Table of ContentsIntroductionDissection of the 1999 Oklahoma Tornado DisasterConclusionIntroductionNatural hazard refers to catastrophic events or phenomena of atmospheric, geological, and hydrological problems that can cause deaths, property damage, social and environmental disruption and can indirectly cause social grievances and resource shortages. These include earthquakes, tornadoes, volcanic eruptions, tsunamis, floods, typhoons and thunderstorms, hurricane outbreaks, etc. It usually happens randomly, that is, it is probabilistic and its result is usually given taking into account the direct and indirect effects it causes. Say no to plagiarism. Get a tailor-made essay on “Why Violent Video Games Should Not Be Banned”? Get the original essay Tornadoes are violent, rotating columns of air with speeds of more than 200 miles per hour that extend from thunderstorms to the ground and are likely to occur anywhere and at any time. with enormous energies that can destroy structures, overturn vehicles, and create deadly flying debris, which has devastating effects on physical and human geography, as evidenced in Oklahoma in 1999. This hazard formation occurs in the following sequence: Supercells or a large thunderstorm occur in a cumulonimbus. cloud. A change in wind direction and speed at high altitude causes the air to swirl horizontally. Air rising from the ground pushes the swirling air and overturns it, forming a funnel of swirling air that begins to draw in more warm air from the ground which then elongates and extends toward the ground to inform of a very strong wind which is called a tornado. This is likely to occur anywhere and at any time, but most prevalent in the temperate zone and in the afternoon when thunderstorms are more widespread. This tornado registered F-5 strength on the Fujista Tornado Scale and occurred for nearly an hour and 38 minutes, extending 38 miles from Chickasha through southern Oklahoma City and the suburbs from Bridge Creek, Newcastle, Moore, Midwest City and Del City. Having started as a low tornado in range, this disaster later intensified and spread to other areas, primarily affecting counties in Texas and Oklahoma. Initially, meteorologists observed that the atmosphere was unstable and that wind changes, based on a special weather balloon, indicated a high possibility of a tornado developing, leading to the possibility of a tornado being declared elevated by the Storm Prediction Center (SPC) at 4 p.m. Central Daylight Time on May 3. This led to widespread awareness through television, direct telephone calls, sirens, AM/FM radio, and National Oceanic and Atmospheric Administration (NOAA) weather radio, which showed that civil society was aware even so many feared that evacuation could lead to more devastating effects due to short time frames while others escaped via various modes such as vehicles to safer areas. However, timely warming for preparedness and special programs should take into account long tornado warning times and street-level television coverage to allow residents to make informed decisions to reduce risk by possibly sheltering or moving away from the path of the tornado. The first storms hit northwest Texas. and southwest Oklahoma before expanding northeast to Oklahoma City and Tusla. 15,.