17 Modeling Global Warming Computer modeling is complicated by the Earth's feedback processes that sometimes make it necessary to use different
equations under changing simulated environments.
Shaw, S. & Riha, S. J. Assessing temperature - based PET
equations under a changing climate in temperate, deciduous forests.
By badly, I mean totally wrong — moreover, the slight decline is well understood by the solution to the diffusion
equation under changing stimulus.
Not exact matches
If so, then the Stefan - Boltzmann
equation applied to the observed temperature
change (and projected temperature
change under double CO2) should approximately tell you the total forcing incorporating climate system feedbacks?
Therefore, the August - Roche - Magnus
equation implies that saturation water vapor pressure
changes approximately exponentially with temperature
under typical atmospheric conditions, and hence the water - holding capacity of the atmosphere increases by about 7 % for every 1 °C rise in temperature.
Furthermore, it can be seen from the thermodynamic constraints embodied in the first
equation that the effects of condensation on the horizontal pressure gradient (in the particular case
under consideration) are always tied to the latent heat term ξ, not the volume
change term γ alone; that is, γ is always multiplied by ξ.