Weather Alert in Kansas
Flood Warning issued August 28 at 8:16PM CDT until August 30 at 2:01AM CDT by NWS Wichita KS
AREAS AFFECTED: Cowley, KS; Sumner, KS
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas... Slate Creek At Wellington affecting Cowley and Sumner Counties. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Slate Creek at Wellington. * WHEN...Until early Saturday morning. * IMPACTS...At 20.0 feet, Flood waters cover several low lying spots along Seneca Road between 40th and 60th Street just southeast of Wellington. Woods Park within the city floods. Slate Creek comes to roadway's edge at mile marker 15 on the the Kansas Turnpike. * ADDITIONAL DETAILS... - At 8:01 PM CDT Thursday the stage was 21.3 feet. - Forecast...The river is expected to rise to a crest of 21.4 feet just after midnight tonight. It will then fall below flood stage early tomorrow afternoon. - Flood stage is 19.0 feet.
INSTRUCTION: Do not drive into flooded areas or go around barricades. Nearly two feet of water will carry most vehicles away. Turn around, don't drown. Additional information is available at www.weather.gov. The next statement will be issued Friday 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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