Weather Alert in Ohio
Flood Warning issued April 2 at 11:48AM EDT until April 5 at 8:00AM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Coshocton, OH
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Ohio... Muskingum River At Coshocton affecting Coshocton County. * WHAT...Minor flooding is forecast. * WHERE...Muskingum River at Coshocton. * WHEN...From late tonight to Sunday morning. * IMPACTS...At 13.0 feet, Water reaches low lying areas between Tuscarawas and Walhonding Rivers just upstream of the confluence of the two rivers. At 15.0 feet, Low areas are flooded and water reaches a few homes along Route 16 south of Coshocton and along County Route 1A north of Coshocton. At 16.0 feet, Flood waters begin to affect the Lake Park area along the Walhonding River and begins backwater flooding along Mill Creek north of Lake Park and along Route 83. Flood waters will begin to enter yards in low-lying areas along County Route 1A. * ADDITIONAL DETAILS... - At 11:00 AM EDT Thursday the stage was 13.8 feet. - Bankfull stage is 13.0 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight to a crest of 15.1 feet tomorrow morning. It will then fall below flood stage early Sunday morning. - Flood stage is 15.0 feet. - Flood History...This crest compares to a previous crest of 15.1 feet on 03/05/1993. - 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 1000 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.
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