Weather Alert in Louisiana
Flood Advisory issued June 19 at 9:41PM CDT until July 5 at 7:00PM CDT by NWS Jackson MS
AREAS AFFECTED: Madison, LA; Tensas, LA; Claiborne, MS; Jefferson, MS; Warren, MS
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Mississippi...Louisiana...Arkansas... Mississippi River Near Greenville affecting Washington, East Carroll, Issaquena and Chicot Counties. Mississippi River At Natchez affecting Adams, Wilkinson and Concordia Counties. Mississippi River At Vicksburg affecting Madison, Jefferson, Warren, Tensas and Claiborne Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River at Vicksburg. * WHEN...Until Saturday, July 05. * IMPACTS...At 39.5 feet, The Long Lake Road to Eagle Lake Road becomes impassable about 1 mile north of the Long Lake Community. * ADDITIONAL DETAILS... - At 9:00 PM CDT Thursday the stage was 38.9 feet. - Forecast...The river is expected to rise to a crest of 39.2 feet Saturday, June 28. - Action stage is 35.0 feet. - Flood stage is 43.0 feet.
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. Additional information is available at www.water.noaa.gov/wfo/jan The next statement will be issued Friday morning at 1100 AM CDT.
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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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