T l2

where mw = ln[C^(T) /Cw] is the water vapour potential, Cw the concentration of water vapour in the atmosphere, and Cw = Cf(T) the concentration corresponding to its saturation value at the environmental temperature.

By summing Eqs. (4.3)-(4.5) and substituting the corresponding expressions for the fluxes qh and qw from Section 10.2 we obtain the general expression for the function of dissipation:

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