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dc.contributor.authorGibson, NP
dc.contributor.authorNokolov, N
dc.contributor.authorSing, DK
dc.contributor.authorBarstow, J
dc.contributor.authorEvans, TE
dc.contributor.authorKataria, T
dc.contributor.authorWilson, PA
dc.date.accessioned2017-03-06T14:41:20Z
dc.date.issued2017-0211
dc.description.abstractWe present transmission spectroscopy of the hot-Jupiter WASP-31b using FORS2 on the VLT during two primary transits. The observations cover a wavelength range of ≈400–840 nm. The light curves are corrupted by significant systematics, but these were to first order invariant with wavelength and could be removed using a commonmode correction derived from the white light curves. We reach a precision in the transit depth of ≈140 ppm in 15 nm bins, although the precision varies significantly over the wavelength range. Our FORS2 observations confirm the cloud-deck previously inferred using HST/STIS. We also re-analyse the HST/STIS data using a Gaussian process model, finding excellent agreement with earlier measurements. We reproduce the Rayleigh scattering signature at short wavelengths (. 5300 ˚A) and the cloud-deck at longer wavelengths. However, our FORS2 observations appear to rule out the large potassium feature previously detected using STIS, yet it is recovered from the HST/STIS data, although with reduced amplitude and significance (≈ 2.5σ). The discrepancy between our results and the earlier STIS detection of potassium (≈ 4.3σ) is either a result of telluric contamination of the ground-based observations, or an underestimate of the uncertainties for narrow-band features in HST/STIS when using linear basis models to account for the systematics. Our results further demonstrate the use of ground-based multi-object spectrographs for the study of exoplanet atmospheres, and highlight the need for caution in our interpretation of narrow-band features in low-resolution spectra of hot-Jupiters.en_GB
dc.description.sponsorshipThis work is based on observations collected at the European Organisation for Astronomical Research in the Southern Hemisphere under ESO programme 096.C-0765. N. P. G. gratefully acknowledges support from the Royal Society in the form of a University Research Fellowship. N. N, D. K. S, and T. M. E. acknowledge funding from the European Research Council under the European Unions Seventh Framework Programme (FP7/2007-2013) / ERC grant agreement no. 336792. J. K. B. is supported by a Royal Astronomical Society Research Fellowship. P.A.W. acknowledges the support of the French Agence Nationale de la Recherche (ANR), under program ANR-12-BS05-0012 ‘Exo-Atmos’. We are grateful to the developers of the NumPy, SciPy, Matplotlib, iPython and Astropy packages, which were used extensively in this work (Jones et al. 01 ; Hunter 2007; P´erez & Granger 2007; Astropy Collaboration et al. 2013).en_GB
dc.identifier.citationVol. 67 (4), pp. 4591-4605en_GB
dc.identifier.doi10.1093/mnras/stx353
dc.identifier.urihttp://hdl.handle.net/10871/26254
dc.language.isoenen_GB
dc.publisherOxford University Press (OUP) / Royal Astronomical Societyen_GB
dc.subjectmethods: data analysisen_GB
dc.subjectstars: individual (WASP-31)en_GB
dc.subjectplanetary systemsen_GB
dc.subjecttechniques: spectroscopicen_GB
dc.subjecttechniques: Gaussian processesen_GB
dc.titleVLT/FORS2 comparative transmission spectroscopy II: confirmation of a cloud-deck and Rayleigh scattering in WASP-31b, but no potassium?en_GB
dc.typeArticleen_GB
dc.identifier.issn1365-2966
dc.descriptionThis is the author accepted manuscript. The final version is available from OUP via the DOI in this record.en_GB
dc.identifier.journalMonthly Notices of the Royal Astronomical Societyen_GB


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