Weather Alert in Ohio
Flood Warning issued May 5 at 10:30AM EDT until May 6 at 11:00AM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Tuscarawas, OH
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Ohio... Stillwater Creek At Uhrichsville affecting Tuscarawas County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Stillwater Creek at Uhrichsville. * WHEN...Until Tuesday morning. * IMPACTS...At 10.0 feet, Stillwater Creek comes out of its banks in several locations resulting in overflowing in poor drainage areas. Minor flooding of low lying areas begins. * ADDITIONAL DETAILS... - At 10:00 AM EDT Monday the stage was 10.1 feet. - Bankfull stage is 7.6 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 10:00 AM EDT Monday was 10.1 feet. - Forecast...The river is expected to rise to a crest of 10.2 feet this afternoon. It will then fall below flood stage late tonight. - Flood stage is 10.0 feet. - Flood History...This crest compares to a previous crest of 10.3 feet on 09/10/2004. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at weather.gov/pbz. The next statement will be issued this evening at 1030 PM EDT.
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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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