Weather Alert in Oklahoma
Flood Warning issued May 27 at 8:17PM CDT until May 29 at 6:30AM CDT by NWS Norman OK
AREAS AFFECTED: Atoka, OK
DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Clear Boggy Creek near Caney affecting Atoka County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Clear Boggy Creek near Caney. * WHEN...Until Thursday 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 PM CDT Tuesday the stage was 28.8 feet. - Bankfull stage is 26.0 feet. - Forecast...The Clear Boggy Creek is expected to fall below flood stage early Thursday morning and continue falling. - 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 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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