Convert any temperature into Celsius, Fahrenheit, Kelvin and Rankine at once. Absolute zero is enforced, formulas use your numbers, and reference charts cover freezing, body heat, boiling and oven settings.
Enter one value; all four scales appear in the result
Celsius and Fahrenheit are everyday relative scales; Kelvin and Rankine are absolute scales that start at absolute zero. This converter routes every input through kelvin so the four outputs stay consistent, then shows the algebra with the value you typed — not generic placeholders.
°C = (°F − 32) × 5/9 °F = °C × 9/5 + 32 K = °C + 273.15 °R = °F + 459.67 = K × 9/5 Absolute zero: 0 K = 0 °R = −273.15 °C = −459.67 °F
(98.6 − 32) × 5/9 = 37 °C. Kelvin = 37 + 273.15 = 310.15 K. Rankine = 98.6 + 459.67 = 558.27 °R.
−40 °C × 9/5 + 32 = −40 °F. The scales meet at that single point.
0 K = −273.15 °C = −459.67 °F = 0 °R. Anything colder is rejected.
| Landmark | °C | °F | K | °R |
|---|---|---|---|---|
| Absolute zero | -273.15 | -459.67 | 0 | 0 |
| Freezing point of water | 0 | 32 | 273.15 | 491.67 |
| Room temperature (≈20 °C) | 20 | 68 | 293.15 | 527.67 |
| Body temperature (37 °C) | 37 | 98.6 | 310.15 | 558.27 |
| Boiling point of water | 100 | 212 | 373.15 | 671.67 |
| Oven 180 °C | 180 | 356 | 453.15 | 815.67 |
| Oven 200 °C | 200 | 392 | 473.15 | 851.67 |
| Oven 220 °C | 220 | 428 | 493.15 | 887.67 |
| °C | °F | K | °R |
|---|---|---|---|
| -40 | -40 | 233.15 | 419.67 |
| -35 | -31 | 238.15 | 428.67 |
| -30 | -22 | 243.15 | 437.67 |
| -25 | -13 | 248.15 | 446.67 |
| -20 | -4 | 253.15 | 455.67 |
| -15 | 5 | 258.15 | 464.67 |
| -10 | 14 | 263.15 | 473.67 |
| -5 | 23 | 268.15 | 482.67 |
| 0 | 32 | 273.15 | 491.67 |
| 5 | 41 | 278.15 | 500.67 |
| 10 | 50 | 283.15 | 509.67 |
| 15 | 59 | 288.15 | 518.67 |
| 20 | 68 | 293.15 | 527.67 |
| 25 | 77 | 298.15 | 536.67 |
| 30 | 86 | 303.15 | 545.67 |
| 35 | 95 | 308.15 | 554.67 |
| 40 | 104 | 313.15 | 563.67 |
| 45 | 113 | 318.15 | 572.67 |
| 50 | 122 | 323.15 | 581.67 |
| 55 | 131 | 328.15 | 590.67 |
| 60 | 140 | 333.15 | 599.67 |
| 65 | 149 | 338.15 | 608.67 |
| 70 | 158 | 343.15 | 617.67 |
| 75 | 167 | 348.15 | 626.67 |
| 80 | 176 | 353.15 | 635.67 |
| 85 | 185 | 358.15 | 644.67 |
| 90 | 194 | 363.15 | 653.67 |
| 95 | 203 | 368.15 | 662.67 |
| 100 | 212 | 373.15 | 671.67 |
Related tools: Fahrenheit to Celsius Converter · Heat Index Converter · Wind Chill Converter.
Celsius (°C), Fahrenheit (°F), Kelvin (K) and Rankine (°R). Enter one value and unit; the page shows all four together with the working formula using your numbers.
Absolute zero is 0 K (also 0 °R), equal to −273.15 °C or −459.67 °F. Nothing can be colder; values below that threshold return a clear error instead of nonsense numbers.
The Celsius and Fahrenheit scales cross at −40. From °C to °F you multiply by 9/5 and add 32: (−40)×9/5 + 32 = −72 + 32 = −40. The same point appears in the −40 to 100 °C chart below.
Both are absolute scales starting at absolute zero. Rankine degrees are the same size as Fahrenheit degrees: °R = K × 9/5, and °R = °F + 459.67.
Kelvin is the SI unit for thermodynamic temperature. Gas laws, black-body radiation and most lab equations expect kelvin because ratios and differences stay physically meaningful from absolute zero.
Temperature scales use different zero points and step sizes, so they are **not** proportional like meters and feet. Treat conversions as affine transforms: multiply then add (or the inverse).
Celsius and Fahrenheit relate through a linear map with offset 32°F at freezing and a 9/5 slope between boiling and freezing spans. Kelvin shares Celsius-sized degrees but anchors at absolute zero. Because of the offset, **doubling** a Fahrenheit number has no physical meaning—always convert to a thermodynamic-friendly unit before reasoning about ratios.
°F = °C × 9/5 + 32; °C = (°F − 32) × 5/9; K = °C + 273.15.
Human body temperature near 37°C maps to 98.6°F via the affine formula—not by multiplying by a single conversion factor like length units.
Use the Temperature calculator: enter a value, choose the unit you are converting from and to, then read the equivalent. When comparing weather forecasts, stick to one scale per comparison so offsets do not confuse large versus small changes.
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