In this explanation what is changing is the altitude at which emission occurs, and at higher levels it is colder, so this level needs to warm up to maintain the radiative balance; what would happen once the altitude of
radiative emission reaches above the tropopause?
Not exact matches
RCP4.5 was updated from earlier GCAM scenarios to incorporate historical
emissions and land cover information common to the RCP process and follows a cost - minimizing pathway to
reach the target
radiative forcing.
In order to
reach such
radiative forcing levels, greenhouse gas
emissions (and indirectly
emissions of air pollutants) are reduced substantially, over time (Van Vuuren et al. 2007a).
whereF is radiant - energy flux at the emitting surface; εis emissivity, set at 1 for a blackbody that absorbs and emits all irradiance
reaching its emitting surface (by Kirchhoff's law of
radiative transfer, absorption and
emission are equal and simultaneous), 0 for a whitebody that reflects all irradiance, and (0, 1) for a graybody that partly absorbs / emits and partly reflects; and σ ≈ 5.67 x 10 — 8 is the Stefan - Boltzmann constant.