Weather Alert in Oklahoma
Flood Warning issued April 28 at 8:02PM CDT until April 30 at 3:20AM CDT by NWS Norman OK
AREAS AFFECTED: Cotton, OK
DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Deep Red Creek near Randlett affecting Cotton County. * WHAT...Moderate flooding is occurring and moderate flooding is forecast. * WHERE...Deep Red Creek near Randlett. * WHEN...Until early Wednesday morning. * IMPACTS...At 24.0 feet, Valley-wide flooding of croplands... pastures... and local roads occurs and is accompanied by flood depths up to 4 feet with swift currents. * ADDITIONAL DETAILS... - At 7:30 PM CDT Monday the stage was 24.0 feet. - Bankfull stage is 20.0 feet. - Forecast...The Deep Red Creek is expected to fall below flood stage late tomorrow evening and continue falling. - Flood stage is 20.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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 is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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