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Aug 03, 2023A reflective, metal
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There are no planets intermediate in size between Earth and Neptune in our Solar System, yet these objects are found around a substantial fraction of other stars [1]. Population statistics show that close-in planets in this size range bifurcate into two classes based on their radii [2, 3]. It is hypothesized that the group with larger radii (referred to as "sub-Neptunes") is distinguished by having hydrogen-dominated atmospheres that are a few percent of the total mass of the planets [4]. GJ 1214b is an archetype sub-Neptune that has been observed extensively using transmission spectroscopy to test this hypothesis [5-14]. However, themeasured spectra are featureless, and thus inconclusive, due to the presence of high-altitude aerosols in the planet's atmosphere. Here we report a spectroscopic thermal phase curve of GJ 1214b obtained with JWST in the mid-infrared. The dayside and nightside spectra (average brightness temperatures of 553 ± 9 and 437 ± 19 K, respectively) each show >3σ evidence of absorption features, with H2O as the most likely cause in both. The measured global thermal emission implies that GJ 1214b's Bond albedo is 0.51 ± 0.06. Comparison between the spectroscopic phase curve data and three-dimensional models of GJ 1214b reveal a planet with a high metallicity atmosphere blanketed by a thick and highly reflective layer of clouds or haze.
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Department of Astronomy, University of Maryland, College Park, MD, USA
Eliza M.-R. Kempton, Arjun B. Savel, Kenneth E. Arnold, Matthew C. Nixon, Matej Malik & Jegug Ih
Department of Astronomy & Astrophysics, University of Chicago, Chicago, IL, USA
Michael Zhang, Jacob L. Bean & Qiao Xue
Max-Planck-Institut für Astronomie, Heidelberg, Germany
Maria E. Steinrueck & Sebastian Zieba
Earth and Planets Laboratory, Carnegie Institution for Science, Washington, DC, USA
Anjali A. A. Piette & Peter Gao
Department of Physics, University of Oxford, Oxford, UK
Vivien Parmentier & Jake Taylor
Department of Astronomy, University of Michigan, Ann Arbor, MI, USA
Isaac Malsky & Emily Rauscher
School of Physics and Astronomy, University of Leicester, Leicester, UK
Michael T. Roman
BAER Institute, NASA Ames Research Center, Moffet Field, CA, USA
Taylor J. Bell
Institut Trottier de Recherche sur les Exoplanètes and Département de Physique, Université de Montréal, Montréal, QC, Canada
Jake Taylor
Center for Computational Astrophysics, Flatiron Institute, New York, NY, USA
Arjun B. Savel
Johns Hopkins Applied Physics Laboratory, Laurel, MD, USA
Kevin B. Stevenson
Steward Observatory, University of Arizona, Tucson, AZ, USA
Megan Mansfield
European Space Agency, Space Telescope Science Institute, Baltimore, MD, USA
Sarah Kendrew
Leiden Observatory, Leiden University, Leiden, The Netherlands
Sebastian Zieba
Paris Region Fellow, Marie Sklodowska-Curie Action, Paris, France
Elsa Ducrot
AIM, CEA, CNRS, Université Paris-Saclay, Université de Paris, Gif-sur-Yvette, France
Elsa Ducrot, Achrène Dyrek & Pierre-Olivier Lagage
Department of Physics and Astronomy, Vanderbilt University, Nashville, TN, USA
Keivan G. Stassun
Center of Excellence in Information Systems, Tennessee State University, Nashville, TN, USA
Gregory W. Henry
Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ, USA
Travis Barman
Eureka Scientific, Inc., Oakland, CA, USA
Roxana Lupu
NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
Tiffany Kataria
Department of Physics & Astronomy, Johns Hopkins University, Baltimore, MD, USA
Guangwei Fu
School of Earth & Space Exploration, Arizona State University, Tempe, AZ, USA
Luis Welbanks
Department of Astronomy & Astrophysics, University of California, Santa Cruz, CA, USA
Peter McGill
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Correspondence to Eliza M.-R. Kempton.
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Kempton, E.MR., Zhang, M., Bean, J.L. et al. A reflective, metal-rich atmosphere for GJ 1214b from its JWST phase curve. Nature (2023). https://doi.org/10.1038/s41586-023-06159-5
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Received: 11 February 2023
Accepted: 02 May 2023
Published: 10 May 2023
DOI: https://doi.org/10.1038/s41586-023-06159-5
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