Weather Alert in Kansas
Flash Flood Warning issued August 28 at 6:27AM CDT until August 28 at 10:30AM CDT by NWS Wichita KS
AREAS AFFECTED: Chautauqua, KS; Montgomery, KS
DESCRIPTION: FFWICT The National Weather Service in Wichita has issued a * Flash Flood Warning for... Northeastern Chautauqua County in southeastern Kansas... Southern Montgomery County in southeastern Kansas... * Until 1030 AM CDT. * At 627 AM CDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Up to 5 inches of rain have fallen. Additional rainfall amounts up to 2 inches are possible in the warned area through this morning. Flash flooding is possible. HAZARD...Life threatening flash flooding. Thunderstorms producing flash flooding. SOURCE...Radar. IMPACT...Life threatening flash flooding of creeks and streams, urban areas, highways, streets and underpasses. * Some locations that may experience flash flooding include... Coffeyville, Independence, Caney, Dearing, Elk City, Tyro, Havana, Bolton, Independence Airport, Elk City Lake, Elk City State Park 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 is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - 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
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