Carbon-rich Giant Planets: Atmospheric Chemistry, Thermal Inversions, Spectra, and Formation conditions
Nikku Madhusudhan (Princeton), Olivier Mousis (CNRS, France), Torrence, V. Johnson (NASA JPL), Jonathan I. Lunine (Cornell)

TL;DR
This paper explores the atmospheric chemistry, spectral signatures, and formation conditions of carbon-rich giant planets, highlighting how high C/O ratios influence observable features and challenge existing models of planetary atmospheres.
Contribution
It provides a detailed analysis of the chemistry and spectra of carbon-rich giant planets and discusses formation scenarios that lead to high C/O ratios in their atmospheres.
Findings
High C/O ratios cause depletion of H2O and TiO/VO in atmospheres.
Spectral signatures of CRPs differ significantly from solar composition planets.
High C/O ratios can explain the lack of thermal inversions in some hot Jupiters.
Abstract
The recent inference of a carbon-rich atmosphere, with C/O >= 1, in the hot Jupiter WASP-12b motivates the exotic new class of carbon-rich planets (CRPs). We report a detailed study of the atmospheric chemistry and spectroscopic signatures of carbon-rich giant planets (CRGs) and the compositions of icy planetesimals required for their formation, and the apportionment of ices, rock, and volatiles in their envelopes. For C/O >= 1, most of the atmospheric oxygen is occupied by CO for T > 1400 K and pressure (P) < 1 bar, causing a substantial depletion in H2O, and an overabundance of CH4 compared to those obtained by assuming solar abundances (C/O = 0.54) in chemical equilibrium. These differences in chemistry cause distinctly observable signatures in spectra. We also find that a C/O >= 1 strongly depletes the abundances of TiO and VO available to form thermal inversions, which is adequate…
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