Thank you for the replies.
Hm DaleSpam interesting two posts!
A few questions: (if you don't have time for them all, then I'm also happy if you could just look at question 3
1) "So, basically we have just c doubling and the permittivity and permeability halving and no other changes." Well I suppose there could be more changes, right? Would it in principle suffice to check each of the dimensionless fundamental constants for a change?
2) So let's for a moment define meter as the length of a certain rod and a second in a similar way (earth's orbit or something). Now let L_c be the distance light travels in one second, expressed in meter. Now define \beta = \frac{L_c}{[L_c]}, then beta is a dimensionless number! It's equal to the amount of rods light passes in a certain fraction of Earth's orbit. What if say \beta' = 2 \beta? Surely this is an observational difference. So does that imply there must be a change in one of the 26(I think) fundamental dimensionless constants? I suppose it does, right? Because if it doesn't, then there wouldn't be an observational difference, although there certainly is. How do you know what dimensionless constants changed?
3) If I want to focus on changing k, does it mean that I have to find a dimensionless constant with k in it, so I know what has to change for it to be observable? The weird thing is, k has Kelvin as units (I mean, it has that unit in its unit), so there probably won't be any dimensionless constant for it! Unless N_A (Avog. number) = R/k can be seen as a dimensionless constant, but Baez didn't count it as one, and it might just be a definition? And if one argues "well then maybe k can't be involved in any observational difference", but surely that is wrong if we see PV = kNT => k = PV/NT. If I don't change the definitions involving the right hand side, then a change in k most definitely will be observational?