Weather Alert in Missouri
Flood Warning issued April 2 at 4:12AM CDT until April 5 at 12:00AM CDT by NWS Springfield MO
AREAS AFFECTED: Vernon, MO
DESCRIPTION: ...The National Weather Service in Springfield MO has issued a Flood Warning for the following rivers in Kansas...Missouri... Little Osage River at Fulton affecting Bourbon County. Little Osage River near Horton affecting Vernon County. For the Little Osage River...including Fulton, Horton...Moderate flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Little Osage River near Horton. * WHEN...Until early Sunday morning. * IMPACTS...At 45.0 feet, moderate flooding occurs at the gage site. Low lying areas along Route D near Stotesbury flood. * ADDITIONAL DETAILS... - At 3:45 AM CDT Thursday the stage was 39.3 feet. - Bankfull stage is 41.0 feet. - Forecast...The river is expected to rise above flood stage this morning to a crest of 43.9 feet early tomorrow afternoon. It will then fall below flood stage Saturday evening. - Flood stage is 41.0 feet. - Flood History...This crest compares to a previous crest of 44.0 feet on 04/20/2013. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Many flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued late tonight at 415 AM CDT.
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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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