Weather Alert in Kansas
Flood Warning issued June 5 at 1:53AM CDT until June 7 at 3:40PM CDT by NWS Wichita KS
AREAS AFFECTED: Cowley, KS
DESCRIPTION: ...The Flood Warning continues for the following rivers in Kansas... Walnut River at Winfield affecting Butler and Cowley Counties. Walnut River at Arkansas City affecting Cowley County. * WHAT...Minor flooding is forecast. * WHERE...Walnut River at Arkansas City. * WHEN...From this afternoon to Saturday afternoon. * IMPACTS...At 18.0 feet, Considerable flooding of farmland can be expected. There is considerable flooding upstream along the west bank of the Walnut River. On the east bank, the ground slopes upward so that only about a 300 foot wide strip of land would be affected. * ADDITIONAL DETAILS... - At 1:15 AM CDT Thursday the stage was 17.1 feet. - Forecast...The river is expected to rise above flood stage this afternoon to a crest of 19.5 feet tomorrow evening. It will then fall below flood stage early Saturday morning. - Flood stage is 18.0 feet.
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. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov. The next statement will be issued this afternoon at 200 PM CDT.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
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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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