Weather Alert in Kansas
Flood Warning issued June 3 at 4:10PM CDT until June 5 at 1:21AM CDT by NWS Topeka KS
AREAS AFFECTED: Coffey, KS
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas... Salt Creek near Lyndon affecting Osage County. Neosho River Near Neosho Rapids affecting Lyon County. ...The Flood Warning continues for the following rivers in Kansas... Neosho River at Leroy affecting Coffey County. * WHAT...Moderate flooding is forecast. * WHERE...Neosho River at Leroy. * WHEN...From this evening to early Thursday morning. * IMPACTS...At 21.0 feet, At this stage the river is at bankfull and minor overflows begin and the road to Moody begins to flood. At 23.0 feet, Significant overflows begin and about 100 acres of land nearby are inundated. The road under the railroad viaduct on the right bank floods. At 27.0 feet, The Missouri, Pacific and the Missouri, Kansas and Texas Railroad tracks overflow. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 25.0 feet just after midnight tonight. It will then fall below flood stage tomorrow morning. - Flood stage is 23.0 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 Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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