Weather Alert in Louisiana
Flood Warning issued May 8 at 8:22PM CDT until May 11 at 1:00PM CDT by NWS Shreveport LA
AREAS AFFECTED: De Soto, LA; Panola, TX; Shelby, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Louisiana...Texas... Sabine River At Logansport affecting De Soto, Panola and Shelby Counties. For the Sabine River...including Mineola, Hawkins, Gladewater, Longview, Beckville, Logansport...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Sabine River at Logansport. * WHEN...Until Sunday afternoon. * IMPACTS...At 28.0 feet, Expect lowland flooding problems of the heavily wooded floodplain to continue for several days. * ADDITIONAL DETAILS... - At 7:45 PM CDT Thursday the stage was 27.6 feet. - Bankfull stage is 27.0 feet. - Forecast...The river is expected to rise above flood stage early Saturday morning to a crest of 28.1 feet Saturday morning. It will then fall below flood stage Saturday evening. - Flood stage is 28.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Friday evening at 830 PM 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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