Weather Alert in Oklahoma
Flood Advisory issued May 7 at 8:50AM CDT until May 8 at 1:00PM CDT by NWS Norman OK
AREAS AFFECTED: Jefferson, OK
DESCRIPTION: ...The Flood Advisory is extended for the following rivers in Oklahoma... Beaver Creek at Waurika affecting Jefferson County. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Beaver Creek at Waurika. * WHEN...Until early tomorrow afternoon. * IMPACTS...At 22.0 feet, Flooding of lowlands along the creek in Jefferson County extends from near Waurika to near Sugden... southward to the confluence of Beaver Creek with the Red River. * ADDITIONAL DETAILS... - At 8:00 AM CDT Wednesday the stage was 20.5 feet. - Bankfull stage is 25.0 feet. - Forecast...The Beaver Creek is expected to rise to a crest of 21.9 feet this afternoon. - Action stage is 20.0 feet. - Flood stage is 25.0 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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