Possible Carbon Dioxide Above the Thick Aerosols of GJ 1214 b

Fuente: arXiv
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Main Authors: Schlawin, Everett, Ohno, Kazumasa, Bell, Taylor J., Murphy, Matthew M., Welbanks, Luis, Beatty, Thomas G., Greene, Thomas P., Fortney, Jonathan J., Parmentier, Vivien, Edelman, Isaac R., Gill, Samuel, Anderson, David R., Wheatley, Peter J., Henry, Gregory W., Mehta, Nishil, Kreidberg, Laura, Rieke, Marcia J.
Format: Preprint
Published: 2024
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author Schlawin, Everett
Ohno, Kazumasa
Bell, Taylor J.
Murphy, Matthew M.
Welbanks, Luis
Beatty, Thomas G.
Greene, Thomas P.
Fortney, Jonathan J.
Parmentier, Vivien
Edelman, Isaac R.
Gill, Samuel
Anderson, David R.
Wheatley, Peter J.
Henry, Gregory W.
Mehta, Nishil
Kreidberg, Laura
Rieke, Marcia J.
author_facet Schlawin, Everett
Ohno, Kazumasa
Bell, Taylor J.
Murphy, Matthew M.
Welbanks, Luis
Beatty, Thomas G.
Greene, Thomas P.
Fortney, Jonathan J.
Parmentier, Vivien
Edelman, Isaac R.
Gill, Samuel
Anderson, David R.
Wheatley, Peter J.
Henry, Gregory W.
Mehta, Nishil
Kreidberg, Laura
Rieke, Marcia J.
contents Sub-Neptune planets with radii smaller than Neptune (3.9 Re) are the most common type of planet known to exist in The Milky Way, even though they are absent in the Solar System. These planets can potentially have a large diversity of compositions as a result of different mixtures of rocky material, icy material and gas accreted from a protoplanetary disk. However, the bulk density of a sub-Neptune, informed by its mass and radius alone, cannot uniquely constrain its composition; atmospheric spectroscopy is necessary. GJ 1214 b, which hosts an atmosphere that is potentially the most favorable for spectroscopic detection of any sub-Neptune, is instead enshrouded in aerosols (thus showing no spectroscopic features), hiding its composition from view at previously observed wavelengths in its terminator. Here, we present a JWST NIRSpec transmission spectrum from 2.8 to 5.1 um that shows signatures of carbon dioxide and methane, expected at high metallicity. A model containing both these molecules is preferred by 3.3 and 3.6 sigma as compared to a featureless spectrum for two different data analysis pipelines, respectively. Given the low signal-to-noise of the features compared to the continuum, however, more observations are needed to confirm the carbon dioxide and methane signatures and better constrain other diagnostic features in the near-infrared. Further modeling of the planet's atmosphere, interior structure and origins will provide valuable insights about how sub-Neptunes like GJ 1214 b form and evolve.
format Preprint
id arxiv_https___arxiv_org_abs_2410_10183
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Possible Carbon Dioxide Above the Thick Aerosols of GJ 1214 b
Schlawin, Everett
Ohno, Kazumasa
Bell, Taylor J.
Murphy, Matthew M.
Welbanks, Luis
Beatty, Thomas G.
Greene, Thomas P.
Fortney, Jonathan J.
Parmentier, Vivien
Edelman, Isaac R.
Gill, Samuel
Anderson, David R.
Wheatley, Peter J.
Henry, Gregory W.
Mehta, Nishil
Kreidberg, Laura
Rieke, Marcia J.
Earth and Planetary Astrophysics
Sub-Neptune planets with radii smaller than Neptune (3.9 Re) are the most common type of planet known to exist in The Milky Way, even though they are absent in the Solar System. These planets can potentially have a large diversity of compositions as a result of different mixtures of rocky material, icy material and gas accreted from a protoplanetary disk. However, the bulk density of a sub-Neptune, informed by its mass and radius alone, cannot uniquely constrain its composition; atmospheric spectroscopy is necessary. GJ 1214 b, which hosts an atmosphere that is potentially the most favorable for spectroscopic detection of any sub-Neptune, is instead enshrouded in aerosols (thus showing no spectroscopic features), hiding its composition from view at previously observed wavelengths in its terminator. Here, we present a JWST NIRSpec transmission spectrum from 2.8 to 5.1 um that shows signatures of carbon dioxide and methane, expected at high metallicity. A model containing both these molecules is preferred by 3.3 and 3.6 sigma as compared to a featureless spectrum for two different data analysis pipelines, respectively. Given the low signal-to-noise of the features compared to the continuum, however, more observations are needed to confirm the carbon dioxide and methane signatures and better constrain other diagnostic features in the near-infrared. Further modeling of the planet's atmosphere, interior structure and origins will provide valuable insights about how sub-Neptunes like GJ 1214 b form and evolve.
title Possible Carbon Dioxide Above the Thick Aerosols of GJ 1214 b
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2410.10183