Temperature units and temperature scales
To put the measurement of temperature on a quantitative and objective basis, with sufficient accuracy we need an agreed temperature scale, units and reliable thermometers to work with.
Historically, the Fahrenheit scale was based on the melting point of ice at 32 °F and the boiling point of water at 212 °F, both at standard atmospheric pressure. Similarly, the Celsius (centigrade) scale used a ‘fundamental interval’ from 0 °C to 100 °C.
These units and scales are still used, but since 1954 the unit of temperature has been defined following a suggestion originally made by William Thomson, later Lord Kelvin, over 100 years earlier. The Kelvin scale.
What is the Kelvin scale based on?
When a material is cooled, it loses heat, and its temperature decreases. In principle this could continue until a point is reached where there is no more heat left to lose. This temperature is the absolute zero. Kelvin’s scale begins with the value zero at absolute zero and on this scale, water freezes at 273 degrees and boils at 373 degrees.
Since 1954 the unit for thermodynamic (absolute) temperature has been defined by assigning the value 273.16 kelvin to the triple point of water, the unique temperature at which the liquid, solid and vapour phases of pure water are in equilibrium.
All three temperature scales are related to each other.
Temperatures measured in degrees Celsius, use the definition that the temperature t in °C is the temperature T in kelvins minus 273.15:

Thus the triple point of water is both 273.16 K and 0.01 °C exactly.
Relative to Celsius temperatures, Fahrenheit temperatures are defined such that


