Rænkīnes hātgemet

**Rænkīnes hāt-hwearfes gescēad**
	fram Rænkīne	to Rænkīne
Celsius	[°C] = ([°R] − 491.67) × ⁵⁄₉	[°R] = [°C] × ⁹⁄₅+ 491.67
Fārenhād	[°F] = [°R] − 459.67	[°R] = [°F] + 459.67
Kelvin	[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 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 °F	0 °R
Frēosende ord wæteres^[1]	273.15 K	0 °C	32 °F	491.67 °R
Þrīe ord wæteres (by definition)	273.16 K	0.01 °C	32.018 °F	491.688 °R
Sīeðende ord wæteres^[2]	373.1339 K	99.9839 °C	211.9710 °F	671.641 °R

Hāt-hwearf bord

Fruman

↑ Man gemæt þone īs ord clǣnes wæteres æt 0.000089(10) gemetu Celsius - sēo Magnum, B.W. (Sēremōnaþ 1995). "Reproducibility of the Temperature of the Ice Point in Routine Measurements" (PDF). Nist Technical Note 1411. http://www.cstl.nist.gov/div836/836.05/papers/magnum95icept.pdf. Retrieved 2007-02-11.
↑ For 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.

[1] Man gemæt þone īs ord clǣnes wæteres æt 0.000089(10) gemetu Celsius - sēo Magnum, B.W. (Sēremōnaþ 1995). "Reproducibility of the Temperature of the Ice Point in Routine Measurements" (PDF). Nist Technical Note 1411. http://www.cstl.nist.gov/div836/836.05/papers/magnum95icept.pdf. Retrieved 2007-02-11.

[2] For 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.

[1]

[2]