I'm trying to figure out what temperature actually is, and there seem to be a lot of answers floating around:
- average kinetic energy per degree of freedom
- a statistical parameter of the Boltzmann distribution
- partial derivative of energy with respect to entropy
- a unique parameter that governs the black body radiation an object emits
and any of these could be fine, except I have no idea how we could possible measure them (except maybe the first, but people generally seem to say that it's actually wrong).
That is, if I take a traditional, thermal-expansion-based thermometer and put it in contact with something, it measures something which corresponds to all of the definitions given above, which is constant at equilibrium, etc. It seems to measure "temperature".
But what is the physical process by which (for example) $\frac{\partial E}{\partial S}$ governs precisely how much the mercury will rise in a thermometer? Why do we believe that "temperature" (the thing a thermometer measures) corresponds so precisely to "temperature" (any of the four definitions given above)?
(and for that matter, if we take $\frac{\partial E}{\partial S}$ as a definition of temperature, how do we define $S$?)