Weather Alert in Mississippi
Flood Warning issued May 9 at 9:34AM CDT until May 14 at 5:00AM CDT by NWS Mobile AL
AREAS AFFECTED: George, MS; Greene, MS; Perry, MS
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Mississippi... Leaf Near McLain affecting Perry, Greene and George Counties. For the Leaf River...including McLain, New Augusta...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Leaf near McLain. * WHEN...From Monday morning to early Wednesday morning. * IMPACTS...At 18.0 feet, Considerable flooding of agricultural and lowlands near the river. * ADDITIONAL DETAILS... - At 9:15 AM CDT Friday the stage was 16.1 feet. - Forecast...The river is expected to rise to a crest of 18.5 feet early Tuesday morning. It will then fall below flood stage late Tuesday evening. - Flood stage is 18.0 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/mob. Click on the Rivers and Lakes menu for forecasts and observations. The next statement will be issued when updates occur.
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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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