Weather Alert in Oklahoma
Flood Advisory issued May 25 at 10:41AM CDT until May 30 at 7:00AM CDT by NWS Norman OK
AREAS AFFECTED: Atoka, OK
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Oklahoma... Clear Boggy Creek near Caney affecting Atoka County. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Clear Boggy Creek near Caney. * WHEN...Until Friday morning. * IMPACTS...At 25.0 feet, The creek remains mostly within its banks in western Atoka County and the northeastern edge of Bryan County. Some high stages on small feeder streams result in very localized... short-term overflows of mainstem bottomlands. Low-lying fields are briefly cut off from easy access. * ADDITIONAL DETAILS... - At 9:30 AM CDT Sunday the stage was 22.9 feet. - Bankfull stage is 26.0 feet. - Forecast...The Clear Boggy Creek is expected to rise to a crest of 25.5 feet early Wednesday morning. - Action stage is 22.0 feet. - Flood stage is 26.0 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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