Subproject C2 aims at determining entropy and
enthalpy differences between different multivalently binding systems, using the conformation dynamics approach.
Not exact matches
(The
difference between zero and non-zero heat capacity responses is proportional to a radiative imbalance, which is proportional to the rate of change in
enthalpy and thus temperature, barring a change in where the heat is going, etc..)
«SOI representing a pressure differential - > VdP» So you are effectively taking the pressure
difference between two geographic points and using it as a pressure increment applied to the whole atmosphere (whose volume you consider constant) as a change in
enthalpy.
All that is needed is to add heat carried upwards past the denser atmosphere (and most CO2) by convection and the latent heat from water changing state (the majority of heat transport to the tropopause), the albedo effects of clouds, the inability of long wave «downwelling» (the blue balls) to warm water that makes up 2 / 3rds of the Earth's surface, and that due to huge
differences in
enthalpy dry air takes far less energy to warm than humid air so temperature is not a measure of atmospheric heat content.