Weather Alert in Kansas

Recent Locations: Narka, KS  

Flood Warning issued June 3 at 4:16PM CDT until June 6 at 1:33PM CDT by NWS Topeka KS

AREAS AFFECTED: Franklin, KS

DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas... Pottawatomie Creek near Garnett affecting Anderson County. Marais Des Cygnes River near Quenemo affecting Osage and Franklin Counties. Marais Des Cygnes River above Reading affecting Lyon and Osage Counties. Pottawatomie Creek at Lane affecting Franklin County. Marais Des Cygnes River at Ottawa affecting Franklin County. * WHAT...Minor flooding is forecast. * WHERE...Marais Des Cygnes River at Ottawa. * WHEN...From late tonight to early Friday afternoon. * 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 3:30 PM CDT Tuesday the stage was 14.7 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 32.9 feet Thursday morning. It will then fall below flood stage early Friday morning. - 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 is Graupel?

Home - Education - Precipitation - Graupel

Graupel Next Topic: Hail

Graupel is a form of precipitation that is created by atmospheric conditions which cause supercooled water droplets to contact snow crystals and freeze to their surface.

Sometimes known as soft hail or snow pellets, graupel is delicate and easily destroyed by touch. Whereas hail usually falls during severe weather, graupel doesn't require such conditions to form, and can form in mild precipitation similar to situations which produce snowfall.

Next Topic: Hail

Weather Topic: What are Hole Punch Clouds?

Home - Education - Cloud Types - Hole Punch Clouds

Hole Punch Clouds Next Topic: Mammatus Clouds

A hole punch cloud is an unusual occurrence when a disk-shaped hole appears in a cirrostratus, cirrocumulus, or altocumulus cloud.

When part of the cloud forms ice crystals, water droplets in the surrounding area of the cloud evaporate. The effect of this process produces a large elliptical gap in the cloud. The hole punch cloud formation is rare, but it is not specific to any geographic area.

Other names which have been used to describe this phenomena include fallstreak hole, skypunch, and cloud hole.

Next Topic: Mammatus Clouds

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