Weather Alert in Oklahoma
Flood Warning issued April 28 at 8:02PM CDT until April 30 at 3:20AM CDT by NWS Norman OK
AREAS AFFECTED: Cotton, OK
DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Deep Red Creek near Randlett affecting Cotton County. * WHAT...Moderate flooding is occurring and moderate flooding is forecast. * WHERE...Deep Red Creek near Randlett. * WHEN...Until early Wednesday morning. * IMPACTS...At 24.0 feet, Valley-wide flooding of croplands... pastures... and local roads occurs and is accompanied by flood depths up to 4 feet with swift currents. * ADDITIONAL DETAILS... - At 7:30 PM CDT Monday the stage was 24.0 feet. - Bankfull stage is 20.0 feet. - Forecast...The Deep Red Creek is expected to fall below flood stage late tomorrow evening and continue falling. - Flood stage is 20.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov.
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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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