For the single-line greenhouse deficit, use hydrostatic balance, fixed surface pressure , constant gravity , and the dry adiabatThe gas constant and specific heat refer to the background gas. Let be the supplied effective ray cosine. The vertical optical depth and slant transmittance from level to space areThis permits pressure-dependent line widths. With local thermodynamic equilibrium, negligible infrared scattering, a black thermal surface, and no incident thermal radiation from space, the formal radiative transfer solution isThe weights add to one. Subtract the transparent-surface radiance and put , using the narrow-line approximation only in the line deficit. Define its pressure-dependent equivalent widthApproximating each hemispheric flux by times the effective-ray radiance preserves the black-surface flux. The outgoing longwave flux is thereforeIntegration by parts gives the particularly transparent formBoth boundary terms vanish: and . The dry adiabat and monotonic Planck function give . Atmospheric emission replaces part of the warm surface radiation by emission from cooler levels, reducing emission to space for a specified . The inequality is strict when opacity occurs over a nonzero range with temperature contrast; an isothermal absorbing layer at the surface temperature would not produce such a contrast.
For a spherical planet the mean absorbed instellation is . The required global energy balance isConsequently every equilibrium of this model has , with strict warming when . At fixed temperature profile, increasing increases and hence . This argument does not assume that the greenhouse gas changes the stellar-band albedo, surface pressure, or background thermodynamics; those are held fixed. For sufficiently broad or overlapping saturated wings the full frequency-dependent Planck function must replace the narrow-line approximation.
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