Weather Alert in Ohio
Severe Thunderstorm Warning issued March 22 at 10:03PM EDT until March 22 at 10:30PM EDT by NWS Wilmington OH
AREAS AFFECTED: Delaware, OH; Fairfield, OH; Franklin, OH; Madison, OH; Union, OH
DESCRIPTION: SVRILN The National Weather Service in Wilmington has issued a * Severe Thunderstorm Warning for... Franklin County in central Ohio... Northwestern Fairfield County in central Ohio... Southern Delaware County in central Ohio... Southeastern Union County in central Ohio... Northeastern Madison County in central Ohio... * Until 1030 PM EDT. * At 1003 PM EDT, a severe thunderstorm was located over Plain City, moving southeast at 50 mph. HAZARD...Half dollar size hail. SOURCE...Radar indicated. IMPACT...Minor damage to vehicles is possible. * Locations impacted include... Columbus, Dublin, Westerville, Reynoldsburg, Grove City, Delaware, Upper Arlington, Gahanna, Hilliard, Marysville, Pickerington, Worthington, Bexley, Pataskala, Powell, Canal Winchester, Groveport, Plain City, West Jefferson, and Minerva Park. This includes the following Interstates... I-70 in Ohio between mile markers 82 and 113. I-71 in Ohio between mile markers 100 and 128.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Large hail, damaging wind, and continuous cloud to ground lightning are occurring with this storm. Move indoors immediately. Lightning is one of nature's leading killers. Remember, if you can hear thunder, you are close enough to be struck by lightning. Torrential rainfall is occurring with this storm, and may lead to flash flooding. Do not drive your vehicle through flooded roadways. 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 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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