Weather Alert in Louisiana

Recent Locations: Joyce, LA  

Tornado Warning issued February 14 at 11:07PM CST until February 14 at 11:45PM CST by NWS New Orleans LA

AREAS AFFECTED: East Baton Rouge, LA; East Feliciana, LA; West Feliciana, LA

DESCRIPTION: TORLIX The National Weather Service in New Orleans has issued a * Tornado Warning for... Southeastern West Feliciana Parish in southeastern Louisiana... Southern East Feliciana Parish in southeastern Louisiana... Northern East Baton Rouge Parish in southeastern Louisiana... * Until 1145 PM CST. * At 1107 PM CST, severe thunderstorms capable of producing both tornadoes and straight line wind damage were located 7 miles northwest of Zachary, moving east at 35 mph. HAZARD...Tornado. SOURCE...Radar indicated rotation. IMPACT...Flying debris will be dangerous to those caught without shelter. Mobile homes will be damaged or destroyed. Damage to roofs, windows, and vehicles will occur. Tree damage is likely. * This dangerous storm will be near... Zachary and Slaughter around 1110 PM CST.

INSTRUCTION: TAKE COVER NOW! Move to a basement or an interior room on the lowest floor of a sturdy building. Avoid windows. If you are outdoors, in a mobile home, or in a vehicle, move to the closest substantial shelter and protect yourself from flying debris.

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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