Weather Alert in Oklahoma
Flood Warning issued April 19 at 8:07AM CDT until April 23 at 8:10AM CDT by NWS Norman OK
AREAS AFFECTED: Atoka, OK
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Warning for the following rivers in Oklahoma... Clear Boggy Creek near Caney affecting Atoka County. * WHAT...Minor flooding is forecast. * WHERE...Clear Boggy Creek near Caney. * WHEN...From Sunday morning to Wednesday morning. * IMPACTS...At 29.0 feet, Creek levels rise to three feet higher than flood stage in western Atoka County and the northeastern edge of Bryan County. High stages on small feeder streams result in even greater depths to mainstem bottomlands near their points of entry into Clear Boggy Creek. Croplands... pastures... and some secondary rural roads are flooded. * ADDITIONAL DETAILS... - At 7:30 AM CDT Saturday the stage was 10.6 feet. - Bankfull stage is 26.0 feet. - Forecast...The Clear Boggy Creek is expected to rise above flood stage tomorrow morning to a crest of 28.7 feet Monday morning. It will then fall below flood stage early Wednesday morning. - Flood stage is 26.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov.
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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