Weather Alert in Louisiana
Flood Advisory issued July 1 at 10:26AM CDT until July 16 at 1:00AM CDT by NWS Jackson MS
AREAS AFFECTED: Madison, LA; Tensas, LA; Claiborne, MS; Jefferson, MS; Warren, 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 Vicksburg. * WHEN...Until Wednesday, July 16. * IMPACTS...At 38.8 feet, The Vicksburg FloodWall Gate at Crawford street is closed. * ADDITIONAL DETAILS... - At 10:00 AM CDT Tuesday the stage was 38.6 feet. - Forecast...The river is expected to fall to 29.5 feet Tuesday, July 29. - Action stage is 35.0 feet. - Flood stage is 43.0 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 Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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