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Joplin tornado case study

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From: Jaime S.
Added: 22.04.2021
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It was part of a larger late-May tornado outbreak and reached a maximum width of nearly one mile 1. This particular tornado was unusual in that it intensified in strength and grew larger in size at a very fast rate. The tornado tracked eastward across the city, and then continued eastward across Interstate 44 into rural portions of Jasper and Newton counties. It was the third tornado to strike Joplin since May It was the deadliest tornado to strike the U.

How a Midwestern community is healing itself

How Tornadoes Affect People - Words | Internet Public Library

On May 22, , a catastrophic tornado cut a mile path of destruction through Joplin, Mo. It was an overwhelming situation for the community. Residents found themselves displaced from the homes they had lived in for years, many now residing in one of several FEMA trailer parks. Seeing the need to get people back into their houses, Rebuild Joplin, a local nonprofit group, was formed.

Tornado Case Study Of Tornado

Daily 23 Today. Tornado Central. The EF-5 tornado was powerful enough to wrap this heavy-duty hauling vehicle around a tree. Image: weather. The study by the American Society of Civil Engineers found that more than 83 percent of the damage on May 22, , was caused by winds of mph or less, which is equal to the maximum wind speed of an EF2 tornado, and that about 13 percent of the damage was caused by winds of mph, consistent with an EF3 tornado.
Science and Engineering Practices: Analyzing and interpreting data, defining an engineering problem, considering solutions. Crosscutting Concepts: Cause and Effect, Stability and Change, Influence of Science Engineering and Technology on Society and the Natural World All human activity draws on natural resources and has both short and long-term consequences, positive as well as negative, for the health of people and the natural environment. Tornadoes, also called twisters, are columns of air rotating dangerously fast. The air is in motion because of the difference in pressure between the center of tornado very low pressure and the outer edge of the tornado high pressure.

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