jacques-
I already said it was a bad analogy, what more do you want?
I'll try again. In a lifeless system, the total energy of the system will have a maximum potential, x. X= the sum total of all energy storage in all media and forms in the system, beyond which any excess energy must be shed in some way, typically radiated heat.
Using earth as an example, if there were no life forms on the planet, then x would be the maximum energy possible on the planet at any given time. This would include gravitationally induced heat at the core, radiactive elements, atmospheric heat, the kinetic energy of wind, the downward force of water from mountains, and heated surfaces from the sun, which do reach a maximum stored heat from a particular source based upon their albedo(reflectivity) and then radiate all further heat away from that source.
This is plain to see on Mercury. Mercury has reached a rather high mean temperature due to its proximity to the sun. Its sunward side is at a steady temperature that is hot enough that lead would form a puddle on it's surface. But it does not get any hotter. The surface is at a combination of temperature and albedo that has reached equilibrium. Unless the sun's output changes, the surface temp will stay the same. Should humans come and set up solar panels or mining operations, the albedo of Mercury will change, and so will its surface temperature. Meteor or cometary impacts could also change its equilibrium, but short of these events, Mercury is in static equilibrium.
Planets with atmosphere are normally in dynamic equilibrium, constantly changing local conditions, but overall global conditions are the same. Their net energy is always X though.
When life gets added to that equation, it changes it. Life takes energy out of the environment, allowing the planet to accept more energy, creating a small energy deficit in the system. Life gives this energy back as heat, but not all of it. Some ends up stored, as chemical heat. Gasoline, fat, oil, coal, all products of life. Earth had a huge energy storage before the Industrial Age, a significant fraction of which has now been radiated away as heat, which was used for heating and electrical generation. But even as we use it, more is being made, and we are learning to store more energy as well. Life is altering the energy balance of the earth.
Now this wasn't perfect either, but I hope I did better this time.
