The Fahrenheit scale (//) is a temperature scale based on one proposed in 1724 by physicist Daniel Gabriel Fahrenheit (1686–1736). It uses the degree Fahrenheit (symbol: degree Fahrenheit) as the unit. Several accounts of how he originally defined his scale exist. The lower defining point, 0 degrees Fahrenheit, was established as the freezing temperature of a solution of brine made from equal parts of ice, water and a salt (ammonium chloride). Further limits were established as the freezing point of water (32 degrees Fahrenheit) and his best estimate of the average human body temperature (96 degrees Fahrenheit, about 2.6 degrees Fahrenheit less than the modern value due to a later redefinition of the scale). The scale is now usually defined by two fixed points: the temperature at which water freezes into ice is defined as 32 degrees Fahrenheit, and the boiling point of water is defined to be 212 degrees Fahrenheit, a 180 degree Fahrenheit separation, as defined at sea level and standard atmospheric pressure.
|Unit system||Imperial/US customary|
|Named after||Daniel Gabriel Fahrenheit|
|x degree Fahrenheit in ...||... is equal to ...|
|degree Celsius||5/(x − 32)|
Fahrenheit is the first standardized temperature scale to be widely used. It is the official temperature scale in the United States (including its unincorporated territories), its freely associated states in the Western Pacific (Palau, the Federated States of Micronesia and the Marshall Islands), the Cayman Islands, and Liberia. Antigua and Barbuda and other islands which use the same meteorological service, such as Saint Kitts and Nevis, the Bahamas, and Belize, use Fahrenheit and Celsius. All other countries in the world officially now use the Celsius scale, named after Swedish astronomer Anders Celsius. A handful of British Overseas Territories still use Fahrenheit alongside Celsius including the British Virgin Islands, Montserrat, Anguilla, and Bermuda.
|from Fahrenheit||to Fahrenheit|
|Celsius||[ degree Celsius] = ([ degree Fahrenheit] − 32) × 5⁄9||[ degree Fahrenheit] = [ degree Celsius] × 9⁄5 + 32|
|Kelvin||[K] = ([ degree Fahrenheit] + 459.67) × 5⁄9||[ degree Fahrenheit] = [K] × 9⁄5 − 459.67|
|Rankine||[ degree R] = [ degree Fahrenheit] + 459.67||[ degree Fahrenheit] = [ degree R] − 459.67|
|For temperature intervals rather than specific temperatures,|
1 degree Fahrenheit = 1 degree R = 5⁄9 degree Celsius = 5⁄9 K
Comparisons among various temperature scales
On the Fahrenheit scale, the freezing point of water is 32 degrees Fahrenheit ( degree Fahrenheit) and the boiling point is 212 degrees Fahrenheit (at standard atmospheric pressure). This puts the boiling and freezing points of water 180 degrees apart. Therefore, a degree on the Fahrenheit scale is 1⁄180 of the interval between the freezing point and the boiling point. On the Celsius scale, the freezing and boiling points of water are 100 degrees apart. A temperature interval of 1 degree Fahrenheit is equal to an interval of 5⁄9 degrees Celsius. The Fahrenheit and Celsius scales intersect at −40 degrees (i.e., −40 degrees Fahrenheit = −40 degrees Celsius).
Absolute zero is −273.15 degrees Celsius or −459.67 degrees Fahrenheit. The Rankine temperature scale uses degree intervals of the same size as those of the Fahrenheit scale, except that absolute zero is 0 degrees R — the same way that the Kelvin temperature scale matches the Celsius scale, except that absolute zero is 0 Kelvin.
The Fahrenheit scale uses the symbol degree to denote a point on the temperature scale (as does Celsius) and the letter F to indicate the use of the Fahrenheit scale (e.g. "Gallium melts at 85.5763 degrees Fahrenheit"), as well as to denote a difference between temperatures or an uncertainty in temperature (e.g. "The output of the heat exchanger experiences an increase of 72 degrees Fahrenheit" and "Our standard uncertainty is plus or minus 5 degrees Fahrenheit").
For an exact conversion, the following formulas can be applied. Here, f is the value in Fahrenheit and c the value in Celsius:
- f degree Fahrenheitahrenheit to c degree Celsiuselsius : (f − 32) degree Fahrenheit × 5 degrees Celsius/ = (f − 32)/ degree Celsius = c degree Celsius
- c degree Celsiuselsius to f degree Fahrenheitahrenheit : (c degree Celsius × 9 degrees Fahrenheit/) + 32 degrees Fahrenheit = (c × 1.8) degree Fahrenheit + 32 degrees Fahrenheit = f degree Fahrenheit
This is also an exact conversion making use of the identity −40 degrees Fahrenheit = −40 degrees Celsius. Again, f is the value in Fahrenheit and c the value in Celsius:
- f degree Fahrenheitahrenheit to c degree Celsiuselsius : ((f + 40) ÷ 1.8) − 40 = c.
- c degree Celsiuselsius to f degree Fahrenheitahrenheit : ((c + 40) × 1.8) − 40 = f.
Fahrenheit proposed his temperature scale in 1724, basing it on two reference points of temperature. In his initial scale (which is not the final Fahrenheit scale), the zero point was determined by placing the thermometer in a mixture "of ice, of water, and of ammonium chloride (salis Armoniaci) or even of sea salt". This combination forms a eutectic system which stabilizes its temperature automatically: 0 degrees Fahrenheit was defined to be that stable temperature. The second point, 96 degrees, was approximately the human body's temperature (sanguine hominis sani, the blood of a healthy man).
According to a German story, Fahrenheit actually chose the lowest air temperature measured in his hometown Danzig (Gdańsk, Poland) in winter 1708/09 as 0 degrees Fahrenheit, and only later had the need to be able to make this value reproducible using brine.
According to a letter Fahrenheit wrote to his friend Herman Boerhaave, his scale was built on the work of Ole Rømer, whom he had met earlier. In Rømer's scale, brine freezes at zero, water freezes and melts at 7.5 degrees, body temperature is 22.5, and water boils at 60 degrees. Fahrenheit multiplied each value by four in order to eliminate fractions and make the scale more fine-grained. He then re-calibrated his scale using the melting point of ice and normal human body temperature (which were at 30 and 90 degrees); he adjusted the scale so that the melting point of ice would be 32 degrees and body temperature 96 degrees, so that 64 intervals would separate the two, allowing him to mark degree lines on his instruments by simply bisecting the interval six times (since 64 is 2 to the sixth power).
Fahrenheit soon after observed that water boils at about 212 degrees using this scale. The use of the freezing and boiling points of water as thermometer fixed reference points became popular following the work of Anders Celsius and these fixed points were adopted by a committee of the Royal Society led by Henry Cavendish in 1776. Under this system, the Fahrenheit scale is redefined slightly so that the freezing point of water is exactly 32 degrees Fahrenheit, and the boiling point is exactly 212 degrees Fahrenheit or 180 degrees higher. It is for this reason that normal human body temperature is approximately 98.6 degrees (oral temperature) on the revised scale (whereas it was 90 degrees on Fahrenheit's multiplication of Rømer, and 96 degrees on his original scale).
In the present-day Fahrenheit scale, 0 degrees Fahrenheit no longer corresponds to the eutectic temperature of ammonium chloride brine as described above. Instead, that eutectic is at approximately 4 degrees Fahrenheit on the final Fahrenheit scale.
The Fahrenheit scale was the primary temperature standard for climatic, industrial and medical purposes in English-speaking countries until the 1960s. In the late 1960s and 1970s, the Celsius scale replaced Fahrenheit in almost all of those countries—with the notable exception of the United States—typically during their general metrication process.
Fahrenheit is used in the United States, its territories and associated states (all served by the U.S. National Weather Service), as well as the Cayman Islands and Liberia for everyday applications. For example, U.S. weather forecasts, food cooking, and freezing temperatures are typically given in degrees Fahrenheit. Scientists, such as meteorologists, use degrees Celsius or kelvin in all countries.
Early in the 20th century, Halsey and Dale suggested that the resistance to the use of centigrade (now Celsius) system in the U.S. included the larger size of each degree Celsius and the lower zero point in the Fahrenheit system.
Canada has passed legislation favoring the International System of Units, while also maintaining legal definitions for traditional Canadian imperial units. Canadian weather reports are conveyed using degrees Celsius with occasional reference to Fahrenheit especially for cross-border broadcasts. Fahrenheit is still used on virtually all Canadian ovens, Thermometers, both digital and analog, sold in Canada usually employ both the Celsius and Fahrenheit scales.
In the European Union, it is mandatory to use kelvins or degrees Celsius when quoting temperature for "economic, public health, public safety and administrative" purposes, though degrees Fahrenheit may be used alongside degrees Celsius as a supplementary unit. For example, the laundry symbols used in the United Kingdom follow the recommendations of ISO 3758:2005 showing the temperature of the washing machine water in degrees Celsius only. The equivalent label in North America uses one to six dots to denote temperature with an optional temperature in degrees Celsius.
Within the unregulated sector, such as journalism, the use of Fahrenheit in the United Kingdom follows no fixed pattern with degrees Fahrenheit often appearing alongside degrees Celsius. The Daily Mail, on its daily weather page, quotes Celsius first, followed by Fahrenheit in brackets,The Daily Telegraph does not mention Fahrenheit on its daily weather page while The Times also has an all-metric daily weather page but has a Celsius-to-Fahrenheit conversion table. When publishing news stories, much of the UK press have adopted a tendency of using degrees Celsius in headlines and discussion relating to low temperatures and Fahrenheit for high temperatures.[discuss] In February 2006, the writer of an article in The Times suggested that the rationale was one of emphasis: "−6 degrees Celsius" sounds colder than "21 degree Fahrenheit" and "94 degrees Fahrenheit" sounds more impressive than "34 degrees Celsius".
Unicode provides the Fahrenheit symbol at code point U+2109 ℉ DEGREE FAHRENHEIT. However, this is a compatibility character encoded for roundtrip compatibility with legacy encodings. The Unicode standard explicitly discourages the use of this character: "The sequence U+00B0 degree DEGREE SIGN +U+0046 F LATIN CAPITAL LETTER F is preferred over U+2109 ℉ DEGREE FAHRENHEIT, and those two sequences should be treated as identical for searching."
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For decades mercury thermometers were a mainstay in many testing laboratories. If used properly and calibrated correctly, certain types of mercury thermometers can be incredibly accurate. Mercury thermometers can be used in temperatures ranging from about -38 to 350 degrees Celsius. The use of a mercury-thallium mixture can extend the low-temperature usability of mercury thermometers to -56 degrees Celsius. (...) Nevertheless, few liquids have been found to mimic the thermometric properties of mercury in repeatability and accuracy of temperature measurement. Toxic though it may be, when it comes to LiG [Liquid-in-Glass] thermometers, mercury is still hard to beat.
- "Sal Armoniac" was an impure form of ammonium chloride. The French chemist Nicolas Lemery (1645–1715) discussed it in his book Cours de Chymie (A Course of Chemistry, 1675), describing where it occurs naturally and how it can be prepared artificially. It occurs naturally in the deserts of northern Africa, where it forms from puddles of animal urine. It can be prepared artificially by boiling 5 parts of urine, 1 part of sea salt, and one-half part of chimney soot until the mixture has dried. The mixture is then heated in a sublimation pot until it sublimates ; the sublimated crystals are sal Armoniac. See:
- Nicolas Lemery, Cours de chymie … , seventh ed. (Paris, France: Estienne Michallet, 1688), Chapitre XVII: du Sel Armoniac, pp. 338–339.
- English translation: Nicolas Lemery with James Keill, trans., A Course of Chymistry … , third ed. (London, England: Walter Kettilby, 1698), Chap. XVII: of Sal Armoniack, p. 383. Available on-line at: Heinrich Heine University (Düsseldorf, Germany)
- Fahrenheit, Daniele Gabr. (1724) Experimenta & observationes de congelatione aquæ in vacuo factæ a D. G. Fahrenheit, R. S. S (Experiments and observations on water freezing in the void by D. G. Fahrenheit, R. S. S.), Philosophical Transactions of the Royal Society of London, vol. 33, no. 382, page 78 (March–April 1724). Cited and translated in http://www.sizes.com:80/units/temperature_Fahrenheit.htm
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- Eutectic temperature of ammonium chloride and water is listed as −15.9 degrees Celsius (3.38 degrees Fahrenheit) and as −15.4 degrees Celsius (4.28 degrees Fahrenheit) in (respectively)
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|Look up fahrenheit in Wiktionary, the free dictionary.|
- Daniel Gabriel Fahrenheit (Polish-born Dutch physicist) – Encyclopædia Britannica
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