Abstract

ABSTRACT We present a publicly available library of model atmospheres with radiative-convective equilibrium pressure–temperature (P-T) profiles fully consistent with equilibrium chemical abundances, and the corresponding emission and transmission spectrum with R ∼ 5000 at 0.2 µm decreasing to R ∼ 35 at 30 µm, for 89 hot Jupiter exoplanets, for four recirculation factors, six metallicities, and six C/O ratios. We find the choice of condensation process (local/rainout) alters the P-T profile and thereby the spectrum substantially, potentially detectable by James Webb Space Telescope. We find H− opacity can contribute to form a strong temperature inversion in ultrahot Jupiters for C/O ratios ≥ 1 and can make transmission spectra features flat in the optical, alongside altering the entire emission spectra. We highlight how adopting different model choices such as thermal ionization, opacities, line-wing profiles and the methodology of varying the C/O ratio, effects the P-T structure, and the spectrum. We show the role of Fe opacity to form primary/secondary inversion in the atmosphere. We use WASP-17b and WASP-121b as test cases to demonstrate the effect of grid parameters across their full range, while highlighting some important findings, concerning the overall atmospheric structure, chemical transition regimes, and their observables. Finally, we apply this library to the current transmission and emission spectra observations of WASP-121b, which shows H2O and tentative evidence for VO at the limb, and H2O emission feature indicative of inversion on the dayside, with very low energy redistribution, thereby demonstrating the applicability of library for planning and interpreting observations of transmission and emission spectrum.

Highlights

  • The thermal or the pressure-temperature (P-T) structure of a planetary atmosphere is a result of constant feedback between radiative, advective, and chemical processes

  • We investigate the effects of these two condensation approaches on the RCE P-T profiles and thereby the equilibrium chemical abundances, and transmission/emission spectra

  • In this work we create a library of radiative-convective equilibrium P-T profiles and corresponding equilibrium chemical abundances, transmission spectra, emission spectra and contribution functions, for a range of observationally significant exoplanets

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Summary

INTRODUCTION

The thermal or the pressure-temperature (P-T) structure of a planetary atmosphere is a result of constant feedback between radiative, advective, and chemical processes. In Goyal et al (2018), Goyal et al (2019a) and Goyal et al (2019b) we used isothermal P-T profiles and corresponding equilibrium chemical abundances for computing transmission spectra for a wide range of exoplanet atmospheres. RCE P-T profiles for different planets can vary depending on their gravity, host star distance and spectral type, circulation in the planet’s atmosphere and the chemical composition of the atmosphere This can lead to a wide range of possible spectra for a given planet, governed by its P-T profile. The implementation and validation of thermal ionization, H− and Fe opacity used in ATMO is detailed in Appendix A

MODEL DESCRIPTION
Computing P-T profiles in Radiative-Convective equilibrium
Recirculation factor
Contribution Function
NUMERICAL SETUP FOR THE GRID
Chemistry Setup
Opacity Setup
GRID PARAMETER SPACE
RESULTS
Comparing model simulations with rainout and local condensation
Effect of Thermal Ionisation
Effect of Fe opacity
Sensitivity to Grid Parameters
Effect of recirculation factor
Effect of Metallicity
WASP-17b
WASP-121b
INTERPRETING THE OBSERVATIONS OF WASP-121B
CONCLUSIONS
Sensitivity to Model Choices
General Conclusions
Thermal Ionization
Fe Absorption cross-sections
DECOUPLED EMISSION SPECTRUM
Comparing model simulations with different Na and K line wing profiles
Comparing model simulations with different VO line-list sources
Full Text
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