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Eassays about tornados
3 aspects of tornadoes
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The weather condition I decided to focus on is tornados partly because they terrify me, and I wanted to learn as much as possible to see if it would lessen my fear of them. It did not.
Tornados are the most violent weather systems, and most of them have a very short life span. Tornados are rotating column of air in contact with the ground that are usually produced by a severe thunder storm. Often funnel shaped tornados come in all shapes and sizes. Funnel clouds form in response to the steep air pressure rise directed from the tornados outer most edge toward the center. Humid air pressure swells and cools as it is drawn inward towards the center of the system. Cooling of air to below its dew point causes water vapor to condense into cloud
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droplets. If the air is dry, a funnel cloud may or may not form. The United States in one of the few places globally where weather conditions and terrain are perfect to start a tornado. Although that take all over the U.S and Canada most occur in tornado valley. Some tornados consist of two or more minor vortices that orbit each other or about a common center within a massive tornado. Multi-vortex tornados are the most destructive of all tornados, tornados are rated by their intensity and wind speed and miles per hour. Light to incredible, light tornados right from 65-85 miles per hour and incredible is less than 200 Most strong to violent tornados are made by high convective system known as a supercell thunderstorm, supercells are very energetic with updraft speeds reaching at times 150 mph.
Tornado growth in a supercell begins with an interaction between the updraft and the larger-scale horizontal wind. Within tornadic supercell, the horizontal wind exhibits strong vertical shear in both speed and direction, that is, wind strengths and veers with altitude, from south or southeast at the surface to southwest or west aloft. Tornado development requires a special mixture of atmospheric conditions and terrain, so tornados are most frequent in spring over the central United States. Threats of tornados are extremely high winds a powerful updraft, lesser vortices and an abrupt drop in air …show more content…
pressure. There are several different types of tornados waterspouts, dust devils, fire whirls and steam devils.
A waterspout is an intense columnar vortex that occurs over a body of water. They are connected to a towering cumuliform cloud or a cumulonimbus cloud. It is a non-supercell tornado over water. A dust devil is a strong, will-formed and relatively long lived whirlwind ranging from small to large. The primary vertical motion is upward, dust devil are usually harmless but can on rare occasions grow large enough to pose a threat to both people and property. Wiki A fire whirl is a whirlwind induced by fire and often made up of flame or ash. Fire whirls may occur with intense rising heat and turbulent wind conditions combine to form whirling eddies of air. These eddies can contract into a tornado structures that suck in burning debris and combustible gases. A steam devil is a small weak whirlwind over water or sometimes wet land that has a drawn fog into the vortex making it
visible. The National Weather Service confirmed an EF1 tornado touched down during Thursday’s outbreak of severe weather. According to the NWS, the tornado hit about 3.5 miles southeast of Lafayette at Wabash National Trailers. The tornado destroyed a guard shack and caused a car to roll over. A construction trailer was damaged and nearly rolled over, the NWS said. The tornado touched down around 4:40 p.m. and had an estimated wind speed of 100 mph. There were no injuries associated with the tornado. Storm chasers in Wingate, located in Montgomery County south of Tippecanoe County, captured video of the storm as it rolled through Thursday. Tornadoes form under a certain set of weather conditions in which three very different types of air come together in a certain way. Near the ground lies a layer of warm and humid air, along with strong south winds. Colder air and strong west or southwest winds lie in the upper atmosphere. Temperature and moisture differences between the surface and the upper levels create what we call instability. A necessary ingredient for tornado formation the change in wind speed and direction with height is known as wind shear. This wind shear is linked to the eventual development of rotation from which a tornado may form.
Although the tornado of 10 June 1938 has been known about, at least anecdotally, within the scientific community since it was brought to light in 1939 by Metro-Goldwyn-Mayer, this potentially rich source of historic information has lain fallow. It is within this rich field of mobile, American thinking that we undertake this effort. A team of scientists with courage, brains, and even heart brought the resources to bear on the challenge.
Many scientists often find themselves wondering if the tri-state tornado was really a single massive tornado or if it was part of a family of tornadoes that continuously evolve from one supercell to another. Only one factor stands in the way of this theory and that is a cyclical supercell usually has breaks in its destructive path. The tri-state tornado's path of damage appeared to be continuous despite two slight decreases in the destruction. One of which was near the onset of the storm, and one near the demise. No matter which is believed, one thing is for certain, and that is a storm like the tri-state tornado could very well happen again, but there is no telling when or where it may occur.
Water spouts have happen in the Pacific oceans in Huntington Beach where an intense funnel-shaped cloud vortex happens over a body of water. This vortex is a non-supercell form tornado over water.(water spouts definition). During a water spouts you can see dark clouds over the ocean.
According to Webster’s Dictionary, a tornado is a rotating column of air accompanied by a funnel shaped downward extension of a cumulonimbus cloud and having a vortex several hundred yards in diameter whirling destructively at speeds of up to three hundred miles per hour. There are six classifications of tornadoes, which are measured on what is known as the Fujita Scale. These tornadoes range from an F0 to an F5, which is the most devastating of all. Abnormal warm, humid, and oppressive weather usually precede the formation of a tornado. Records of American tornadoes date back to 1804 and have been known to occur in every state of the United States.
On May 20th, 2013 a EF 5 tornado hit Moore, Oklahoma and surrounding towns, with a path as wide as 1.3 miles wide (2.1 km) and had a wind speed, estimated at its peak, of 210 miles per hour (340 km/h). Killing 24 people, and injuring 377, this was one of the United States worst tornadoes in the past few years, along side the Joplin, Missouri tornado, in 2011. One of Mother Nature’s most dangerous and still very mysterious phenomenons averages about 1,200 reported each year, resulting in 80 deaths and injuring 1500. With very little known about them, especially whether or not they will form is one of the questions that plague meteorologist to this very day. What causes tornadoes, how does the tilt and gravity of the earth affect the winds to produce a tornado, and what will the future hold about our understanding of tornadoes?
Tornadoes form from wind shears. Wind shears form from warm air that is found at ground level; when it’s raised, the updraft meets a down draft of cooler air that is moved in the opposite direction of the warm air. When both are pushed towards the Earth, this creates wind shear. A spinning tube of air, created from wind shear; tilts upward into a vertical position, as the updraft sucks up moisture from the ground and into the sky. As the warm air cools high in the sky; this produces condensation. The condensation then produces thunderclouds, which rise to 30,000+ feet. The spinning formations of air are then trapped and lifted into the thundercloud. This begins as swirling motion and as continued (if the winds remained viable), a supercell will form. Mesocyclones as they are known are a rotating cloud. If these rotating clouds run into humid air it will spi...
As evening approached, several thunderstorms began to take on the characteristics of a supercell thunderstorm. Supercells, which are intense, broadly rotating thunderstorms, are the most v...
National Oceanic and Atmospheric Administration (NOAA)/National Climatic Data Center (NCDC), (2001). U.S. Tornado Climatology. Accessed on 9//27/2011 at http://www.ncdc.noaa.gov/oa/climate/severeweather/tornadoes.html#deadly
Tornadoes are devastating atmospheric events that affect the ecology and the lives of people in their paths. Tornadoes are defined as “a violently rotating column of air, in contact with the ground, either pendant from a cumuliform cloud or underneath a cumuliform cloud, and often (but not always) visible as a funnel cloud” (Glossary of Meterology, 2011). The Tri-state tornado was the most deadly tornado in the United States. It stayed on the ground for a total of 219 miles through areas of Missouri, Illinois, and Indiana, killed a total of 695 people, and an estimated $16.5 million in damages (National Weather Service, 2011). Luckily, the tornado’s path was largely rural farmland with scattered small towns between them.
I would like to start out by what we know about tornados and outbreaks, and what is said to be the cause of such catastrophic events, such as the outbreak that occurred November 17th in the Midwestern, portion of the United States. Tornado outbreaks occur when there are multiple tornados that are said to be produced by the same weather system. The classification of an outbreak can vary depending on interpretation. It is said that in order to be classified as a “tornado outbreak” there must be a certain number of tornados that touch down. It is said that the US has the most tornados of any country. This can be attributed the location with in the mid latitude. The Rocky Mountains, have the ability to block moisture and “buckle” the atmospheric flow; thus forcing a lot of dry air at mid-levels of the troposphere, due to downslope winds. While the Rockies are forming a “dry-line” the Gulf of Mexico on the other hand contributes a lot of low level moisture. This mixture of warm air and cold air is to blame for the large number of tornados that form in the US. These events are most prevalent in the Midwestern and Southeastern United States, along with the Great Plains also known as (tornado alley) although some of these systems have been known to move as far North as Canada. The tornado outbreak that took place on the 17th of November is said to have been the one of the largest outbreaks to have occurred in eight years. This particular storm spawned a total of 72 tornados that swept through seven states, according to the National Weather Service. This outbreak is being considered the fourth largest outbreak of its kind, especially this time of year.
An ordinary-single cell is the most common, but multicell and supercells are responsible for the severe thunderstorms. The ordinary single-cell thunderstorms are short lived with three stages: the cumulus, the mature, and the dissipating stages. In the last stage, it eliminates the upward supply of high humidity air needed to maintain a thunderstorm. On the other hand, multicell storms are composed of severe individual single-cell storms that can make storms last for several hours. There is dense, cold air of the downdraft that forms the gust front which forms new cells. Then, groups of these thunderstorms tend to join into larger systems referred to as mesoscale convective
A tornado requires some basic ingredients to come together. First, energy in the form of warm, moist air must exist to feed thunder storms. Second, there must be a top layer of hot, dry air called a cap. This air acts like a lid on a simmering pot, holding in the warm air that’s accumulating in the atmosphere below until the storm’s ready to burst. Last, there has to be rotating winds speeding in oppositedirections at two different levels in the atmosphere, a phenomenon called wind shear, can cause the storms to rotate. Tornado alley is perfectly situated to meet these requirements. (1)
Tornadoes are one of the deadliest and most unpredictable villains mankind will ever face. There is no rhyme or reason, no rhythm to it’s madness. Tornados are one of the most terrifying natural events that occur, destroying homes and ending lives every year. April 29th, 1995, a calm, muggy, spring night I may never forget. Jason, a buddy I grew up with, just agreed to travel across state with me so we could visit a friend in Lubbock. Jason and I were admiring the beautiful blue bonnets, which traveled for miles like little blue birds flying close to the ground. The warm breeze brushed across the tips of the blue bonnets and allowed them to dance under the perfectly clear blue sky. In the distance, however, we could see darkness. A rumbling sky was quickly approaching.
1. According to the USA Today Tornado Information website, a tornado is a "violently rotating column of air in contact with the ground and pendant from a thunderstorm." Therefore, thunderstorms are the first step in the creation of a tornado.
A tornado is defined as a violently rotating column extending from a thunderstorm to the ground. The most violent tornadoes are capable of tremendous destruction with wind speeds of two hundred and fifty miles per hour or more. Damage paths can be more than one mile wide and fifty miles long. In an average year, eight hundred tornadoes are reported nationwide, resulting in eighty deaths and over one thousand five hundred injuries. In the body of my essay, I will tell you about types of tornadoes, where tornadoes come from, where and when tornadoes occur, the damage they inflict, variations of tornadoes, and how to detect tornadoes.