Resonance scattering by sodium in Mercury's atmosphere. I - The effect of phase and atmospheric smearing
The dependence of the intensity in the sodium D1 and D2 lines on the planetary phase and position of the disk is presented. Theoretical intensities are convolved with an atmospheric point spread function with FWHM of 0.5 and 2.0 arcsec for planetary phases 60 and 90 deg. It is shown that although the absolute intensities are extremely dependent on seeing, the I(D2)/I(D1) ratio remains a reliable indicator of column abundance regardless of the seeing function. For a uniform distribution of sodium, limb brightening will be apparent for a seeing disk with FWHM of 0.5 arcsec but will not be apparent for a FWHM of 2.0 arcsec.