snorkack said:
And my point is that if the atmosphere of Venus were 100 % N2, but the same total pressure of 92 bar, Venus would be much cooler.
Obviously, if you change the composition of Venus' atmosphere, and remove the gases responsible for its greenhouse effect, a lower equilibrium atmospheric temperature should result, after the trapped heat is permitted to radiate into space. The trick is, getting rid of all that CO2.
So if Mars were warmer, would this cause large change in atmospheric composition and pressure as the polar ice caps evaporate into an atmosphere much denser than the existing one, and consisting mostly of water vapour?
The Martian atmosphere, what little there is, appears to be almost entirely CO2.
Since Mars no longer has a magnetosphere, the solar wind interacts directly with the upper atmosphere, stripping it away. There's nothing to indicate that the already ultra-low atmospheric pressure on the surface of Mars won't get lower over time.
If the Martian atmosphere did become thicker for some reason, this same process would gradually recur to strip gases from the upper atmosphere unless a means were found to replace the lost atmospheric mass.
Perhaps this is already occurring on Mars to some extent, and the atmosphere has reached a point of long-term stability. There appears to be plenty of water distributed in the crust of the planet outside of the polar regions.
The low atmospheric pressure on Mars indicates a low total atmospheric mass. CO2 on Mars is the same substance responsible for Venus' extreme climate conditions, but there is too little CO2 in Mars' atmosphere to trap sufficient solar radiation to warm it up much. (Mars gets only 43% of the solar radiation that Earth does due to its distance further from the sun.)