The Fujita Scale is used to rate the intensity of a tornado oleh examining the damage caused oleh the tornado after it has passed over a man-made structure.

The "Percentage of All Tornadoes 1950-1994" pie chart reveals that the vast majority of tornadoes are either weak atau do damage that can only be attributed to a weak tornado. Only a small percentage of tornadoes can be correctly classed as violent. Such a chart became possible only after the acceptance of the Fujita Scale as the official classification system for tornado damage. It is quite possible that an even higher percentage of all tornadoes are weak. Each tahun the National Weather Service documents about 1000 tornado touchdowns in the United States. There is evidence that 1000 atau lebih additional weak tornadoes may occur each tahun and go completely undocumented.

The "Percentage of Tornado-Related Deaths 1950-1994" pie chart shows that while violent tornadoes are few in number, they cause a very high percentage of tornado-related deaths. The Tornado Project has analyzed data prior to 1950, and found that the percentage of deaths from violent tornadoes was even greater in the past. This is because the death tolls prior to the introduction of the forecasting/awareness programs were enormous: 695 dead(Missouri-Illinois-Indiana, March 18, 1925); 317 dead(Natchez, Mississippi, May 7, 1840);.255 dead(St. Louis, Missouri and East St. Louis, Illinois, May 27, 1896); 216 dead(Tupelo, Mississippi, April 5, 1936); 203 dead(Gainesville, GA, April 6, 1936). In lebih baru saja times, no single tornado has killed lebih than 50 people since 1971.

The Fujita Scale(also known as the Fujita-Pearson Scale) may not be a perfect system for linking damage to wind speed, but it had distinct advantages over what had gone on before its inception. And it was simple enough to use in daily practice without involving much additional expenditure of time atau money. From a practical point of view, it is doubtful that any other system would have found its way into widespread accepted use, even to this day. The entire premise of estimating wind speeds from damage to non-engineered structures is very subjective and is difficult to defend from various meteorological perspectives. Nothing less than the combined influence and and prestige of the late Professor Fujita and Allen Pearson, director of NSSFC(National Severe Storm Forecast Center) in 1971 could have brought this much needed system into widespread use. The FPP scale rates the intensity of the tornado, and measured both the path length and the path width. The Fujita part of the scale is as follows:

A key point to remember is this: the size of a tornado is not necessarily an indication of its intensity. Large tornadoes can be weak, and small tornadoes can be violent. A good example of a relatively "small" tornado would be the Pampa, Texas tornado of 1995, which can be seen in Tornado Video Classics III. This tornado is pictured on the right side of the slipcase, shown here. Notice the debris in the air. Eyewitnesses to this tornado claim to have seen as many as 6 vehicles in the air at the same time when it passed over a parking lot. Another consideration is the stage in the life cycle of the tornado. A "small" tornado may have been larger, and is at the "shrinking" stage of its life cycle, like the Tracy, Minnesota tornado on one of our posters, and also our logo, seen on the navigation bar to the left if anda are using our frames. Large tornadoes can also be strong and small tornadoes can be weak. The Fujita Scale is based on damage, not the appearance of the funnel. Storm spotters, storm chasers and other weather observers often try to estimate the intensity of a tornado when they are in the field, basing their judgement on the rotational speed and amount of debris being generated as well as the width. However, the official estimate is made after the tornado has passed. Personnel from the National Weather Service office that issued the warning survey the site to determine the F-Scale rating. Sometimes they call in experts from out of the area. Aerial surveys are occasionally done after violent tornadoes to determine the exact damage track. Insurance companies may also call in wind engineers to do their own evaluations, but the official rating is set oleh the NWS. A few of the things they all look for are:

* attachment of the walls and floor to the foundation of the building
* attachment of the roof to the rafters and walls
* whether atau not there are steel reinforcing rods in concrete atau cinder block walls
* whether there is mortar between the cinder blocks

After the NWS office does the survey, the official rating is recorded, and eventually diposting at the SPC site. If it is a killer tornado we also post the rating on our site with the keterangan of the event, and on our "all tornadoes" page. The NWS office may also write up a lebih extensive report, which may atau may not be diposting on the web. A good example of such a laporan would be the one done on the Florida tornadoes of March, 1998.

The Fujita Scale is very subjective, and varies according to how experienced the surveyor is. We have many readers who have tried to do their own "surveys" of tornado damage when storms have occurred in their area. However, the less experienced the surveyor is, the lebih likely he/she is to be awed oleh the damage, and the lebih likely they are to give it a high rating. Brian Smith of the Omaha, Nebraska area NWS office, a former student of Dr. Fujita and an expert frequently brought in to do site surveys, tells of hearing about a tee-shirt with the words "F-3 My Foot" printed on it.

Media hype and inexperience with tornado damage also plays a big part in exaggerated F-Scale claims seen on televisi atau in the paper. A reporter may see a collapsed concrete block halaman awal and be very impressed, never noticing that there was no mortar between the blocks. They may be aghast to see a park whose trees have been leveled, but not know that the species had very shallow roots, planted in soil that was soft and soggy from torrential rains, and thus easily toppled. They may see a roof that had been blown a quarter of a mile from its house, and not know that the roof was attached to the house with only a few nails, and when lofted into the air, acted as a "sail." They may see a light post that is bent at a 30 degree angle and think that it must have taken a 600 mph wind to do that, not knowing that a mobil van, van had been blown into the pole, bending it, then been towed off to help clear the streets. For some of the media, the exaggerations make for a better story than the actual facts. Fortunately, they often make up for this oleh printing helpful stories about aid available and inspirational human interest stories.

As if doing a site survey of a track is not difficult enough, tornadic storms may also be accompanied oleh complex combinations of strong downbursts and other straight line winds. Separating tornado damage from other wind damage makes for a daunting, difficult task for even the most experienced surveyor.

The Seymour, Texas, tornado of April 10, 1979 is a prime example of a tornado that is destined to be misjudged on the Fujita Scale. This spectacular funnel was probably capable of F4 damage, had it passed through a town. It produced only telephone pole and pohon damage, and thus could be rated no higher than F2 damage. The Seymour tornado was in the same family as the devastating Wichita Falls, Texas tornado, which remains as of this writing, the most damaging in US history. Video of this tornado is used in the Fujita Scale segment of Tornado Video Classics II

Professor Fujita continued his work until his death at the age of 78. Mr. Pearson is semi-retired, and is very active on the web.