Weather Alert in Oklahoma
Flood Advisory issued August 28 at 2:28AM CDT until August 30 at 1:00AM CDT by NWS Norman OK
AREAS AFFECTED: Kingfisher, OK; Logan, OK
DESCRIPTION: ...The National Weather Service in Norman has issued a Flood Advisory for the following rivers in Oklahoma... Salt Fork Arkansas River near Alva affecting Woods and Alfalfa Counties. Chikaskia River near Blackwell affecting Kay and Grant Counties. Cimarron River near Dover affecting Kingfisher and Logan Counties. * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Cimarron River near Dover. * WHEN...From early this morning to early Saturday morning. * IMPACTS...At 15.0 feet, The river remains within its banks through Kingfisher County and into western Logan County. Some oilfield equipment in low bottoms may be isolated for a short time. * ADDITIONAL DETAILS... - At 1:30 AM CDT Thursday the stage was 10.9 feet. - Bankfull stage is 17.0 feet. - Forecast...The Cimarron River is expected to rise to a crest of 15.3 feet tomorrow morning. - Action stage is 15.0 feet. - Flood stage is 17.0 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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