Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion

The lack of close-in Neptune-mass exoplanets evident in transit surveys has largely been attributed to either photoevaporative mass loss or high-eccentricity migration. To distinguish between these two possibilities, we investigate the origins of TOI-1259 A b, a Saturn-mass (0.4 M _J , 1.0 R _J ) ex...

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Main Authors: Morgan Saidel, Shreyas Vissapragada, Jessica Spake, Heather A. Knutson, Dion Linssen, Michael Zhang, Michael Greklek-McKeon, Jorge Pérez-González, Antonija Oklopčić
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Astronomical Journal
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Online Access:https://doi.org/10.3847/1538-3881/ada49f
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author Morgan Saidel
Shreyas Vissapragada
Jessica Spake
Heather A. Knutson
Dion Linssen
Michael Zhang
Michael Greklek-McKeon
Jorge Pérez-González
Antonija Oklopčić
author_facet Morgan Saidel
Shreyas Vissapragada
Jessica Spake
Heather A. Knutson
Dion Linssen
Michael Zhang
Michael Greklek-McKeon
Jorge Pérez-González
Antonija Oklopčić
author_sort Morgan Saidel
collection DOAJ
description The lack of close-in Neptune-mass exoplanets evident in transit surveys has largely been attributed to either photoevaporative mass loss or high-eccentricity migration. To distinguish between these two possibilities, we investigate the origins of TOI-1259 A b, a Saturn-mass (0.4 M _J , 1.0 R _J ) exoplanet lying along the upper edge of the Neptune desert. TOI-1259 A b's close-in ( P = 3.48 days) orbit and low bulk density make the planet particularly vulnerable to photoevaporation. We studied the upper atmosphere of TOI-1259 A b using metastable helium 1083 nm transits observed with Palomar/WIRC and Keck/NIRSPEC. We report a band-integrated excess absorption of 0.395% ± 0.072% with Palomar/WIRC and a spectroscopically resolved 5.5 ± 0.94 km s ^−1 blueshifted absorption of 2.4% ± 0.52% ( T _1 – T _4 ) and 3.5% ± 0.72% ( T _2 – T _3 ) with Keck/NIRSPEC. These measurements indicate the presence of an extended escaping atmosphere. Fitting these signals with a Parker wind model, we determine a corresponding atmospheric mass-loss rate of log( $\dot{M}$ ) = 10.2–10.65 g s ^−1 for thermosphere temperatures between 7900 and 8600 K. This relatively low rate suggests that this planet would not have been significantly altered by mass loss even if it formed in situ. However, the presence of a white dwarf companion, TOI-1259 B, hints that this planet may not have formed close-in, but rather migrated inward relatively late. Given the estimated parameters of the proto−white dwarf companion, we find that high-eccentricity migration is possible for the system.
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spelling doaj-art-83950b47f71848d1a23e2b614bce8a752025-08-20T02:08:15ZengIOP PublishingThe Astronomical Journal1538-38812025-01-01169210410.3847/1538-3881/ada49fAtmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf CompanionMorgan Saidel0https://orcid.org/0000-0001-9518-9691Shreyas Vissapragada1https://orcid.org/0000-0003-2527-1475Jessica Spake2https://orcid.org/0000-0002-5547-3775Heather A. Knutson3https://orcid.org/0000-0002-5375-4725Dion Linssen4https://orcid.org/0000-0001-6025-6663Michael Zhang5https://orcid.org/0000-0002-0659-1783Michael Greklek-McKeon6https://orcid.org/0000-0002-0371-1647Jorge Pérez-González7https://orcid.org/0000-0001-7144-589XAntonija Oklopčić8https://orcid.org/0000-0002-9584-6476Division of Geological and Planetary Sciences, California Institute of Technology , Pasadena, CA 91125, USA ; msaidel@caltech.eduCarnegie Science Observatories , 813 Santa Barbara Street, Pasadena, CA 91101, USACarnegie Science Observatories , 813 Santa Barbara Street, Pasadena, CA 91101, USADivision of Geological and Planetary Sciences, California Institute of Technology , Pasadena, CA 91125, USA ; msaidel@caltech.eduAnton Pannekoek Institute of Astronomy, University of Amsterdam , Science Park 904, 1098 XH Amsterdam, The NetherlandsDepartment of Astronomy & Astrophysics, University of Chicago , Chicago, IL 60637, USADivision of Geological and Planetary Sciences, California Institute of Technology , Pasadena, CA 91125, USA ; msaidel@caltech.eduDepartment of Physics and Astronomy, University College London , Gower Street, WC1E 6BT London, UKAnton Pannekoek Institute of Astronomy, University of Amsterdam , Science Park 904, 1098 XH Amsterdam, The NetherlandsThe lack of close-in Neptune-mass exoplanets evident in transit surveys has largely been attributed to either photoevaporative mass loss or high-eccentricity migration. To distinguish between these two possibilities, we investigate the origins of TOI-1259 A b, a Saturn-mass (0.4 M _J , 1.0 R _J ) exoplanet lying along the upper edge of the Neptune desert. TOI-1259 A b's close-in ( P = 3.48 days) orbit and low bulk density make the planet particularly vulnerable to photoevaporation. We studied the upper atmosphere of TOI-1259 A b using metastable helium 1083 nm transits observed with Palomar/WIRC and Keck/NIRSPEC. We report a band-integrated excess absorption of 0.395% ± 0.072% with Palomar/WIRC and a spectroscopically resolved 5.5 ± 0.94 km s ^−1 blueshifted absorption of 2.4% ± 0.52% ( T _1 – T _4 ) and 3.5% ± 0.72% ( T _2 – T _3 ) with Keck/NIRSPEC. These measurements indicate the presence of an extended escaping atmosphere. Fitting these signals with a Parker wind model, we determine a corresponding atmospheric mass-loss rate of log( $\dot{M}$ ) = 10.2–10.65 g s ^−1 for thermosphere temperatures between 7900 and 8600 K. This relatively low rate suggests that this planet would not have been significantly altered by mass loss even if it formed in situ. However, the presence of a white dwarf companion, TOI-1259 B, hints that this planet may not have formed close-in, but rather migrated inward relatively late. Given the estimated parameters of the proto−white dwarf companion, we find that high-eccentricity migration is possible for the system.https://doi.org/10.3847/1538-3881/ada49fExoplanet evolutionExoplanetsExoplanet atmospheresExoplanet astronomyPlanetary atmospheresExtrasolar gaseous planets
spellingShingle Morgan Saidel
Shreyas Vissapragada
Jessica Spake
Heather A. Knutson
Dion Linssen
Michael Zhang
Michael Greklek-McKeon
Jorge Pérez-González
Antonija Oklopčić
Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
The Astronomical Journal
Exoplanet evolution
Exoplanets
Exoplanet atmospheres
Exoplanet astronomy
Planetary atmospheres
Extrasolar gaseous planets
title Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
title_full Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
title_fullStr Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
title_full_unstemmed Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
title_short Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet with a White Dwarf Companion
title_sort atmospheric mass loss from toi 1259 a b a gas giant planet with a white dwarf companion
topic Exoplanet evolution
Exoplanets
Exoplanet atmospheres
Exoplanet astronomy
Planetary atmospheres
Extrasolar gaseous planets
url https://doi.org/10.3847/1538-3881/ada49f
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