Weather Alert in Oklahoma
Flood Advisory issued April 28 at 8:01PM CDT until May 2 at 7:00PM CDT by NWS Norman OK
AREAS AFFECTED: Cotton, OK; Jefferson, OK; Tillman, OK; Clay, TX; Wichita, TX
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Oklahoma...Texas... Red River near Burkburnett affecting Wichita, Clay, Cotton, Tillman and Jefferson Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Red River near Burkburnett. * WHEN...Until Friday evening. * IMPACTS...At 9.0 feet, Crop and range lands... oil fields... and rural roads are affected. Some low-lying areas near the river may be isolated by high water in side channels. Bottomlands near Davidson Oklahoma begin to flood several hours before the crest approaches the Burkburnett area. The flood crest reaches the area along the river near Taylor Oklahoma several hours later. Cattle and other property should be relocated to places which are higher than nearby river banks to avoid being stranded. * ADDITIONAL DETAILS... - At 7:15 PM CDT Monday the stage was 8.6 feet. - Bankfull stage is 9.0 feet. - Forecast...The Red River is near its crest and is expected to begin falling by Tuesday morning. - Action stage is 7.0 feet. - Flood stage is 9.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. 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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