The Trenberth energy flux diagram of the radiative-convective model for global climate change shows incoming solar radiation (ISR) being dissipated as longer wavelength black body radiation emitted from the global surface, then from the top of the atmosphere (OLR). These energy fluxes may be recycled as heat by greenhouse gases like water and CO2 before eventual longwave emission to space. Increasing levels of greenhouse gases like CO2 and thus water force rises in tropospheric temperature, a function of global surface heat capacity. This model is linked to the meteorology of the atmosphere to determine effects on climate and extreme weather. Climate modelling has only a minor role for chemical thermodynamics and even less for quantum theory. To rectify this, we have introduced action mechanics, allowing several new developments.
The Carnot cycle estimates maximum efficiency of heat engines [1], where absorption of radiative heat with no cyclic change in temperature of a working fluid requires an efficient transition to work. Reversible transfers of heat to vortical or gravitational work followed by turbulent heat release is predicted to control rises in temperature, if greenhouse gases increase. Predicted variations in heat capacity may require the need for climate management of extreme weather. Some means of testing this new thermodynamic hypothesis from its predictions will be discussed.