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 Photos

 

This photo was taken on a turnpike ~ 10-20 miles north of Norman, OK. USA in April of 1991. 

Photo by Bryan Patrick


These tornadoes were spawned by a cyclic supercell in the United States on the 29th May 2001


A large land spout type tornado NW of McLeans Ridges on 29th January 2001


 

:: Tornadoes

Tornado, violently rotating column of air extending from within a thundercloud down to ground level. The strongest tornadoes may sweep houses from their foundations, destroy brick buildings, toss cars and school buses through the air, and even lift railroad cars from their tracks. Tornadoes vary in diameter from tens of meters to nearly 2 km (1 mi), with an average diameter of about 50 m (160 ft). Most tornadoes in the northern hemisphere create winds that blow counterclockwise around a center of extremely low atmospheric pressure. In the southern hemisphere the winds generally blow clockwise. Peak wind speeds can range from near 120 km/h (75 mph) to almost 500 km/h (300 mph). The forward motion of a tornado can range from a near standstill to almost 110 km/h (70 mph).

A tornado becomes visible when a condensation funnel made of water vapor (a funnel cloud) forms in extreme low pressures, or when the tornado lofts dust, dirt, and debris upward from the ground

. A mature tornado may be columnar or tilted, narrow or broad—sometimes so broad that it appears as if the parent thundercloud itself had descended to ground level. Some tornadoes resemble a swaying elephant's trunk. Others, especially very violent ones, may break into several intense suction vortices—intense swirling masses of air—each of which rotates near the parent tornado. A suction vortex may be only a few meters in diameter, and thus can destroy one house while leaving a neighboring house relatively unscathed.

Scientists study tornadoes to gain a better understanding of their formation, behavior, and structure. Scientists who study tornadoes have a variety of powerful research tools at their disposal. Advances in computer technology make it possible to simulate the thunderstorms that spawn tornadoes using computer models running on desktop computers. Doppler radars, which detect the rain in clouds, allow meteorologists, scientists who study weather, to "see" the winds inside the storms that spawn tornadoes. Modern video camera footage and reports from trained storm-spotters provide an unprecedented amount of high-quality tornado documentation. These tools all contribute greatly to the scientific understanding of tornadoes. This information may eventually lead to increased tornado warning times, better guidelines for building construction (especially schools), and improved safety tips.

 

Formation

Many tornadoes, including the strongest ones, develop from a special type of thunderstorm known as a supercell. A supercell is a long-lived, rotating thunderstorm 10 to 16 km (6 to 10 mi) in diameter that may last several hours, travel hundreds of miles, and produce several tornadoes. Supercell tornadoes are often produced in sequence, so that what appears to be a very long damage path from one tornado may actually be the result of a new tornado that forms in the area where the previous tornado died. Sometimes, tornado outbreaks occur, and swarms of supercell storms may occur. Each supercell may spawn a tornado or a sequence of tornadoes.

 This information has brought it to you from Encarta 2002

 

 

 

 

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