Weather Alert in Louisiana
Flood Warning issued April 24 at 8:23PM CDT by NWS Lake Charles LA
AREAS AFFECTED: St. Martin, LA; St. Mary, LA
DESCRIPTION: ...The Flood Warning continues for the following rivers in Louisiana...Texas... Atchafalaya River At Morgan City Bayou Vermilion Near Carencro Vermilion River At Lafayette, Surrey Street Gage Sabine River Near Deweyville Additional information is available at www.weather.gov. * WHAT...Moderate flooding is forecast. * WHERE...Atchafalaya River at Morgan City. * WHEN...From Friday evening until further notice. * IMPACTS...At 7.0 feet, Buildings at the foot of Ann Street on the river side of the flood wall will flood as water overtops the Rio Oil Company dock. Buildings on the river side of the Berwick floodwall will flood. River traffic restrictions will be strictly enforced. In addition, backwater flooding could potentially impact portions areas around Lake Palourde and Stephensville. * ADDITIONAL DETAILS... - At 7:00 PM CDT Thursday the stage was 5.8 feet. - Forecast...The river is expected to rise above flood stage tomorrow evening and continue rising to a crest of 7.0 feet Saturday, May 03. - Flood stage is 6.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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