Magnesium Silicate Clouds in the Atmosphere of HD 209458b from a Rule-Based Tree-Structured Data Reduction

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Main Authors: Chubb, Katy L., Grant, David, Wakeford, Hannah R., Moran, Sarah E., Batalha, Natasha E., Egan, Arika, Fairman, Charlotte, Powell, Diana, Stevenson, Kevin B., Alderson, Lili, Gao, Peter, Kataria, Tiffany, Lewis, Nikole K., MacDonald, Ryan J., Mullens, Mark Marley Elijah, Sing, David K., Valenti, Jeff A.
Format: Preprint
Published: 2026
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author Chubb, Katy L.
Grant, David
Wakeford, Hannah R.
Moran, Sarah E.
Batalha, Natasha E.
Egan, Arika
Fairman, Charlotte
Powell, Diana
Stevenson, Kevin B.
Alderson, Lili
Gao, Peter
Kataria, Tiffany
Lewis, Nikole K.
MacDonald, Ryan J.
Mullens, Mark Marley Elijah
Sing, David K.
Valenti, Jeff A.
author_facet Chubb, Katy L.
Grant, David
Wakeford, Hannah R.
Moran, Sarah E.
Batalha, Natasha E.
Egan, Arika
Fairman, Charlotte
Powell, Diana
Stevenson, Kevin B.
Alderson, Lili
Gao, Peter
Kataria, Tiffany
Lewis, Nikole K.
MacDonald, Ryan J.
Mullens, Mark Marley Elijah
Sing, David K.
Valenti, Jeff A.
contents HD 209458b is the canonical hot Jupiter: the first to have its atmosphere measured and the first to hint at the role of aerosols in exoplanet atmospheres through the muting of Na absorption signatures in the optical. Here we present JWST MIRI/LRS transmission observations of HD 209458b from 5-12 microns, directly measuring the absorption signatures of its clouds for the first time. The observations indicate the presence of magnesium silicates, most likely Mg2SiO4 or a mixture of Mg2SiO4 and MgSiO3. We also present a new methodology to reduce observational data, whereby the analysis is formulated as a rule-based model with a tree structure, enabling key decisions to be identified and uncertain decisions to be incorporated into subsequent modeling. With this data reduction, and using a combination of ARCiS free retrievals and PICASO+Virga self consistent forward models, we are able to show that amorphous Mg2SiO4 clouds explain the LRS data to high significance over either a clear (Delta ln(Z)=16.63) or gray cloud atmosphere (Delta ln(Z)=22.26). By combining the LRS dataset with archival JWST NIRCam and HST optical and near-infrared observations, we are able to more robustly constrain the properties of the magnesium silicate condensates, finding particle sizes of approximately 0.1 microns and atmospheric pressures of the clouds of roughly 1-10 millibar. Our results add to the growing detections of silicate clouds as a dominant atmospheric component of hot Jupiters, with the exact silicate species contextualizing the atmospheric chemistry and potentially formation conditions of these planets.
format Preprint
id arxiv_https___arxiv_org_abs_2606_00177
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Magnesium Silicate Clouds in the Atmosphere of HD 209458b from a Rule-Based Tree-Structured Data Reduction
Chubb, Katy L.
Grant, David
Wakeford, Hannah R.
Moran, Sarah E.
Batalha, Natasha E.
Egan, Arika
Fairman, Charlotte
Powell, Diana
Stevenson, Kevin B.
Alderson, Lili
Gao, Peter
Kataria, Tiffany
Lewis, Nikole K.
MacDonald, Ryan J.
Mullens, Mark Marley Elijah
Sing, David K.
Valenti, Jeff A.
Earth and Planetary Astrophysics
Instrumentation and Methods for Astrophysics
HD 209458b is the canonical hot Jupiter: the first to have its atmosphere measured and the first to hint at the role of aerosols in exoplanet atmospheres through the muting of Na absorption signatures in the optical. Here we present JWST MIRI/LRS transmission observations of HD 209458b from 5-12 microns, directly measuring the absorption signatures of its clouds for the first time. The observations indicate the presence of magnesium silicates, most likely Mg2SiO4 or a mixture of Mg2SiO4 and MgSiO3. We also present a new methodology to reduce observational data, whereby the analysis is formulated as a rule-based model with a tree structure, enabling key decisions to be identified and uncertain decisions to be incorporated into subsequent modeling. With this data reduction, and using a combination of ARCiS free retrievals and PICASO+Virga self consistent forward models, we are able to show that amorphous Mg2SiO4 clouds explain the LRS data to high significance over either a clear (Delta ln(Z)=16.63) or gray cloud atmosphere (Delta ln(Z)=22.26). By combining the LRS dataset with archival JWST NIRCam and HST optical and near-infrared observations, we are able to more robustly constrain the properties of the magnesium silicate condensates, finding particle sizes of approximately 0.1 microns and atmospheric pressures of the clouds of roughly 1-10 millibar. Our results add to the growing detections of silicate clouds as a dominant atmospheric component of hot Jupiters, with the exact silicate species contextualizing the atmospheric chemistry and potentially formation conditions of these planets.
title Magnesium Silicate Clouds in the Atmosphere of HD 209458b from a Rule-Based Tree-Structured Data Reduction
topic Earth and Planetary Astrophysics
Instrumentation and Methods for Astrophysics
url https://arxiv.org/abs/2606.00177