Greenhouse gases don't block
all outgoing radiant energy — it merely slows it down by capturing more infrared photons and re-emitting in all directions including down — increasing net energy retained at any instant in the atmosphere.
I'm not aware that it is common knowledge that MODTRAN programs can calculate the change in
outgoing radiant energy as a function of a change in surface temperature, all other factors held constant.
It is the density, not the composition which gives more or less opportunities for such instances of energy transfer between molecules whilst the incoming and
outgoing radiant energy is negotiating the atmosphere.
Not exact matches
The time scales involved remain miniscule on the level of an individual molecule BUT on a planetary scale they become highly significant and build up to a measurable delay between arrival of solar
radiant energy and its release to space as
outgoing radiation.
Cloud and Earth's
Radiant Energy System (CERES) instruments aboard NASA satellites measure incoming and outgoing radiant power at the top of the atmo
Radiant Energy System (CERES) instruments aboard NASA satellites measure incoming and
outgoing radiant power at the top of the atmo
radiant power at the top of the atmosphere.