Weather Alert in Ohio
Flood Warning issued March 27 at 11:59AM EDT until April 1 at 2:00AM EDT by NWS Pittsburgh PA
AREAS AFFECTED: Coshocton, OH
DESCRIPTION: ...The National Weather Service in Pittsburgh has issued a Flood Warning 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 this evening to late Tuesday night. * 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. At 18.0 feet, Moderate flooding occurs along County Route 1A and lower areas along Route 16 south. Widespread flooding occurs from the Lake Park area south to near the intersection of Routes 83 and 36. Homes around North Water Street in Coshocton floods. * ADDITIONAL DETAILS... - At 11:00 AM EDT Friday the stage was 12.6 feet. - Bankfull stage is 13.0 feet. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 17.0 feet tomorrow evening. It will then fall below flood stage Tuesday evening. - Flood stage is 15.0 feet. - Flood History...This crest compares to a previous crest of 16.9 feet on 02/13/2019. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at weather.gov/pbz. The next statement will be issued late tonight at midnight EDT.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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