Weather Alert in Louisiana
Flood Warning issued May 9 at 12:12PM CDT until May 13 at 1:00AM CDT by NWS Lake Charles LA
AREAS AFFECTED: Acadia, LA; Evangeline, LA; St. Landry, LA
DESCRIPTION: ...Forecast flooding changed from Minor to Moderate severity and increased in duration for the following rivers in Louisiana... Bayou Des Cannes Near Eunice Additional information is available at www.weather.gov. * WHAT...Minor flooding is occurring and moderate flooding is forecast. * WHERE...Bayou Des Cannes near Eunice. * WHEN...Until early Tuesday morning. * IMPACTS...At 19.8 feet, IT IS ESTIMATED THAT 18 STRUCTURES NEAR THE BAYOU WILL BE FLOODED. * ADDITIONAL DETAILS... - At 11:15 AM CDT Friday the stage was 17.8 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 11:15 AM CDT Friday was 17.8 feet. - Forecast...The river is expected to rise to a crest of 18.0 feet this evening. It will then fall below flood stage Monday evening. - Flood stage is 16.0 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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