Not exact matches
This microwave
radiation virtually freely penetrates into the lower atmosphere, providing channels
for the influence of solar variability on
terrestrial phenomena.
His research has been closely aligned with the development of increasingly sophisticated satellite platform measurements, such as the
terrestrial radiation budget, ozone and weather - related data, and the need
for increasingly sophisticated atmospheric models to assess and evaluate the information content and utility of these measurements.
That is determined by consideration of the absorption of the atmosphere of
terrestrial radiation (and
radiation emitted by the atmosphere), which essentially ends up determining at what altitude the temperature has to be determined via radiative balance between the Earth system (earth + atmosphere) and the sun and space [which
for the earth system with its current albedo is ~ 255 K].
If you accept diurnal variation as a proxy
for net absorption, since the quantum mechanical effect of absorption is to heat the air, then you can see from Fig. 2 that most of the net absorption occurs below 850 mb and that above 500 mb the tiny amount of net absorption slowly increases showing that it is the result of the absorption of solar not
terrestrial radiation.
When the energy enters and leaves the
terrestrial system, it must be in the form of electromagnetic
radiation, since space is a vacuum and does not provide a medium
for other types of energy transfer (Pierrehumbert 2011).
He then calculates natural sky
radiation for varying
Terrestrial conditions, varying from the Antarctic plateau (high elevation, low temperature, humidity and pressure) to the tropics (high humidity).
The real reasons
for climate changes are uneven solar
radiation,
terrestrial precession (that is, axis gyration), instability of oceanic currents, regular salinity fluctuations of the Arctic Ocean surface waters, etc..