Abstract

Most planets currently amenable to transit spectroscopy are close enough to their host stars to exhibit a relatively strong day to night temperature gradient. For hot planets this leads to a chemical composition dichotomy between the two hemispheres. In the extreme case of ultra-hot Jupiters, some species, such as molecular hydrogen and water, are strongly dissociated on the day side while others, such as carbon monoxide, are not. However, most current retrieval algorithms rely on 1D forward models that are unable to reproduce this effect. We thus investigate how the 3D structure of the atmosphere biases the abundances retrieved using commonly used algorithms. We study the case of Wasp-121b as a prototypical ultra-hot Jupiter. We use the simulations of this planet 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 are then analyzed using the TauREx retrieval code. We find that the ultra-hot Jupiter transmission spectra exhibit muted H2O features that originate on the night side where the temperature, hence the scale-height, is smaller than on the day side. However, the spectral features of molecules present on the day side are boosted by both its high temperature and low mean molecular weight. As a result, the retrieved parameters are strongly biased compared to the ground truth. In particular the [CO]/[H2O] is overestimated by one to three orders of magnitude. This must be kept in mind when using the retrieval analysis to infer the C/O of a planet’s atmosphere. We also discuss whether indicators can allow us to infer the 3D structure of an observed atmosphere. Finally, we show that Wide Field Camera 3 fromHubbleSpace Telescope transmission data of Wasp-121b are compatible with the day–night thermal and compositional dichotomy predicted by models.

Highlights

  • Since the discovery of the first exoplanets, observations have shown a great diversity of objects, from Earth-like planets to ultra-hot Jupiters (UHJ)

  • We investigate whether the variations in composition inside the atmosphere of UHJs may affect transmission spectroscopy as severely as emission spectroscopy

  • We note that the TauREx retrieval code is not designed to take into account the thermal dissociation of H2

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Summary

Introduction

Since the discovery of the first exoplanets, observations have shown a great diversity of objects, from Earth-like planets to ultra-hot Jupiters (UHJ). We investigate whether the variations in composition inside the atmosphere of UHJs may affect transmission spectroscopy as severely as emission spectroscopy These tidally locked planets present a strong day–night contrast both in temperature (Sudarsky et al 2000; Bell & Cowan 2018; Arcangeli et al 2018) and in chemical heterogeneities due to the thermal dissociation of certain species such as H2 O and H2. Caldas et al (2019) highlighted systematic biases on retrieved temperatures using a 1D retrieval model TauREx (Waldmann et al 2015a,b) This earlier study only looked at atmospheres with a homogeneous composition to focus on thermal effects.

Presentation of our spectra generation and retrieval framework
Generation of transmission spectra with Pytmosph3R
Retrieval model
Input models: from simple case to GCM simulations
Effects of the day to night temperature gradient
Composition effects due to the dissociation of some molecules
Results
H2 and H2 O constant in the atmosphere
Thermal dissociation of H2 O with H2 constant
Thermal dissociation of H2 and H2 O
Discussions
Are there hints of 3D structures in real data?
Conclusion
Full Text
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