Rænkīnes hātgemet
{| class="wikitable" align="right" style="margin: 0 0 0.5em 1em;"
|+'''Rænkīnes hāt-hwearfes gescēad'''
|-
!
!fram Rænkīne
!to Rænkīne
|-
!height=30pt|[[Celsius]]
|[°C]&nbsp;=&nbsp;([°R]&nbsp;−&nbsp;491.67)&nbsp;×&nbsp;<span class="frac"><sup>5</sup>⁄<sub>9</sub></span>
|[°R]&nbsp;=&nbsp;[°C]&nbsp;×&nbsp;<span class="frac"><sup>9</sup>⁄<sub>5 </sub>+ &nbsp;491.67</span>
|-
!height=30pt|[[Fārenhād]]
|[°F]&nbsp;=&nbsp;[°R]&nbsp;−&nbsp;459.67
|[°R]&nbsp;=&nbsp;[°F]&nbsp;+&nbsp;459.67
|-
!height=30pt|[[Kelvin]]
|[K]&nbsp;=&nbsp;[°R]&nbsp;×&nbsp;<span class="frac"><sup>5</sup>⁄<sub>9</sub></span>
|[°R]&nbsp;=&nbsp;[K]&nbsp;×&nbsp;<span class="frac"><sup>9</sup>⁄<sub>5</sub></span>

|-
|colspan="3" align="center" | For temperature ''intervals'' rather than specific temperatures,<br/>1 °R = 1 °F = <span class="frac"><sup>5</sup>⁄<sub>9</sub></span> °C = <span class="frac"><sup>5</sup>⁄<sub>9</sub></span> K<br/><small>[[temperature conversion formulas|Comparisons among various temperature scales]]
|}

'''Rankine''' is hātgemet þe bierþ þone nama Scyttisces [[engineer]] and [[physicist]] [[William John Macquorn Rankine]], þe hit teohhode in 1859.

Se tācn '''gemetu Rænkīnes''' is '''°R''' (oþþe '''°Ra''' to healdienne hīe āsundor fram þǣm [[Rømer scale|Rømer]] and [[Réaumur scale|Réaumur]] hātgemetum).  Nāht on begen þǣm Kelvin and Rankine hātgemetum is [[wǣre nāht]], ac þæt Rankines gemet is efen mid ānum gemete [[Fārenhād]]es, būton þonne ān gemet [[Celsius]] þȳ Kelvin hātgemete. Hāt −459.67 °F is wǣre efen mid 0 °R.

<!-- Some engineering fields in the [[United States|U.S.]] and [[Canada]] measure thermodynamic temperature using the Rankine scale.<ref name="physorg">http://www.physorg.com/tags/temperature/</ref> However, throughout the entire scientific world thermodynamic temperature is measured in Kelvin.<ref name="physorg"/> The US [[National Institute of Standards and Technology]] does not recommend using degrees Rankine in NIST publications.<ref name="SP811">[http://physics.nist.gov/Pubs/SP811/appenB8.html B.8 Factors for Units Listed Alphabetically] from [http://physics.nist.gov/Pubs/SP811/contents.html Guide for the Use of the International System of Units (SI)], NIST Special Publication 811, 2008 edition, Ambler Thompson and Barry N. Taylor</ref>

Some key temperatures relating the Rankine scale to other temperature scales are shown in the table below. -->

{| class="wikitable"
|-
|
! Kelvin
! Celsius
! Fahrenheit
! Rankine
|-
! Wǣre nāht<br>(by definition)
|align="center"|0 K
|align="center"|−273.15 °C
|align="center"|−459.67 °F
|align="center"|0 °R
|-
! Frēosende ord wæteres<ref>Man gemæt þone īs ord clǣnes wæteres æt 0.000089(10) gemetu Celsius - sēo {{cite journal | last = Magnum | first = B.W. | year = 1995 | month = Sēremōnaþ
 | title = Reproducibility of the Temperature of the Ice Point in Routine Measurements
 | journal = Nist Technical Note | volume = 1411 
 | url = http://www.cstl.nist.gov/div836/836.05/papers/magnum95icept.pdf
 | format = PDF | accessdate = 2007-02-11 }} 
</ref> 
|align="center"|273.15 K
|align="center"|0 °C
|align="center"|32 °F
|align="center"|491.67 °R
|-
! Þrīe ord wæteres<br>(by definition)
|align="center"|273.16 K
|align="center"|0.01 °C
|align="center"|32.018 °F
|align="center"|491.688 °R
|-
! Sīeðende ord wæteres<ref>For [[Vienna Standard Mean Ocean Water]] at one [[Atmosphere (unit)|standard atmosphere]] (101.325 kPa) when calibrated solely per the two-point definition of thermodynamic temperature. Older definitions of the Celsius scale once defined the boiling point of water under one standard atmosphere as being precisely 100&nbsp;°C. However, the current definition results in a boiling point that is actually 16.1&nbsp;mK less. For more about the actual boiling point of water, see [[Vienna Standard Mean Ocean Water#VSMOW in temperature measurement|VSMOW in temperature measurement]].</ref>
|align="center"|373.1339 K
|align="center"|[[Celsius#Melting_and_boiling_points_of_water|99.9839 °C]]
|align="center"|211.9710 °F
|align="center"|671.641 °R
|}

==Hāt-hwearf bord==

{{Timeline Temperature Conversion}}

==Fruman==

{{reflist}}

[[Flocc:Hātgemetu]]
+Rænkīnes hāt-hwearfes gescēadfram Rænkīneto RænkīneCelsius[°C] = ([°R] − 491.67) × 5⁄9[°R] = [°C] × 9⁄5 +  491.67Fārenhād[°F] = [°R] − 459.67[°R] = [°F] + 459.67Kelvin[K] = [°R] × 5⁄9[°R] = [K] × 9⁄5 For temperature intervals rather than specific temperatures,1 °R = 1 °F = 5⁄9 °C = 5⁄9 K<small>Comparisons among various temperature scales

Rankine is hātgemet þe bierþ þone nama Scyttisces engineer and physicist William John Macquorn Rankine, þe hit teohhode in 1859.

Se tācn gemetu Rænkīnes is °R (oþþe °Ra to healdienne hīe āsundor fram þǣm Rømer and Réaumur hātgemetum).  Nāht on begen þǣm Kelvin and Rankine hātgemetum is wǣre nāht, ac þæt Rankines gemet is efen mid ānum gemete Fārenhādes, būton þonne ān gemet Celsius þȳ Kelvin hātgemete. Hāt −459.67 °F is wǣre efen mid 0 °R.

 Kelvin Celsius Fahrenheit Rankine Wǣre nāht(by definition)0 K−273.15 °C−459.67 °F0 °R Frēosende ord wæteresMan gemæt þone īs ord clǣnes wæteres æt 0.000089(10) gemetu Celsius - sēo   273.15 K0 °C32 °F491.67 °R Þrīe ord wæteres(by definition)273.16 K0.01 °C32.018 °F491.688 °R Sīeðende ord wæteresFor Vienna Standard Mean Ocean Water at one standard atmosphere (101.325 kPa) when calibrated solely per the two-point definition of thermodynamic temperature. Older definitions of the Celsius scale once defined the boiling point of water under one standard atmosphere as being precisely 100 °C. However, the current definition results in a boiling point that is actually 16.1 mK less. For more about the actual boiling point of water, see VSMOW in temperature measurement.373.1339 K99.9839 °C211.9710 °F671.641 °R

Hāt-hwearf bord

Fruman

Flocc:Hātgemetu