While gas is launched out of the quasar at very high temperatures, there is enough time for some of it to cool
through radiative cooling — similar to how the Earth cools down on a cloudless night
Not exact matches
Physicists have achieved record temperature reductions of more than 40 °C using
radiative cooling, which beams heat
through the atmosphere
ENSO events, for example, can warm or
cool ocean surface temperatures
through exchange of heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the distribution and extent of cloud cover (which influences the
radiative balance in the lower atmosphere).
ENSO events, for example, can warm or
cool ocean surface temperatures
through exchange of heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the distribution and extent of cloud cover (which influences the
radiative balance in the lower atmosphere).
The troposphere is currently
cooling radiatively at about 2K / day, and adding CO2 to the atmosphere generally increases the
radiative cooling (primarily
through increases in water vapor, though how these details play out also depend on the details of the surface budget).
But the troposphere can still warm with an increased
radiative cooling term because it is also balanced by heating
through latent heat release, subsidence, solar absorption, increased IR flux from the surface, etc..
Even parabolic troughs might run
radiative cooling through pipes placed halfway between the collector vacuum pipes and the mirror surface since these pipes would see
cool portions of the sky not occupied by the Sun.
Absent
radiative warming it will still warm
through conduction and convection and it will
cool radiatively because all matter above absolute zero radiates and I'm pretty sure the nitrogen in our atmosphere is matter and it has a temperature above absolute zero therefore it radiates a continuous black body spectrum characteristic of that temperature.
For example, removing dark boreal forests primarily leads to global
cooling through the
radiative effects of increasing local albedo [21 — 23].
1) Mr Squid says the atmosphere in the dark side slows the rate of
cooling and not
through a
radiative process.
While the atmosphere on the «dark» side does indeed slow the rate of
cooling, it doesn't do so
through it's
radiative processes.