Bibcode
Parviainen, H.; Pallé, E.; Chen, G.; Nortmann, L.; Murgas, F.; Nowak, G.; Aigrain, S.; Booth, A.; Abazorius, M.; Iro, N.
Bibliographical reference
Astronomy and Astrophysics, Volume 609, id.A33, 16 pp.
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1
2018
Journal
Citations
19
Refereed citations
16
Description
Aims: We set out to study the atmosphere of WASP-80b, a warm
inflated gas giant with an equilibrium temperature of 800 K, using
ground-based transmission spectroscopy covering the spectral range from
520 to 910 nm. The observations allow us to probe the existence and
abundance of K and Na in WASP-80b's atmosphere, existence of
high-altitude clouds, and Rayleigh-scattering in the blue end of the
spectrum. Methods: We observed two spectroscopic time series of
WASP-80b transits with the OSIRIS spectrograph installed in the Gran
Telescopio Canarias (GTC), and use the observations to estimate the
planet's transmission spectrum between 520 nm and 910 nm in 20 nm-wide
passbands, and around the K I and Na I resonance doublets in 6 nm-wide
passbands. We jointly model three previously published broadband
datasets consisting of 27 light curves, prior to a transmission
spectroscopy analysis in order to obtain improved estimates of the
planet's orbital parameters, average radius ratio, and stellar density.
The parameter posteriors from the broadband analysis are used to set
informative priors on the transmission spectroscopy analysis. The final
transmission spectroscopy analyses are carried out jointly for the two
nights using a divide-by-white approach to remove the common-mode
systematics, and Gaussian processes to model the residual
wavelength-dependent systematics. Results: We recover a flat
transmission spectrum with no evidence of Rayleigh scattering or K I or
Na I absorption, and obtain an improved system characterisation as a
by-product of the broadband- and GTC-dataset modelling. The transmission
spectra estimated separately from the two observing runs are consistent
with each other, as are the transmission spectra estimated using either
a parametric or nonparametric systematics model. The flat transmission
spectrum favours an atmosphere model with high-altitude clouds over
cloud-free models with stellar or sub-stellar metallicities.
Conclusions: Our results disagree with the recently published discovery
of strong K I absorption in WASP-80b's atmosphere based on ground-based
transmission spectroscopy with FORS2 at VLT.
The analysis code with the raw and processed data are publicly available
through GitHub from http://https://github.com/hpparvi/Parviainen-2017-WASP-80b
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