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part 2: thermodynamic duo
2

distribution processes and their thermodynamic description.
distribution processes and their thermodynamic description.

- distribution processes and their thermodynamic and kinetic description.
distribution processes and their thermodynamic description.

and of course, ecsv = acsv if in local thermodynamic equilibrium.
and of course, ecsv = acsv if in local thermodynamic equilibrium.

this is not unusual, either in earth history, or in thermodynamic systems.
this is certainly not the place.

sea surface temps would probably correspond better to the idea of surface as you use it in you thermodynamic view.
sea surface temps would probably correspond better to the idea of surface as you use it in you thermodynamic view.

... in other words, it would help if you learned the underlying microscopic processes that give rise to thermodynamic properties and laws.
... in other words, it would help if you learned the underlying microscopic processes that give rise to thermodynamic properties and laws.

of course, the absorptivity of the layer is equal to the emissivity of the layer (local thermodynamic equilibrium)
of course, the absorptivity of the layer is equal to the emissivity of the layer (local thermodynamic equilibrium)

at local thermodynamic equilibrium, emmissivity = absorptivity (at each location and time, direction, and wavelength).
at local thermodynamic equilibrium, emmissivity = absorptivity (at each location and time, direction, and wavelength).

1. assume local thermodynamic equilibrium, at least below some height level (that is at least above the tropopause).
1. assume local thermodynamic equilibrium, at least below some height level (that is at least above the tropopause).

http://skepticalscience.com/the-2nd-law-of-thermodynamics-and-the-greenhouse-effect.html
http://skepticalscience.com/translation.php?a=1&l=2