Weather Alert in Texas
Flood Advisory issued July 9 at 5:50PM CDT until July 9 at 9:00PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Ellis, TX; Hill, TX
DESCRIPTION: * WHAT...Urban and small stream flooding caused by excessive rainfall is expected. * WHERE...Portions of central and north central Texas, including the following counties, in central Texas, Hill. In north central Texas, Ellis. * WHEN...Until 900 PM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - Doppler radar indicated heavy rain due to thunderstorms. This will likely cause urban and small stream flooding. Low lying and/or poor drainage areas will experience minor flooding in the advisory area. - Some locations that will experience flooding include... Waxahachie, Ennis, Hillsboro, Whitney, Palmer, Italy, Itasca, Maypearl, Bardwell, Alma, Bynum, Carl's Corner, Aquilla Lake, Bardwell Lake, Lake Whitney State Park, Lake Whitney, Garrett, Milford, Abbott and Malone.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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