Weather Alert in Ohio
Flood Warning issued May 31 at 3:30AM EDT until May 31 at 5:15AM EDT by NWS Charleston WV
AREAS AFFECTED: Washington, OH; Tyler, WV
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Portions of southeast Ohio, including the following county, Washington and northern West Virginia, including the following county, Tyler. * WHEN...Until 515 AM EDT. * IMPACTS...Flooding of rivers, creeks, streams is imminent or occurring. * ADDITIONAL DETAILS... - At 327 AM EDT, Automated gauges indicated water issues on smaller rivers and larger creeks and streams from previous rainfall including Middle Island Creek, and the Little Muskingum River. - Some locations that will experience flooding include... Marietta, Middlebourne, Williamstown, Paden City, Sistersville, Matamoras, Lowell, Macksburg, Friendly, Lower Salem, New Matamoras, Devola and Lima. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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
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