Weather Alert in Louisiana
Flood Advisory issued July 1 at 10:26AM CDT by NWS Jackson MS
AREAS AFFECTED: Concordia, LA; Adams, MS; Wilkinson, MS
DESCRIPTION: ...The Flood Advisory is extended for the following rivers in Mississippi...Louisiana...Arkansas... Mississippi River Near Greenville affecting Issaquena, East Carroll, Chicot and Washington Counties. Mississippi River At Natchez affecting Wilkinson, Adams and Concordia Counties. Mississippi River At Vicksburg affecting Madison, Warren, Tensas, Jefferson and Claiborne Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River at Natchez. * WHEN...Until further notice. * IMPACTS...At 47.0 feet, Water begins to enter the Carthage Point Road area south of Natchez. * ADDITIONAL DETAILS... - At 10:00 AM CDT Tuesday the stage was 46.9 feet. - Forecast...The river is expected to rise to a crest of 46.9 feet this afternoon. - Action stage is 38.0 feet. - Flood stage is 48.0 feet. - http://www.weather.gov/safety/flood
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 this evening at 1030 PM CDT.
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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
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