Weather Alert in Ohio
Severe Thunderstorm Warning issued April 29 at 2:26PM EDT until April 29 at 3:15PM EDT by NWS Wilmington OH
AREAS AFFECTED: Clinton, OH; Fayette, OH; Pickaway, OH; Ross, OH
DESCRIPTION: SVRILN The National Weather Service in Wilmington has issued a * Severe Thunderstorm Warning for... Southern Fayette County in central Ohio... Northeastern Clinton County in southwestern Ohio... Southern Pickaway County in central Ohio... Northern Ross County in south central Ohio... * Until 315 PM EDT. * At 226 PM EDT, a severe thunderstorm was located over Sabina, moving east at 45 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to trees and power lines. * Locations impacted include... Deer Creek Lake, East Ringgold, New Vienna, Good Hope, Kingston, Austin, Sabina, Circleville, Lees Creek, Rock Mills, Williamsport, New Holland, Washington Court House, New Martinsburg, Pancoastburg, Plano, Aw Marion State Park, Clarksburg, Staunton, and Andersonville.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. To report severe weather, 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 Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
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
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