I have been struggling to get some kind of intuition about this definition.
Let's say some object is at some specific temperature, say 100 in some scale. So, temperature is defined as the rate of change in dE/dS of that object. Is it not true that nothing can stay at the same temperature without some input of energy (presumably it would otherwise naturally radiate and lose energy)? Now, for the temperature to remain constant and if the energy input equals the energy output doesn't dE = 0, which would make T = 0, which seems to be contradictory?
Am I making any sense here?
Hi PS, you seem to be viewing the derivative strictly in terms of ... well, in terms of the system taking an *actual* energy step dE, noticing that S changed by dS, and figuring out what its temperature is from those actual steps.
Try some analogies on other quantities for which the derivatives make sense. Tension in an elastic rope, for example, is F = dE/dx. Does that mean a rope that's not *actually in the process of stretching* doesn't have a tension ("there's no dx")? The slope of a mountainside is dy/dx. Does that mean the mountain-slope is only really there when you're climbing it, and ceases to be a slope when you stop? No.
A better way to think about it is from Zig's explanation. A real, macroscopic system, internally in thermal equilibrium, will have some stockpile of energy. That energy is almost-but-not-quite uniformly spread---the distribution jitters around a bit due to statistical fluctuations---and those statistical fluctuations correspond to entropy changes. So both of the quantities in the derivative---the dE and the dS---are being "explored" by various parts of the system, even if it's not losing net energy.
If you bring in another system and put it contact with the first one, you'll see that the statistical sloshing-around of energy can include both systems. But it's not obvious what that means---does the new system steal energy from the old one? Or donate it? Or do they basically keep (aside from temporary fluctuations) their initial energy stores?
This is a case where you can see an actual dE and an actual dS. Obviously the combined system will seek out a lower-entropy state; it'll try to increase the total entropy. You can convince yourself (try it!) that:
a) in a case where the new system has a larger dS/dE, the new system will have to donate energy to the old one in order to increase total entropy.
b) in a case where the new system has a smaller dS/dE, the new system will have to steal energy from the old one in order to increase total entropy.
So that's a nice way to see that this quantity "dS/dE" has the same behavior that we expect of a temperature---it's the thing that determines which direction heat flows.