JpGU-AGU Joint Meeting 2020

Presentation information

[E] Poster

P (Space and Planetary Sciences ) » P-AE Astronomy & Extrasolar Bodies

[P-AE22] Exoplanets

convener:Masahiro Ikoma(Department of Earth and Planetary Science, The University of Tokyo), Norio Narita(The University of Tokyo), Yuka Fujii(National Astronomical Observatory of Japan)

[PAE22-P07] WASP-76 b: A Tale of Two Spectra

*Billy Nelson Edwards1, Quentin Changeat1, Robin Baeyens2, Angelos Tsiaras1, Ingo Waldmann1 (1.University College London , 2.Instituut voor Sterrenkunde, KU-Leuven)

Keywords:Transmission and emission spectroscopy, Ultra-hot Jupiters, Hubble Space Telescope

The Hubble Space Telescope’s Wide Field Camera 3 (WFC3) has been widely used for transmission and emission spectroscopy of exoplanet atmospheres, identifying the main molecular constituents, detecting the presence of clouds and probing their thermal structure. Hubble observations of the emission spectra of a number of ultra-hot Jupiters have led to somewhat surprising results. Initially, these very hot planets were predicted to have inverted temperature pressure profiles due to strong optical absorption by TiO/VO in the upper atmospheres. However, observations of their emission spectra have been inconclusive on their thermal structure and composition. While some datasets show rich spectral features, others can be fit with simple blackbody models.

I will present the analysis of the Hubble transmission and emission spectra of WASP-76 b, an ultra-hot Jupiter with a day-side temperature of ~2500 K. The data was reduced and fitted using the open-source codes Iraclis and TauREx3. Previous studies of the WFC3 transmission spectra of WASP-76 b found hints of TiO and VO or non-grey clouds. Accounting for a fainter stellar companion to WASP-76, we reanalyse this data and show that removing the effects of this background star changes the slope of the spectrum, resulting in these visible absorbers no longer being detected, removing the need for a non-grey cloud model to adequately fit the data but maintaining the strong water feature previously seen. However, our analysis of the emission spectrum suggests the presence of vanadium oxide (VO) and an atmospheric thermal inversion, with tentative evidence for titanium oxide (TiO) and a muted water (H2O) feature.