Titan's atmosphere as observed by Cassini/VIMS solar occultations: CH, CO and evidence for CH absorption
arXiv:1405.6324 · doi:10.1016/j.icarus.2014.10.004
Abstract
We present an analysis of the VIMS solar occultations dataset, which allows us to extract vertically resolved information on the characteristics of Titan's atmosphere between 100-700 km with a characteristic vertical resolution of 10 km. After a series of data treatment procedures, 4 occultations out of 10 are retained. This sample covers different seasons and latitudes of Titan. The transmittances show clearly the evolution of the haze and detect the detached layer at 310 km in Sept. 2011 at mid-northern latitudes. Through the inversion of the transmission spectra with a line-by-line radiative transfer code we retrieve the vertical distribution of CH and CO mixing ratio. The two methane bands at 1.4 and 1.7 μm are always in good agreement and yield an average stratospheric abundance of %. This is significantly less than the value of 1.48% obtained by the GCMS/Huygens instrument. The analysis of the residual spectra after the inversion shows that there are additional absorptions which affect a great part of the VIMS wavelength range. We attribute many of these additional bands to gaseous ethane, whose near-infrared spectrum is not well modeled yet. Ethane contributes significantly to the strong absorption between 3.2-3.5 μm that was previously attributed only to C-H stretching bands from aerosols. Ethane bands may affect the surface windows too, especially at 2.7 μm. Other residual bands are generated by stretching modes of C-H, C-C and C-N bonds. In addition to the C-H stretch from aliphatic hydrocarbons at 3.4 μm, we detect a strong and narrow absorption at 3.28 μm which we tentatively attribute to the presence of PAHs in the stratosphere. C-C and C-N stretching bands are possibly present between 4.3-4.5 μm. Finally, we obtain the CO mixing ratio between 70-170 km. The average result of ppm is in good agreement with previous studies.
arXiv comment51 pages, 28 figures
References in corpus (2)
Cited by in corpus (18)
- Titan's Atmosphere and Climate
- Titan solar occultation observations reveal transit spectra of a hazy world
- Empirical line lists and absorption cross sections for methane at high temperature
- Seasonal evolution of , , and abundances in Titan's lower stratosphere
- Exploring and Validating Exoplanet Atmospheric Retrievals with Solar System Analog Observations
- Assessment of Isoprene as a Possible Biosignature Gas in Exoplanets with Anoxic Atmospheres
- The Transit Transmission Spectrum of a Cold Gas Giant Planet
- Titan Science with the James Webb Space Telescope (JWST)
- Detectability of biosignatures on LHS 1140 b
- Seasonal evolution of temperatures in Titan's lower stratosphere
- Distribution and intensity of water ice signature in south Xanadu and Tui Regio
- The 3.4 μm absorption of the Titan's stratosphere: contribution of ethane, propane, butane and complex hydrogenated organics
- Retrieval of Chemical Abundances in Titan's Upper Atmosphere from Cassini UVIS Observations with Pointing Motion
- Cloud and Haze Parameterization in Atmospheric Retrievals: Insights from Titan's Cassini Data and JWST Observations of Hot Jupiters
- Transparency of 2 μm window of Titan's atmosphere
- Modeling transmission windows in Titan's lower troposphere: Implications for infrared spectrometers aboard future aerial and surface missions
- The Detection-vs-Retrieval Challenge: Titan as an Exoplanet
- Science goals and new mission concepts for future exploration of Titan's atmosphere geology and habitability: Titan POlar Scout/orbitEr and In situ lake lander and DrONe explorer (POSEIDON)