Water Dissociation and Rotational Broadening in the Atmosphere of KELT-20 b from High-resolution Spectroscopy
- Creators
-
Finnerty, Luke1
-
Xin, Yinzi2
-
Xuan, Jerry W.2
-
Inglis, Julie2
-
Fitzgerald, Michael P.1
-
Agrawal, Shubh3
-
Baker, Ashley2
- Bartos, Randall4
-
Blake, Geoffrey A.2
-
Calvin, Benjamin1, 2
- Cetre, Sylvain5
-
Delorme, Jacques-Robert2, 5
- Doppmann, Greg5
-
Echeverri, Daniel2
-
Horstman, Katelyn2
-
Hsu, Chih-Chun6
-
Jovanovic, Nemanja2
-
Liberman, Joshua2, 7
-
López, Ronald A.1
-
Martin, Emily C.8
-
Mawet, Dimitri2, 4
-
Morris, Evan8
- Pezzato, Jacklyn2
-
Ruffio, Jean-Baptiste9
-
Sappey, Ben9
- Schofield, Tobias2
-
Skemer, Andrew8
-
Venenciano, Taylor10
-
Wallace, J. Kent4
-
Wallack, Nicole L.11
-
Wang 王, Jason J. 劲飞6
-
Wang 王, Ji 吉12
-
1.
University of California, Los Angeles
-
2.
California Institute of Technology
-
3.
University of Pennsylvania
-
4.
Jet Propulsion Lab
-
5.
W.M. Keck Observatory
-
6.
Northwestern University
-
7.
University of Arizona
-
8.
University of California, Santa Cruz
-
9.
University of California, San Diego
-
10.
Pomona College
-
11.
Carnegie Institution for Science
-
12.
The Ohio State University
Abstract
We present atmospheric retrievals from Keck/KPIC Phase II observations of the ultrahot Jupiter (UHJ) KELT-20/MASCARA-2 b. Previous free retrievals of molecular abundances for UHJs have been impacted by significant model biases due to variations in vertical abundance profiles, which we address by including molecular dissociation into our retrieval framework as an additional free parameter. We measure the abundance of CO (logCOMMR=−2.5−0.5+0.6) and obtain a lower limit on the abundance of H2O (logH₂OMMR=−1.5_(−1.0)^(+0.8), >−3.0 at 95% confidence) in the atmosphere of KELT-20 b. These abundances yield an atmospheric C/O=0.1_(−0.1)^(+0.4) (C/O < 0.9 at 95% confidence) and suggest a metallicity approximately solar to 10 × solar. H2O is dissociated at pressures below logPH2O=−1.2_(−0.7)^(+0.5) bar, roughly consistent with predictions from chemical equilibrium models, and suggesting that the retrieved composition is not a result of assumptions about the vertical mixing profiles. We also constrain the rotational velocity of KELT-20 b to vsini=7.5±0.7 km s−1, suggesting the presence of a jet comparable to the sound speed in the direction of the planet's rotation, assuming the actual rotation of the planet is tidally locked.
Copyright and License
© 2025. 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. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.
Acknowledgement
The thank the anonymous referee whose thorough and insightful comments greatly improved this work. L. F. is a member of UAW local 4811. L.F. acknowledges the support of the W.M. Keck Foundation, which also supports development of the KPIC facility Data Reduction Pipeline. The contributed Hoffman2 computing node used for this work was supported by the Heising-Simons Foundation grant #2020-1821. Funding for KPIC has been provided by the California Institute of Technology, the Jet Propulsion Laboratory, the Heising-Simons Foundation (grants #2015-129, #2017-318, #2019-1312, #2023-4597, and #2023-4598), the Simons Foundation (through the Caltech Center for Comparative Planetary Evolution), and the NSF under grant AST-1611623. D.E. acknowledges support from the NASA Future Investigators in NASA Earth and Space Science and Technology (FINESST) fellowship under award #80NSSC19K1423, as well as support from the Keck Visiting Scholars Program (KVSP) to install the Phase II upgrades for KPIC. J.X. acknowledges support from the NASA Future Investigators in NASA Earth and Space Science and Technology (FINESST) award #80NSSC23K1434.
This work used computational and storage services associated with the Hoffman2 Shared Cluster provided by UCLA Institute for Digital Research and Education's Research Technology Group. L.F. thanks Briley Lewis for her helpful guide to using Hoffman2, and Paul Mollière for his assistance in adding additional opacities to petitRADTRANS.
The data presented herein were obtained at the W. M. Keck Observatory, which is operated as a scientific partnership among the California Institute of Technology, the University of California and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W. M. Keck Foundation. W. M. Keck Observatory access was supported by Northwestern University and the Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA). The authors wish to recognize and acknowledge the very significant cultural role and reverence that the summit of Maunakea has always had within the indigenous Hawaiian community. We are most fortunate to have the opportunity to conduct observations from this mountain.
This research has made use of the NASA Exoplanet Archive, which is operated by the California Institute of Technology, under contract with the National Aeronautics and Space Administration under the Exoplanet Exploration Program. This research has made use of the Exoplanet Follow-up Observation Program (ExoFOP; doi:10.26134/ExoFOP5) website, which is operated by the California Institute of Technology, under contract with the National Aeronautics and Space Administration under the Exoplanet Exploration Program.
Facilities
Keck:II - KECK II Telescope (NIRSPEC/KPIC).
Software References
astropy (Astropy Collaboration et al. 2013, 2018), dynesty (J. S. Speagle 2020), corner (D. Foreman-Mackey 2016), petitRADTRANS (P. Mollière et al. 2019, 2020), numpy (R.C. Harris et al. 2020), scipy (P. Virtanen et al. 2020), matplotlib (J. D. Hunter 2007).
Files
Name | Size | Download all |
---|---|---|
md5:80b3261d4b2947377659517ec2eba463
|
28.1 MB | Preview Download |
Additional details
- W. M. Keck Foundation
- Heising-Simons Foundation
- 2020-1821
- California Institute of Technology
- Jet Propulsion Laboratory
- Heising-Simons Foundation
- 2015-129
- Heising-Simons Foundation
- 2017-318
- Heising-Simons Foundation
- 2019-1312
- Heising-Simons Foundation
- 2023-4597
- Heising-Simons Foundation
- 2023-4598
- Simons Foundation
- National Science Foundation
- AST-1611623
- National Aeronautics and Space Administration
- 80NSSC19K1423
- National Aeronautics and Space Administration
- 80NSSC23K1434
- Accepted
-
2025-03-01
- Available
-
2025-05-23Published
- Caltech groups
- Astronomy Department, Caltech Center for Comparative Planetary Evolution, Division of Geological and Planetary Sciences (GPS), Division of Physics, Mathematics and Astronomy (PMA)
- Publication Status
- Published