Weather Alert in Ohio
Flood Warning issued April 1 at 10:04PM EDT until April 4 at 2:00PM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Coshocton, OH
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Ohio... Stillwater Creek At Uhrichsville affecting Tuscarawas County. Muskingum River At Coshocton affecting Coshocton County. * WHAT...Minor flooding is forecast. * WHERE...Muskingum River at Coshocton. * WHEN...From Thursday evening to Saturday afternoon. * 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 9:00 PM EDT Wednesday the stage was 13.0 feet. - Bankfull stage is 13.0 feet. - Forecast...The river is expected to rise above flood stage Thursday evening to a crest of 15.1 feet early Friday morning. It will then fall below flood stage Saturday 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 Thursday afternoon at noon EDT.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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