Introduction to Tornadoes A tornado looks like a column of air or condensed funnel, which is moving anti-clockwise at high speeds with one end of the column being in contact with the ground and the other touching the heavy clouds (Galiano, 2000, p. 3). Sometimes, the vertical funnels consist of clouds of debris, dirt, objects, or dust. Conversely, tornadoes occur in various shapes and sizes including rope-like, wedge-shaped, classical, fat cylinders, and conical tornadoes. Furthermore, tornadoes can be classified into several types including supercell, waterspout, landspout, gustnado, dust devil, and firewhirls. Accordingly, a wedge-shaped tornado consists of straight edges, a non-funnel shape, and its damage path is usually wide. Moreover, its width is much bigger than its height. On the other hand, classical tornadoes consist of funnels that never touch the ground, and thus, the ground surface rises in such a way that the tornado is half funnel and half dirt or dust (Prokos, 2008, p. 10). During any form of tornado, some vital signs can be noticed such as the occurrence of a dark-green sky, dense and low-lying clouds, unusual loud sounds, and large hails. Therefore, it is advisable for one to take immediate cover upon observing these weather changes. Thus, some of the safety measures during a tornado include avoiding windows, discussing safety measures with family members, avoiding mobile homes, stopping the car if driving, avoiding trees and tall buildings, and lying flat on the ground or a ditch while protecting the head (CDC, 2007). To further understand the dynamics of tornadoes, the Bernoulli’s principle has been utilized to explain the principle behind the formation of tornadoes. Accordingly, in fluid dynamics, the principle has it that in some fluids with zero velocity (theoretical fluids displaying inviscid flow), an increase in the velocity of the fluid follows a subsequent decrease in fluid pressure or potential energy. As a result, the formation of tornadoes can be affected by Bernoulli’s principle since most tornadoes show a local vortex (the wall of the air column) flow whereby the velocity of the flow is greatest at the center of the vortex (Grazulis, 2001, p. 20). The sound made by most tornadoes involves loud roars, which resemble the sound made by freight trains, waterfalls, or jet engines. According to the Earth Systems Laboratory Study of Sound, the use of infrasonic arrays is effective in detecting tornadoes occurring in high plains several minutes before they can touch the ground. This study referred to as infrasonics involves detection of infrasonic signatures, vibrations, or disturbed waves with frequencies below the level detectable by the human ear (Galiano, 2000). Furthermore, the study shows that tornado sounds are caused by the tornado vortex winds and the interaction between airflows and the ground dust or debris. Moreover, the funnel clouds have been shown to produce whistling, buzzing, humming, and whining sounds. Tornado Variations As mentioned earlier, tornadoes occur in many shapes, sizes, and categories. For example, landspout also known as dust-tube tornado is a tornado with lesser intensity compared to supercell tornadoes, and thus, they occur for a short period. As opposed to supercell tornadoes, which involve