Journal
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 488, Issue 2, Pages 2222-2234Publisher
OXFORD UNIV PRESS
DOI: 10.1093/mnras/stz1753
Keywords
techniques: spectroscopic; planets and satellites: atmospheres
Categories
Funding
- NASA [NAS 5-26555]
- Space Telescope Science Institute
- Leverhulme Trust
- University of Exeter PhD Studentship - UK Science and Technology Facilities Council (STFC) studentship
- STFC Consolidated Grant [ST/R000395/1]
- European Research Council
- [ATMO 757858]
- STFC [1784036, ST/J001627/1, ST/R000395/1] Funding Source: UKRI
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WASP-121b is a transiting gas giant exoplanet orbiting close to its Roche limit, with an inflated radius nearly double that of Jupiter and a dayside temperature comparable to a late M dwarf photosphere. Secondary eclipse observations covering the 1.1-1.6 mu m wavelength range have revealed an atmospheric thermal inversion on the dayside hemisphere, likely caused by high-altitude absorption at optical wavelengths. Here we present secondary eclipse observations made with the Hubble Space Telescope Wide Field Camera 3 spectrograph that extend the wavelength coverage from 1.1 mu m down to 0.8 mu m. To determine the atmospheric properties from the measured eclipse spectrum, we performed a retrieval analysis assuming chemical equilibrium, with the effects of thermal dissociation and ionization included. Our best-fitting model provides a good fit to the data with reduced chi(2)(nu) = 1.04. The data diverge from a blackbody spectrum and instead exhibit emission due to H- shortward of 1.1 mu m. The best-fitting model does not reproduce a previously reported bump in the spectrum at 1.25 mu m, possibly indicating this feature is a statistical fluctuation in the data rather than a VO emission band as had been tentatively suggested. We estimate an atmospheric metallicity of [M/H] = 1.09(-0.69)(+0.57), and fit for the carbon and oxygen abundances separately, obtaining [C/H] = -0.29(-0.48)(+0.61) and [O/H] = 0.18(-0.60)(+0.64). The corresponding carbon-to-oxygen ratio is C/O = 0.49(-0.37)(+0.65), which encompasses the solar value of 0.54, but has a large uncertainty.
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