Weather Alert in Louisiana
Severe Thunderstorm Warning issued February 14 at 11:27PM CST until February 14 at 11:45PM CST by NWS Lake Charles LA
AREAS AFFECTED: Iberia, LA; St. Martin, LA; St. Mary, LA
DESCRIPTION: At 1127 PM CST, severe thunderstorms were located along a line extending from Port Allen to 12 miles south of Cypremort Point, moving east at 45 mph. HAZARD...60 mph wind gusts. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. Locations impacted include... New Iberia, Catahoula, Franklin, Jeanerette, Cypremort Point, Avery Island, Baldwin, Loreauville, Butte La Rose, Glencoe, Lydia, Sorrel, Cote Blanche Island, Lake Fausse Pointe, Charenton, and Weeks Island.
INSTRUCTION: A Tornado Watch remains in effect until 200 AM CST for south central and southwestern Louisiana. Remain alert for a possible tornado! Tornadoes can develop quickly from severe thunderstorms. If you spot a tornado go at once into a small central room in a sturdy structure. For your protection move to an interior room on the lowest floor of a building.
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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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