Weather Alert in Kansas

Recent Locations: Coolidge, KS  
Current Alerts for Coolidge, KS: Severe Thunderstorm Watch

Flood Warning issued June 3 at 8:13PM CDT until June 6 at 5:51AM CDT by NWS Topeka KS

AREAS AFFECTED: Franklin, KS

DESCRIPTION: ...The Flood Warning continues for the following rivers in Kansas... Pottawatomie Creek at Lane affecting Franklin County. Pottawatomie Creek near Garnett affecting Anderson County. Salt Creek near Lyndon affecting Osage County. Marais Des Cygnes River near Quenemo affecting Osage and Franklin Counties. Marais Des Cygnes River at Ottawa affecting Franklin County. ...The Flood Warning is extended for the following rivers in Kansas... Marais Des Cygnes River above Reading affecting Lyon and Osage Counties. * WHAT...Minor flooding is forecast. * WHERE...Marais Des Cygnes River at Ottawa. * WHEN...From late tonight to early Friday morning. * IMPACTS...At 30.0 feet, Neosho Road east of Ottawa floods. At 31.0 feet, Lowland areas near the river continue to flood. * ADDITIONAL DETAILS... - At 7:30 PM CDT Tuesday the stage was 23.5 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 32.1 feet early Thursday morning. It will then fall below flood stage Thursday afternoon. - Flood stage is 30.0 feet.

INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. This product along with additional weather and stream information is available at www.weather.gov/top/.

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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

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

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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