Weather Alert in Kansas
Flood Warning issued September 10 at 6:49PM CDT until September 13 at 3:00PM CDT by NWS Topeka KS
AREAS AFFECTED: Ottawa, KS
DESCRIPTION: ...The Flood Warning continues for the following rivers in Kansas... Salt Creek near Ada affecting Ottawa County. * WHAT...Moderate flooding is occurring and moderate flooding is forecast. This approaches the flood of record. * WHERE...Salt Creek near Ada. * WHEN...Until Saturday afternoon. * IMPACTS...At 18.0 feet, Minor low land flooding along the Salt Creek. At 20.0 feet, 50th Road just south of the bridge over the Salt Creek floods. At 20.2 feet, Deck of 50th Road bridge over the Salt Creek floods. At 21.0 feet, Flood waters are over one half mile wide over cultivated farm land 3 miles east southeast of the town of Ada. * ADDITIONAL DETAILS... - At 5:45 PM CDT Wednesday the stage was 21.7 feet. - Forecast...The river is expected to fall below flood stage early Saturday morning and continue falling to 14.5 feet early Monday afternoon. - Flood stage is 18.0 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 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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