The Hubble/ STIS near-ultraviolet transmission spectrum of HD 189733 b
Author
Cubillos, P.E.Fossati, L.
Koskinen, T.
Huang, C.
Sreejith, A.G.
France, K.
Wilson, Cauley, P.
Haswell, C.A.
Affiliation
Lunar and Planetary Laboratory, University of ArizonaIssue Date
2023-03-24Keywords
Planets and satellites: atmospheresPlanets and satellites: gaseous planets
Techniques: spectroscopic
Metadata
Show full item recordPublisher
EDP SciencesCitation
A&A 671, A170 (2023)Journal
Astronomy and AstrophysicsRights
© The Authors 2023. Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License.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
The benchmark hot Jupiter HD 189733 b has been a key target, used to lay out the foundations of comparative planetology for giant exo-planets. As such, HD 189733 b has been extensively studied across the electromagnetic spectrum. Here we report the observation and analysis of three transit light curves of HD 189733 b obtained with Hubble/STIS in the near-ultraviolet (NUV), the last remaining unexplored spectral window to be probed with present-day instrumentation for this planet. The NUV is a unique window for atmospheric mass-loss studies owing to the strong resonance lines and large photospheric flux. Overall, from a low-resolution analysis (R = 50) we found that the planet's NUV spectrum is well characterized by a relatively flat baseline, consistent with the optical-infrared transmission, plus two regions at ∼2350 and ∼2600 Å that exhibit a broad and significant excess absorption above the continuum. From an analysis at a higher resolution (R = 4700), we found that the transit depths at the core of the magnesium resonance lines are consistent with the surrounding continuum. We discarded the presence of Mg II absorption in the upper atmosphere at a ∼2- 4Ï confidence level, whereas we could place no significant constraint for Mg I absorption. These broad absorption features coincide with the expected location of Fe II bands; however, solar-abundance hydrodynamic models of the upper atmosphere are not able to reproduce the amplitude of these features with iron absorption. This scenario would require a combination of little to no iron condensation in the lower atmosphere super-solar metallicities and a mechanism to enhance the absorption features (such as zonal wind broadening). The true nature of this feature remains to be confirmed. © 2023 The Authors.Note
Open access articleISSN
0004-6361Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1051/0004-6361/202245064
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Except where otherwise noted, this item's license is described as © The Authors 2023. Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License.

