Weather Alert in Texas
Flood Warning issued May 10 at 8:43PM CDT by NWS Shreveport LA
AREAS AFFECTED: Gregg, TX; Smith, TX; Upshur, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Sabine River Near Gladewater affecting Smith, Gregg and Upshur Counties. For the Sabine River...including Mineola, Hawkins, Gladewater, Longview, Beckville, Logansport...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Sabine River near Gladewater. * WHEN...Until further notice. * IMPACTS...At 32.0 feet, Lowland flooding will continue to slowly decrease over the next several days. * ADDITIONAL DETAILS... - At 8:15 PM CDT Saturday the stage was 25.8 feet. - Bankfull stage is 25.0 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight and continue rising to a crest of 30.9 feet Thursday morning. - Flood stage is 26.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Sunday evening at 845 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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