High resolution spectroscopy of Pluto's atmosphere: detection of the 2.3 m CH bands and evidence for carbon monoxide
arXiv:1104.4312 · doi:10.1051/0004-6361/201116954
Abstract
The goal is to determine the composition of Pluto's atmosphere and to constrain the nature of surface-atmosphere interactions. We perform high--resolution spectroscopic observations in the 2.33--2.36 m range, using CRIRES at the VLT. We obtain (i) the first detection of gaseous methane in this spectral range, through lines of the + and + bands (ii) strong evidence (6- confidence) for gaseous CO in Pluto. For an isothermal atmosphere at 90 K, the CH and CO column densities are 0.75 and 0.07 cm-am, within factors of 2 and 3, respectively. Using a physically--based thermal structure model of Pluto's atmosphere also satisfying constraints from stellar occultations, we infer CH and CO mixing ratios q= 0.6% (consistent with results from the 1.66 m range) and q = 0.5. The CO atmospheric abundance is consistent with its surface abundance. As for Triton, it is probably controlled by a thin, CO-rich, detailed balancing layer resulting from seasonal transport and/or atmospheric escape.
Astronomy and Astrophysics Letters, in press
References in corpus (3)
- Pluto's lower atmosphere structure and methane abundance from high-resolution spectroscopy and stellar occultations
- Detection of CO in Triton's atmosphere and the nature of surface-atmosphere interactions
- Near-Infrared Spectral Monitoring of Triton with IRTF/SpeX II: Spatial Distribution and Evolution of Ices
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