.gov.
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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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