Weather Alert in Ohio
Special Weather Statement issued February 19 at 11:44PM EST by NWS Wilmington OH
AREAS AFFECTED: Franklin; Licking; Fairfield
DESCRIPTION: At 1143 PM EST, a strong thunderstorm was located over Canal Winchester, moving northeast at 55 mph. HAZARD...Wind gusts up to 40 mph, pea size hail, and very heavy rain. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Hail may cause minor damage to vegetation. Visibility will be poor and hydroplaning is possible. Locations impacted include... Newark, Lancaster, Pickerington, Heath, Granville, Canal Winchester, Baltimore, Buckeye Lake, Hebron, Millersport, Pleasantville, Harbor Hills, Fairfield Beach, Thornport, Granville South, Etna, Royalton, Lithopolis, Thurston, and Kirkersville. This includes I-70 in Ohio between mile markers 117 and 137. If outdoors, consider seeking shelter inside a sturdy building. Motorists should slow down and use extra caution. To report hazardous weather conditions, go to our website at weather.gov/iln and submit your report via social media, when you can do so safely.
INSTRUCTION: N/A
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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