Weather Alert in Louisiana
Flood Warning issued May 12 at 9:58AM CDT until May 15 at 7:00AM CDT by NWS Lake Charles LA
AREAS AFFECTED: Calcasieu, LA
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Louisiana... Calcasieu River Near Kinder Bayou Nezpique Near Basile Bayou Vermilion Near Carencro ...The Flood Warning continues for the following rivers in Louisiana...Texas... Calcasieu River Near Salt Water Barrier Atchafalaya River At Morgan City Calcasieu River near White Oak Park Mermentau River Near Mermentau Vermilion River At Lafayette, Surrey Street Gage Sabine River Near Deweyville ...The Flood Warning is cancelled for the following rivers in Louisiana... West Fork of The Calcasieu River At Sam Houston Jones SP Calcasieu River Near Glenmora Additional information is available at www.weather.gov. * WHAT...Minor flooding is forecast. * WHERE...Calcasieu River near Salt Water Barrier. * WHEN...Until Thursday morning. * ADDITIONAL DETAILS... - At 8:00 AM CDT Monday the stage was 2.2 feet. - Forecast...The river will oscillate around flood stage with a maximum value of 4.0 feet this afternoon. - Flood stage is 4.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - 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
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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