Weather Alert in Louisiana
Flood Warning issued May 6 at 10:45AM CDT until May 9 at 4:00PM CDT by NWS Lake Charles LA
AREAS AFFECTED: Acadia, LA; Evangeline, LA; St. Landry, LA
DESCRIPTION: ...The National Weather Service in Lake Charles LA has issued a Flood Warning for the following rivers in Louisiana... Bayou Des Cannes Near Eunice Vermilion River At Lafayette, Surrey Street Gage Additional information is available at www.weather.gov. * WHAT...Minor flooding is forecast. * WHERE...Bayou Des Cannes near Eunice. * WHEN...From late Wednesday night to Friday afternoon. * IMPACTS...At 16.0 feet, Minor flooding begins along the bayou with a few structures right along the bayou threatened. * ADDITIONAL DETAILS... - At 10:15 AM CDT Tuesday the stage was 1.4 feet. - Forecast...The river is expected to rise above flood stage early Thursday morning to a crest of 17.0 feet early Thursday afternoon. It will then fall below flood stage late Friday morning. - 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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