Distribution in the Upper Atmosphere of Sodium Atoms Excited by Sunlight

Abstract
Calculation is made of the distribution of atoms excited to the P322 state by solar radiation, direct and reflected from the earth for a model sodium layer between 70 and 100 km. Account is taken of the attenuation by resonance absorption of sunlight in the layer before the solar photons reach a given point in the layer. This absorption grossly modifies the scattered intensity at twilight, causing minima to appear at about 5° solar depression and reducing greatly the difference in scattering for thicknesses between 2×109 cm2 and 2×1011 atoms/cm2 in late twilight. The effect of imprisonment, not included, is expected to modify only the late twilight results.

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