Weather Alert in Oklahoma
Flood Warning issued June 18 at 8:21PM CDT until June 20 at 8:12AM CDT by NWS Tulsa OK
AREAS AFFECTED: Adair, OK; Cherokee, OK; Delaware, OK
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Oklahoma... Illinois River at Chewey affecting Delaware, Adair and Cherokee Counties. * WHAT...Minor flooding is forecast. * WHERE...Illinois River at Chewey. * WHEN...From late Thursday night to Friday morning. * IMPACTS...At 12.0 feet, minor flooding occurs from near Fidler's Bend to near Hanging Rock. Road access near the river to residential homes southeast of Chewey Bridge may be compromised. Water begins to impact 630 Road east of the Cherokee/Adair County line. Floating the river is too hazardous due to strong turbulence. * ADDITIONAL DETAILS... - At 7:15 PM CDT Wednesday the stage was 6.3 feet. - Forecast...The river is expected to rise above flood stage early Friday morning to a crest of 12.1 feet early Friday morning. It will then fall below flood stage early Friday morning. - Flood stage is 12.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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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