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Tornado damage in Lorain, Ohio The Xenia, Ohio tornado from the 1974 Super Outbreak. This tornado was rated by Ted Fujita himself as an F6 , but it was retroactively downgraded to F5 [ 1 ] Tornadoes in the state of Ohio are relatively uncommon, with roughly 16 tornadoes touching down every year since 1804, the year with the first recorded event ...
In older events, the number of tornadoes officially counted is likely underestimated. Historical context: Much of the tornado activity in the American Midwestern area is relatively unknown and significantly under-reported prior to the middle of the 1800s as few people lived there to record the yearly activity.
This flood is still the flood of record for the Great Miami River watershed. The volume of water that passed through the river channel during this storm equaled the monthly flow over Niagara Falls. [3] The Great Miami River watershed covers nearly 4,000 square miles (10,000 km 2) and 115 miles (185 km) of channel that feeds into the Ohio River. [4]
The National Weather Service is surveying storm damage today to confirm whether tornadoes touched down. The Wilmington office, which covers Central Ohio, said it dispatched crews shortly after 9 ...
Thursday night, severe weather led to 20 tornado warnings across Ohio, leaving a trail of storm damage and cutting power to thousands. Severe storms and confirmed tornadoes in Mercer, Crawford and ...
A 100-year flood is a flood event that has on average a 1 in 100 chance (1% probability) of being equaled or exceeded in any given year. [1] A 100-year flood is also referred to as a 1% flood. [2] For coastal or lake flooding, a 100-year flood is generally expressed as a flood elevation or depth, and may include wave effects. For river systems ...
The National Weather Service in Cleveland on Thursday confirmed two tornadoes touched down in Lorain and Cuyahoga counties on Tuesday.
Weather map from National Weather Service On Saturday, August 18, a warm front pushed northward into Iowa and Illinois, where it became stationary . Warm, moist air pushing over the frontal boundary fueled showers and thunderstorms that moved in a west-to-east fashion, training over the same areas for hours at a time.