Weather Alert in Ohio
Flood Advisory issued March 5 at 1:34PM EST until March 5 at 6:30PM EST by NWS Wilmington OH
AREAS AFFECTED: Clinton, OH; Fairfield, OH; Fayette, OH; Highland, OH; Hocking, OH; Pickaway, OH; Ross, OH
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...The following counties, in central Ohio, Fairfield, Fayette, Hocking and Pickaway. In south central Ohio, Highland and Ross. In southwest Ohio, Clinton. * WHEN...Until 630 PM EST. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 134 PM EST, local law enforcement reported minor flooding in the advisory area. Between 1.5 and 2.5 inches of rain have fallen. Additional rainfall amounts up to 0.5 inches are possible. - Some locations that may experience flooding include... Lancaster, Chillicothe, Washington Court House, Circleville, Wilmington, Logan, Greenfield, Nelsonville, Ashville, Sabina, South Bloomfield, Bremen, Leesburg, New Vienna, Kingston, Williamsport, New Holland, Logan Elm Village, North Folk Village and Hocking Hills State Park.
INSTRUCTION: Be aware of your surroundings and do not drive on flooded roads. To report flooding, go to our website at weather.gov/iln and submit your report via social media, when you can do so safely.
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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