Weather Alert in Missouri

Recent Locations: Licking, MO  

Flood Warning issued June 4 at 4:31AM CDT until June 7 at 8:20AM CDT by NWS Springfield MO

AREAS AFFECTED: Vernon, MO

DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas...Missouri... Little Osage River at Fulton affecting Bourbon County. Little Osage River near Horton affecting Vernon County. ...The Flood Warning continues for the following rivers in Missouri... Marmaton River near Nevada affecting Vernon County. For the Little Osage River...including Fulton, Horton...Minor flooding is forecast. For the Marmaton River...including Nevada...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Marmaton River near Nevada. * WHEN...From this morning to Saturday morning. * IMPACTS...At 22.0 feet, flood waters impact the county road west of Nevada at the gage site. * ADDITIONAL DETAILS... - At 3:45 AM CDT Wednesday the stage was 15.4 feet. - Bankfull stage is 20.0 feet. - Forecast...The river is expected to rise above flood stage late this morning to a crest of 22.2 feet tomorrow morning. It will then fall below flood stage Friday morning. - Flood stage is 20.0 feet. - Flood History...This crest compares to a previous crest of 22.2 feet on 04/28/2013. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Many flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued late tonight at 445 AM CDT.

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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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