Rankine to Romer

°R

1 °R

°Rø

-135.612083333333333333331 °Rø

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Quick Reference Table (Rankine to Romer)

Rankine (°R)Romer (°Rø)
0-135.90375
459.67-1.8333333333333333333345
491.677.5
527.6718
558.2726.925
671.6760

About Rankine (°R)

Rankine (°R) is an absolute temperature scale that uses Fahrenheit-sized degrees. Like the kelvin it starts at absolute zero (0°R), but its degree intervals match Fahrenheit rather than Celsius. This makes it useful in US customary engineering thermodynamics — particularly older American aerospace, HVAC, and mechanical engineering literature — where Fahrenheit-based calculations must account for absolute temperature. Water freezes at 491.67°R, boils at 671.67°R, and body temperature is 558.27°R. The Rankine scale is rarely used today outside legacy US engineering calculations; SI units with kelvin have largely replaced it internationally and increasingly within the US engineering community as well.

Jet engine combustion temperatures around 2,500°F (1,371°C) equal approximately 2,960°R in thermodynamic calculations. Cryogenic oxygen (−183°C) is about 163°R.

Etymology: Named after Scottish engineer William John Macquorn Rankine (1820–1872), who proposed the scale in 1859. Rankine made major contributions to thermodynamics, steam engine theory, and civil engineering. The Rankine cycle — the theoretical model for steam power plants — is also named after him.

About Romer (°Rø)

The Rømer scale (°Rø) is a historical temperature scale created by Danish astronomer Ole Christensen Rømer in 1701 — one of the earliest quantitative thermometric scales. Rømer set 7.5°Rø as the freezing point of water and 60°Rø as the boiling point. The lower reference of 0°Rø was set below the coldest Danish winter temperature to avoid negative readings. Body temperature is approximately 22.5°Rø. The Rømer scale is historically significant because Daniel Gabriel Fahrenheit visited Rømer in Copenhagen in 1708, was directly inspired by his work, and later developed the Fahrenheit scale partly building on Rømer's two-point calibration method. Today it is purely of historical interest.

The freezing point of water is 7.5°Rø. A pleasant summer day (25°C) is approximately 20.6°Rø. Boiling water is 60°Rø.

Etymology: Named after Ole Christensen Rømer (1644–1710), the Danish astronomer who also made the first quantitative measurement of the speed of light in 1676, using observations of Jupiter's moon Io. He proposed the temperature scale around 1701 using wine and water thermometers with two fixed calibration points.


Rankine – Frequently Asked Questions

Rankine is used in US customary thermodynamic calculations where absolute temperature is needed but Fahrenheit-scale degrees are preferred. It appears in older American engineering standards for steam power, HVAC, and aerospace — disciplines where engineers needed an absolute scale compatible with Fahrenheit-unit formulas without converting to kelvin.

Both start at absolute zero (0 K = 0°R), but their degree sizes differ. One kelvin equals 1.8 Rankine degrees, matching the 1.8 ratio between Celsius and Fahrenheit degree sizes. So 273.15 K = 491.67°R. To convert: °R = K × 1.8.

Divide by 1.8 to get kelvin, then subtract 273.15. Formula: °C = (°R / 1.8) − 273.15. For example, 491.67°R ÷ 1.8 = 273.15 K; 273.15 − 273.15 = 0°C. Alternatively: °C = (°R − 491.67) / 1.8.

Absolute zero is 0°R, the same as 0 K and −273.15°C (−459.67°F). Because Rankine starts at absolute zero, it has no negative values — a property shared with kelvin. This is what makes it useful in thermodynamics: equations requiring absolute temperature work directly without offset corrections.

Rankine use has declined significantly. Most modern engineering, including US aerospace and HVAC standards, has shifted to SI units (kelvin). Rankine persists mainly in legacy documents, some US university thermodynamics courses that teach both systems, and niche industries still working from older US customary standards. New engineering work rarely specifies Rankine.

Romer – Frequently Asked Questions

The Rømer scale was created by Danish astronomer Ole Christensen Rømer around 1701. Rømer is also famous for being the first person to measure the speed of light quantitatively in 1676, determining it by observing time variations in the eclipses of Jupiter's moon Io from different positions of Earth in its orbit.

Rømer set 0°Rø below the coldest temperature he expected in Denmark so that all practical outdoor measurements would be positive. This was a common design principle for early thermometric scales — avoiding negative values in everyday use. The 7.5 value arose from his calibration methodology using two fixed reference points and dividing the interval into 52.5 equal parts.

Normal body temperature (37°C) is approximately 22.5°Rø on the Rømer scale. Rømer himself used body temperature as one of his calibration reference points, which Fahrenheit later borrowed when constructing the Fahrenheit scale — translating Rømer's body temperature reference into his own 96°F calibration point.

Daniel Gabriel Fahrenheit visited Ole Rømer in Copenhagen in 1708 and observed his thermometers and calibration method. Fahrenheit adopted Rømer's idea of using two fixed reference points and the principle of avoiding negative temperatures in common conditions. He then redesigned the scale — multiplying Rømer's degrees by approximately 4 and shifting the zero — to achieve finer graduation and a different zero point.

Unlikely. Rømer's scale had an awkward 7.5°Rø freezing point and a 52.5-degree span — not easy to memorize or subdivide cleanly. Celsius's 0-to-100 design was simpler, aligned with the decimal metric system sweeping Europe, and gained powerful institutional backing from Swedish and French academies. Fahrenheit's scale — partly derived from Rømer's — won in the English-speaking world largely due to British imperial reach. Rømer's real legacy is indirect: inspiring Fahrenheit, who then dominated for 250 years.

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