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Grant_2023_ApJL_956_L29.pdf
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Author
Grant, D.Lewis, N.K.
Wakeford, H.R.
Batalha, N.E.
Glidden, A.
Goyal, J.
Mullens, E.
MacDonald, R.J.
May, E.M.
Seager, S.
Stevenson, K.B.
Valenti, J.A.
Visscher, C.
Alderson, L.
Allen, N.H.
Cañas, C.I.
Colón, K.
Clampin, M.
Espinoza, N.
Gressier, A.
Huang, J.
Lin, Z.
Long, D.
Louie, D.R.
Peña-Guerrero, M.
Ranjan, S.
Sotzen, K.S.
Valentine, D.
Anderson, J.
Balmer, W.O.
Bellini, A.
Hoch, K.K.W.
Kammerer, J.
Libralato, M.
Mountain, C.M.
Perrin, M.D.
Pueyo, L.
Rickman, E.
Rebollido, I.
Sohn, S.T.
van der Marel, R.P.
Watkins, L.L.
Affiliation
Lunar and Planetary Laboratory, Department of Planetary Sciences, University of ArizonaIssue Date
2023-10-16
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American Astronomical SocietyCitation
David Grant et al 2023 ApJL 956 L29Journal
Astrophysical Journal LettersRights
© 2023. The Author(s). Published by the American Astronomical Society. Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence.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
Clouds are prevalent in many of the exoplanet atmospheres that have been observed to date. For transiting exoplanets, we know if clouds are present because they mute spectral features and cause wavelength-dependent scattering. While the exact composition of these clouds is largely unknown, this information is vital to understanding the chemistry and energy budget of planetary atmospheres. In this work, we observe one transit of the hot Jupiter WASP-17b with JWST’s Mid-Infrared Instrument Low Resolution Spectrometer and generate a transmission spectrum from 5 to 12 μm. These wavelengths allow us to probe absorption due to the vibrational modes of various predicted cloud species. Our transmission spectrum shows additional opacity centered at 8.6 μm, and detailed atmospheric modeling and retrievals identify this feature as SiO2(s) (quartz) clouds. The SiO2(s) clouds model is preferred at 3.5-4.2σ versus a cloud-free model and at 2.6σ versus a generic aerosol prescription. We find the SiO2(s) clouds are composed of small ∼0.01 μm particles, which extend to high altitudes in the atmosphere. The atmosphere also shows a depletion of H2O, a finding consistent with the formation of high-temperature aerosols from oxygen-rich species. This work is part of a series of studies by our JWST Telescope Scientist Team (JWST-TST), in which we will use Guaranteed Time Observations to perform Deep Reconnaissance of Exoplanet Atmospheres through Multi-instrument Spectroscopy (DREAMS). © 2023. The Author(s). Published by the American Astronomical Society.Note
Open access journalISSN
2041-8205Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.3847/2041-8213/acfc3b
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Except where otherwise noted, this item's license is described as © 2023. The Author(s). Published by the American Astronomical Society. Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence.

