Weather Alert in Missouri
Flood Warning issued May 1 at 8:08AM CDT until May 2 at 8:20AM CDT by NWS Springfield MO
AREAS AFFECTED: Cedar, MO
DESCRIPTION: ...The Flood Warning continues for the following rivers in Missouri... Sac River near Caplinger Mills affecting Cedar County. * WHAT...Minor flooding is occurring. * WHERE...Sac River near Caplinger Mills. * WHEN...Until tomorrow morning. * IMPACTS...At 16.0 feet, minor Flooding occurs at the gage site. The campground at Caplinger Mills floods. * ADDITIONAL DETAILS... - At 7:45 AM CDT Thursday the stage was 16.1 feet. - Bankfull stage is 16.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:45 AM CDT Thursday was 16.4 feet. - Forecast...The river is expected to fall below flood stage this morning and continue falling to 10.1 feet Tuesday morning. - Flood stage is 16.0 feet. - Flood History...This crest compares to a previous crest of 16.1 feet on 07/04/1976. - 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 Friday morning at 815 AM 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
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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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