DETECTION OF H2O AND EVIDENCE FOR TiO/VO IN AN ULTRA-HOT EXOPLANET ATMOSPHERE
Author
Evans, Thomas M.Sing, David K.
Wakeford, H. R.
Nikolov, Nikolay
Ballester, Gilda E.
Drummond, B.
Kataria, Tiffany
Gibson, Neale P.
Amundsen, David S.
Spake, Jessica
Affiliation
Univ Arizona, Lunar & Planetary LabIssue Date
2016-04-21Keywords
planets and satellites: atmospheresstars: individual (WASP-121)
techniques: photometric
techniques: spectroscopic
Metadata
Show full item recordPublisher
IOP PUBLISHING LTDCitation
DETECTION OF H2O AND EVIDENCE FOR TiO/VO IN AN ULTRA-HOT EXOPLANET ATMOSPHERE 2016, 822 (1):L4 The Astrophysical Journal LettersRights
© 2016. The American Astronomical Society. All rights reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We present a primary transit observation for the ultra-hot (T-eq similar to 2400 K) gas giant expolanet WASP-121b, made using the Hubble Space Telescope Wide Field Camera 3 in spectroscopic mode across the 1.12-1.64 mu m wavelength range. The 1.4 mu m water absorption band is detected at high confidence (5.4 sigma) in the planetary atmosphere. We also reanalyze ground-based photometric light curves taken in the B, r', and z' filters. Significantly deeper transits are measured in these optical bandpasses relative to the near-infrared wavelengths. We conclude that scattering by high-altitude haze alone is unlikely to account for this difference and instead interpret it as evidence for titanium oxide and vanadium oxide absorption. Enhanced opacity is also inferred across the 1.12-1.3 mu m wavelength range, possibly due to iron hydride absorption. If confirmed, WASP-121b will be the first exoplanet with titanium oxide, vanadium oxide, and iron hydride detected in transmission. The latter are important species in M/L dwarfs and their presence is likely to have a significant effect on the overall physics and chemistry of the atmosphere, including the production of a strong thermal inversion.ISSN
2041-8213Version
Final published versionSponsors
The authors would like to thank the referee for their prompt and thoughtful review. This work is based on observations made with the NASA/ESA Hubble Space Telescope, obtained at the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., under NASA contract NAS 5-26555. These observations are associated with program GO-14468. The authors are grateful to the WASP-121 discovery team for generously providing the ground-based photometric light curves. The research leading to these results received funding from the European Research Council under the European Union Seventh Framework Program (FP7/2007-2013) ERC grant agreement no. 336792. H.R.W. acknowledges support by an appointment to the NASA Postdoctoral Program at Goddard Space Flight Center, administered by ORAU and USRA through a contract with NASA. N.P.G. gratefully acknowledges support from the Royal Society in the form of a University Research Fellowship.Additional Links
http://stacks.iop.org/2041-8205/822/i=1/a=L4?key=crossref.72557cd537c4ccc96ffe7b3f88f6018cae974a485f413a2113503eed53cd6c53
10.3847/2041-8205/822/1/L4
