Weather Alert in Kansas

Recent Locations: Narka, KS  

Flood Warning issued June 3 at 5:08PM CDT until June 3 at 9:15PM CDT by NWS Wichita KS

AREAS AFFECTED: Butler, KS; Chautauqua, KS; Cowley, KS; Elk, KS

DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Portions of South Central and Southeast Kansas, including the following counties, in South Central Kansas, Butler and Cowley. In Southeast Kansas, Chautauqua and Elk. * WHEN...Until 915 PM CDT. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. * ADDITIONAL DETAILS... - At 508 PM CDT, Doppler radar indicated heavy rain due to thunderstorms. Flooding is ongoing or expected to begin shortly in the warned area. - Some locations that will experience flooding include... Sedan, Howard, Cedar Vale, Moline, Longton, Dexter, Grenola, Peru, Latham, Chautauqua, Elk Falls, Cambridge, Niotaze and Hale.

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.

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Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

Next Topic: Sleet

Weather Topic: What is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

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