Weather Alert in Illinois
Flood Warning issued April 18 at 11:33PM EDT until April 20 at 6:00AM EDT by NWS Indianapolis IN
AREAS AFFECTED: Edwards, IL; Gallatin, IL; Wabash, IL; White, IL; Gibson, IN; Knox, IN; Posey, IN
DESCRIPTION: ...The Flood Warning continues for the following rivers in Illinois...Indiana... Wabash River at Mount Carmel. .Minor flooding will continue on the Wabash River at Mount Carmel through late Saturday. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Wabash River at Mount Carmel. * WHEN...Until Sunday morning. * IMPACTS...At 22.9 feet, Water begins to flow over River Road just north of Fifth Street in the Mount Carmel area. * ADDITIONAL DETAILS... - At 11:00 PM EDT Friday /10:00 PM CDT Friday/ the stage was 22.6 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 11:00 PM EDT Friday /10:00 PM CDT Friday/ was 25.3 feet. - Forecast...The river is expected to fall below flood stage tomorrow evening and continue falling and remain below flood stage. - Flood stage is 19.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Caution is urged when walking near riverbanks. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov/ind. The next statement should be issued Saturday afternoon by around 200 PM EDT /100 PM 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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