Abstract

Hot Jupiters (HJs) are very good targets for transmission spectroscopy analysis. Their atmospheres have a large scale height, implying a high signal-to-noise ratio. As these planets orbit close to their stars, they often present strong thermal and chemical heterogeneities between the day- and nightside of their atmosphere. For the hottest of these planets, the thermal dissociation of several species occurs in their atmospheres, which leads to a stronger chemical dichotomy between the two hemispheres. It has already been shown that the current retrieval algorithms, which are using 1D forward models, find biased molecular abundances in ultrahot Jupiters. Here, we quantify the effective temperature domain over which these biases are present. We used a set of 12 simulations of typical HJs fromTeq= 1000 K toTeq= 2100 K performed with the substellar and planetary atmospheric radiation and circulation global climate model and generate transmission spectra that fully account for the 3D structure of the atmosphere with Pytmosph3R. These spectra were then analyzed using the 1D TauREx retrieval code. We find that forJames WebbSpace Telescope like data, accounting for nonisothermal vertical temperature profiles is required over the whole temperature range. We further find that 1D retrieval codes start to estimate incorrect parameter values for planets with equilibrium temperatures greater than 1400 K if there are absorbers in the visible (such as TiO and VO, e.g.) that are able to create a hot stratosphere. The high temperatures at low pressures indeed entail a thermal dissociation of species that creates a strong chemical day-night dichotomy. As a byproduct, we demonstrate that when synthetic observations are used to assess the detectability of a given feature or process using a Bayesian framework (e.g., by comparing the Bayesian evidence of retrievals with different model assumptions), it is valid to use nonrandomized input data as long as the anticipated observational uncertainties are correctly taken into account.

Highlights

  • Transmission spectroscopy enables detecting molecules in exoplanetary atmospheres, measuring molecular abundances, or setting upper limits on them

  • We used a set of 12 simulations of typical Hot Jupiters (HJs) from Teq = 1000 K to Teq = 2100 K performed with the substellar and planetary atmospheric radiation and circulation global climate model and generate transmission spectra that fully account for the 3D structure of the atmosphere with Pytmosph3R

  • For ultrahot Jupiters (UHJs), Pluriel et al (2020b) demonstrated that [CO]/[H2O]estimated with 1D spherically symmetric models can be different by several orders of magnitude because of strong day-to-night heterogeneities: H2O is thermally dissociated on the hot dayside, while it is not on the cool nightside

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Summary

Introduction

Transmission spectroscopy enables detecting molecules in exoplanetary atmospheres, measuring molecular abundances, or setting upper limits on them. The CO abundance remains constant everywhere because the temperature is not high enough in any location for CO to be thermally dissociated For these planets, transmission spectra are the combined result of hot regions in the CO bands and cold regions in the H2O bands. A&A 658, A42 (2022) perature regions where 1D spherically symmetric models can be safely used and where they should not be used for the purpose of estimating physical and chemical parameters To investigate this limit, we have designed and carried out a numerical experiment to identify the origin of the biases and to quantify them. We use TauREx (Waldmann et al 2015) to solve the inverse problem with a 1D forward model and estimate the parameters of interest We refer to this last part as the retrieval process or retrieval for short because we investigate whether correct parameter values are retrieved from the synthetic data.

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