Rankine to Celsius

Bookmark Page Celsius to Rankine (Swap Units)


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℃ =
ºR - 491.67
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More information: Celsius
Rankine to Celsius table - Click here for table options
Rankine Celsius
0ºR -273.15
1ºR -272.59
2ºR -272.04
3ºR -271.48
4ºR -270.93
5ºR -270.37
6ºR -269.82
7ºR -269.26
8ºR -268.71
9ºR -268.15
10ºR -267.59
11ºR -267.04
12ºR -266.48
13ºR -265.93
14ºR -265.37
15ºR -264.82
16ºR -264.26
17ºR -263.71
18ºR -263.15
19ºR -262.59
Rankine Celsius
20ºR -262.04
21ºR -261.48
22ºR -260.93
23ºR -260.37
24ºR -259.82
25ºR -259.26
26ºR -258.71
27ºR -258.15
28ºR -257.59
29ºR -257.04
30ºR -256.48
31ºR -255.93
32ºR -255.37
33ºR -254.82
34ºR -254.26
35ºR -253.71
36ºR -253.15
37ºR -252.59
38ºR -252.04
39ºR -251.48
Rankine Celsius
40ºR -250.93
41ºR -250.37
42ºR -249.82
43ºR -249.26
44ºR -248.71
45ºR -248.15
46ºR -247.59
47ºR -247.04
48ºR -246.48
49ºR -245.93
50ºR -245.37
51ºR -244.82
52ºR -244.26
53ºR -243.71
54ºR -243.15
55ºR -242.59
56ºR -242.04
57ºR -241.48
58ºR -240.93
59ºR -240.37
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A ºF version of the Kelvin scale. Based upon the definitions of the Fahrenheit scale and the experimental evidence that absolute zero is -459.67ºF

℃ =
ºR - 491.67


Although initially defined by the freezing point of water (and later the melting point of ice), the Celsius scale is now officially a derived scale, defined in relation to the Kelvin temperature scale.

Zero on the Celsius scale (0℃) is now defined as the equivalent to 273.15K, with a temperature difference of 1 deg C equivalent to a difference of 1K, meaning the unit size in each scale is the same. This means that 100℃, previously defined as the boiling point of water, is now defined as the equivalent to 373.15K.

The Celsius scale is an interval system but not a ratio system, meaning it follows a relative scale but not an absolute scale. This can be seen because the temperature interval between 20℃ and 30℃ is the same as between 30℃ and 40℃, but 40℃ does not have twice the air heat energy of 20℃.

A temperature difference of 1 deg C is the equivalent of a temperature difference 1.8°F.

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