The conversions

Kelvin to Celsius: °C = K − 273.15

Celsius to kelvin: K = °C + 273.15

Kelvin to Fahrenheit: °F = (K − 273.15) × 9/5 + 32

Kelvin and Celsius use degrees of exactly the same size — a change of one kelvin is a change of one degree Celsius. The only difference is where zero sits, which is why the conversion is pure addition with no multiplication. Fahrenheit needs the extra step because its degrees are a different size.

The anchors worth memorising

Kelvin has no intuitive landmarks, so three reference points do most of the work.

Everyday values on all three scales.
KelvinCelsiusFahrenheitWhat it is
0 K−273.15 °C−459.67 °FAbsolute zero
77 K−196 °C−321 °FLiquid nitrogen boils
184 K−89.2 °C−128.6 °FColdest air ever measured
195 K−78.5 °C−109 °FDry ice sublimes
255 K−18 °C0 °FDomestic freezer
273.15 K0 °C32 °FWater freezes
293 K20 °C68 °FComfortable room
310 K37 °C98.6 °FA hot summer day
373.15 K100 °C212 °FWater boils
5,778 KSurface of the Sun

The three to keep: 273 K freezing, 293 K room, 373 K boiling. Everything else can be worked out from them.

Why the scale exists

Celsius and Fahrenheit both put zero somewhere convenient — the freezing point of water, and a brine mixture respectively. Both choices are arbitrary as far as physics is concerned, and that arbitrariness makes them useless for anything involving ratios.

Kelvin puts zero at the bottom. Absolute zero is not a chosen reference point but the temperature at which there is no thermal energy left to remove, which makes kelvin values proportional to actual energy content.

The practical consequence: doubling a kelvin temperature doubles the thermal energy. Going from 10 °C to 20 °C doubles nothing, because the Celsius zero is not the bottom of anything. This is why the gas laws, radiation calculations and most of thermodynamics are written in kelvin — the arithmetic simply does not work otherwise.

Writing it correctly

The naming follows the convention for units named after people: lowercase when written out, capitalised as a symbol. The unit is named after William Thomson, Lord Kelvin, who worked out the absolute scale in 1848.

Everyday temperatures barely use it

The natural range at the Earth's surface runs from about 184 K to 330 K — a band about 150 kelvin wide, on a scale with no upper limit. Outdoor weather occupies a narrow slice around 273 K.

Which is why kelvin is a laboratory and engineering unit rather than a weather one. For everyday values the Celsius and Fahrenheit converter is the more useful tool, and for what sits at the cold end of the kelvin scale, the extreme cold scale puts dry ice, liquid nitrogen and absolute zero in order.