Weather Alert in Arkansas
Flood Advisory issued July 4 at 8:59AM CDT until July 14 at 1:00PM CDT by NWS Jackson MS
AREAS AFFECTED: Chicot, AR; East Carroll, LA; Issaquena, MS; Washington, MS
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Mississippi...Louisiana...Arkansas... Mississippi River Near Greenville affecting Washington, Issaquena, East Carroll and Chicot Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Mississippi River near Greenville. * WHEN...Until Monday, July 14. * ADDITIONAL DETAILS... - At 8:00 AM CDT Friday the stage was 36.7 feet. - Forecast...The river is expected to rise to a crest of 36.7 feet this afternoon. It will then rise to 37.5 feet early Thursday afternoon. Additional rises are possible thereafter. - Action stage is 36.0 feet. - Flood stage is 48.0 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 Saturday morning at 830 AM CDT.
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Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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