The TORRO tornado intensity scale (or T-Scale) is a scale measuring
tornado intensity
Tornado intensity is the measure of wind speeds and potential risk produced by a tornado. Intensity can be measured by In situ#Earth and atmospheric sciences, ''in situ'' or remote sensing measurements, but since these are impractical for wide- ...
between T0 and T11. It was proposed by Terence Meaden of the
Tornado and Storm Research Organisation (TORRO), a
meteorological
Meteorology is the scientific study of the Earth's atmosphere and short-term atmospheric phenomena (i.e. weather), with a focus on weather forecasting. It has applications in the military, aviation, energy production, transport, agriculture ...
organisation in the
United Kingdom
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Northwestern Europe, off the coast of European mainland, the continental mainland. It comprises England, Scotlan ...
, as an extension of the
Beaufort scale
The Beaufort scale ( ) is an empirical measure that relates wind speed to observed conditions at sea or on land. Its full name is the Beaufort wind force scale. It was devised in 1805 by Francis Beaufort a hydrographer in the Royal Navy. It ...
.
History and derivation from Beaufort scale
The scale was tested from 1972 to 1975 and was made public at a meeting of the
Royal Meteorological Society
The Royal Meteorological Society is an organization that promotes academic and public engagement in weather and climate science. Fellows of the Society must possess relevant qualifications, but Members can be lay enthusiasts. It publishes vari ...
in 1975. The scale sets T0 as the equivalent of 8 on the Beaufort scale and is related to the Beaufort scale (B), up to 12 on the Beaufort scale, by the formula:
: ''B'' = 2 (''T'' + 4)
and conversely:
: ''T'' = ''B''/2 - 4
The
Beaufort scale
The Beaufort scale ( ) is an empirical measure that relates wind speed to observed conditions at sea or on land. Its full name is the Beaufort wind force scale. It was devised in 1805 by Francis Beaufort a hydrographer in the Royal Navy. It ...
was first introduced in 1805, and in 1921 quantified. It expresses the wind speed as faster than v in the formula:
:
v = 0.837 ''B''
3/2 m/s
TORRO scale formula
Most UK tornadoes are T6 or below with the strongest known UK tornado estimated as a T9 (the 1666 Lincolnshire tornado). For comparison, the strongest detected winds in a United States tornado (during the
1999 Oklahoma tornado outbreak) would be T11 using the following formulas:
: ''
v'' = 2.365 (''T''+4)
3/2 m/s
: ''
v'' = 8.511 (''T''+4)
3/2 km/h
The kilometre per hour ( SI symbol: km/h; non-SI abbreviations: kph, kmph, km/hr) is a unit of speed, expressing the number of kilometres travelled in one hour.
History
Although the metre was formally defined in 1799, the term "kilometres per h ...
: ''
v'' = 5.289 (''T''+4)
3/2 mph
: ''
v'' = 4.596 (''T''+4)
3/2 kn
where ''v'' is
wind speed
In meteorology, wind speed, or wind flow speed, is a fundamental atmospheric quantity caused by air moving from high to low pressure, usually due to changes in temperature. Wind speed is now commonly measured with an anemometer.
Wind spe ...
and ''T'' is TORRO intensity number. Wind speed is defined as a 3-second gust at 10
m AGL.
Alternatively, the T-Scale formula may be expressed as:
:
v = 0.837 (2''T''+8)
3/2 m/s
or
:
v = 0.837(2
3/2) (''T''+4)
3/2 m/s
: or
:
Rating process and comparisons to Fujita scale
TORRO claims it differs from the
Fujita scale
The Fujita scale (F-Scale; ), or Fujita–Pearson scale (FPP scale), is a scale for rating tornado intensity, based primarily on the damage tornadoes inflict on human-built structures and vegetation. The official Fujita scale category is determ ...
in that it is "purely" a wind speed scale, whereas the Fujita scale relies on damage for classification, but in practice, damage is utilised almost exclusively in both systems to infer intensity. That is because such a proxy for intensity is usually all that is available, although users of both scales would prefer direct, objective, quantitative measurements. The scale is primarily used in the United Kingdom whereas the Fujita scale has been the primary scale used in North America, continental Europe, and the rest of the world.
At the 2004 European Conference on Severe Storms, Dr. Meaden proposed a unification of the TORRO and Fujita scales as the Tornado Force or TF Scale. In 2007 in the United States, the
Enhanced Fujita Scale
The Enhanced Fujita scale (abbreviated EF-Scale) is a scale that rates tornado intensity based on the severity of the damage a tornado causes. It is used in the United States and France, among other countries. The EF scale is also unofficially ...
replaced the original Fujita Scale from 1971. It made substantial improvements in standardizing damage descriptors through expanding and refining damage indicators and associated degrees of damage, as well as calibrated tornado wind speeds to better match the associated damage. However, the EF Scale, having been designed based on construction practices in the United States, is not necessarily applicable across all regions. The EF-scale and variants thereof are officially used by the United States, Canada, France, and Japan, as well as unofficially in other countries, such as China.
Unlike with the F scale, no analyses have been undertaken at all to establish the veracity and accuracy of the T scale damage descriptors. The scale was written in the early 1970s, and does not take into account changes such as the growth in weight of vehicles or the great reduction in numbers and change of type of railway locomotives, and was written in an environment where tornadoes of F2 or stronger are extremely rare, so little or no first-hand investigation of actual damage at the upper end of the scale was possible. The TORRO scale has more graduations than the F scale which makes it arguably more useful for tornadoes on the lower end of the scale; however, such accuracy and precision are not typically attainable in practice.
Brooks and
Doswell stated that "the problems associated with damage surveys and uncertainties associated with estimating wind speed from observed damage make highly precise assignments dubious".
In survey reports, Fujita ratings sometimes also have extra qualifications added ("minimal F2" or "upper-end F3 damage"), made by investigators who have experience of many similar tornadoes and relating to the fact that the F scale is a damage scale, not a wind speed scale.
Tornadoes are rated after they have passed and have been examined, not whilst in progress. In rating the intensity of a tornado, both direct measurements and inferences from empirical observations of the effects of a tornado are used. Few
anemometer
In meteorology, an anemometer () is a device that measures wind speed and direction. It is a common instrument used in weather stations. The earliest known description of an anemometer was by Italian architect and author Leon Battista Alberti ...
s are struck by a tornado, and even fewer survive, so there are very few
in-situ
is a Latin phrase meaning 'in place' or 'on site', derived from ' ('in') and ' ( ablative of ''situs'', ). The term typically refers to the examination or occurrence of a process within its original context, without relocation. The term is use ...
measurements. Therefore, almost all ratings are obtained from
remote sensing
Remote sensing is the acquisition of information about an physical object, object or phenomenon without making physical contact with the object, in contrast to in situ or on-site observation. The term is applied especially to acquiring inform ...
techniques or as
proxies from damage surveys.
Weather radar
A weather radar, also called weather surveillance radar (WSR) and Doppler weather radar, is a type of radar used to locate precipitation (meteorology), precipitation, calculate its motion, and estimate its type (rain, snow, hail etc.). Modern w ...
is used when available, and sometimes
photogrammetry
Photogrammetry is the science and technology of obtaining reliable information about physical objects and the environment through the process of recording, measuring and interpreting photographic images and patterns of electromagnetic radiant ima ...
or
videogrammetry estimates wind speed by measuring tracers in the vortex. In most cases, aerial and ground damage surveys of structures and vegetation are utilised, sometimes with engineering analysis. Also sometimes available are ground swirl patterns (
cycloidal marks) left in the wake of a tornado. If an on site analysis is not possible, either for retrospective ratings or when personnel cannot reach a site, photographs, videos, or descriptions of damage may be utilised.
TORRO scale parameters
The 12 categories for the TORRO scale are listed below, in order of increasing intensity. Although the wind speeds and photographic damage examples are updated, which are more or less still accurate. However, for the actual TORRO scale in practice, damage indicators (the type of structure which has been damaged) are predominantly used in determining the tornado intensity.
See also
*
Saffir-Simpson Hurricane Scale
*
Tornado intensity and damage
*
Wind engineering
Wind engineering is a subset of mechanical engineering, structural engineering, meteorology, and applied physics that analyzes the effects of wind in the natural and the built environment and studies the possible damage, inconvenience or benefit ...
*
List of tornadoes and tornado outbreaks
References
*
*
* {{cite journal , last = Meaden , first = G. T. , title = A study of tornadoes in Britain, with assessments of the general tornado risk potential and the specific risk potential at particular regional sites , journal =
Journal of Meteorology , volume = 8 , issue = 79 , pages = 151–3 , location = UK , year = 1985
External links
TORRO Tornado Intensity Scale(TORRO)
T-Scale Origins and Scientific Basis(TORRO)
(TORRO)
(TorDACH)
Hazard scales
Wind
Tornado
Scales in meteorology