Weather Alert in Ohio
Severe Thunderstorm Warning issued March 31 at 8:43PM EDT until March 31 at 9:30PM EDT by NWS Cleveland OH
AREAS AFFECTED: Ashland, OH; Crawford, OH; Huron, OH; Marion, OH; Morrow, OH; Richland, OH; Seneca, OH; Wyandot, OH
DESCRIPTION: SVRCLE The National Weather Service in Cleveland has issued a * Severe Thunderstorm Warning for... Southwestern Huron County in north central Ohio... Richland County in north central Ohio... Southeastern Seneca County in northwestern Ohio... Northeastern Marion County in north central Ohio... Northwestern Ashland County in north central Ohio... Eastern Wyandot County in northwestern Ohio... Northeastern Morrow County in north central Ohio... Crawford County in north central Ohio... * Until 930 PM EDT. * At 843 PM EDT, a severe thunderstorm was located 7 miles southeast of Sycamore, or 7 miles northwest of Bucyrus, moving east at 60 mph. HAZARD...60 mph wind gusts. SOURCE...Radar indicated. IMPACT...Expect damage to trees and power lines. * Locations impacted include... Mansfield, Ashland, Bucyrus, Upper Sandusky, Galion, Shelby, Ontario, Lexington, Crestline, Bellville, Plymouth, New Washington, Sycamore, Savannah, Chatfield, Butler, Benton, Nevada, Lucas, and Bailey Lakes.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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