Photolytically generated aerosols in the mesosphere and thermosphere of Titan

Mao-Chang Liang; Yuk L. Yung; Donald E. Shemansky

doi:10.1086/518785

paper

Photolytically generated aerosols in the mesosphere and thermosphere of Titan

arXiv:0705.0145 · doi:10.1086/518785

Abstract

Analysis of the Cassini Ultraviolet Imaging Spectrometer (UVIS) stellar and solar occultations at Titan to date include 12 species: N $_{2}$ (nitrogen), CH $_{4}$ (methane), C $_{2}$ H $_{2}$ (acetylene), C $_{2}$ H $_{4}$ (ethylene), C $_{2}$ H $_{6}$ (ethane), C $_{4}$ H $_{2}$ (diacetylene), C $_{6}$ H $_{6}$ (benzene), C $_{6}$ N $_{2}$ (dicyanodiacetylene), C $_{2}$ N $_{2}$ (cyanogen), HCN (hydrogen cyanide), HC $_{3}$ N (cyanoacetylene), and aerosols distinguished by a structureless continuum extinction (absorption plus scattering) of photons in the EUV. The introduction of aerosol particles, retaining the same refractive index properties as tholin with radius $\sim$ 125 Åand using Mie theory, provides a satisfactory fit to the spectra. The derived vertical profile of aerosol density shows distinct structure, implying a reactive generation process reaching altitudes more than 1000 km above the surface. A photochemical model presented here provides a reference basis for examining the chemical and physical processes leading to the distinctive atmospheric opacity at Titan. We find that dicyanodiacetylene is condensable at $\sim$ 650 km, where the atmospheric temperature minimum is located. This species is the simplest molecule identified to be condensable. Observations are needed to confirm the existence and production rates of dicyanodiacetylene.

A typo in Table 1 was made in the previous version. The corrected tholin abundance is 4.6x10^11. ApJL in press. Will be published on June 1st, or May 21 online

Photolytically generated aerosols in the mesosphere and thermosphere of Titan

Abstract

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