Weather Alert in Illinois
Flood Warning issued May 8 at 9:42AM CDT until May 10 at 10:00AM CDT by NWS Paducah KY
AREAS AFFECTED: Gallatin, IL; Wayne, IL; White, IL
DESCRIPTION: ...The Flood Warning continues for the following river in Illinois... Little Wabash River at Carmi. .The Little Wabash is continuing a very slow fall, and is forecast to drop below flood stage Saturday morning. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Little Wabash River at Carmi. * WHEN...Until late Saturday morning. * ADDITIONAL DETAILS... - At 8:30 AM CDT Thursday the stage was 27.4 feet. - Forecast...The river is expected to fall below flood stage early Saturday morning. - Flood stage is 27.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. 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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