Helium in the Extended Atmosphere of the Warm Super-Puff TOI-1420b

Fuente: arXiv
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Autori principali: Vissapragada, Shreyas, Greklek-McKeon, Michael, Linssen, Dion, MacLeod, Morgan, Thorngren, Daniel P., Gao, Peter, Knutson, Heather A., Latham, David W., López-Morales, Mercedes, Oklopčić, Antonija, González, Jorge Pérez, Saidel, Morgan, Tumborang, Abigail, Yoshida, Stephanie
Natura: Preprint
Pubblicazione: 2024
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author Vissapragada, Shreyas
Greklek-McKeon, Michael
Linssen, Dion
MacLeod, Morgan
Thorngren, Daniel P.
Gao, Peter
Knutson, Heather A.
Latham, David W.
López-Morales, Mercedes
Oklopčić, Antonija
González, Jorge Pérez
Saidel, Morgan
Tumborang, Abigail
Yoshida, Stephanie
author_facet Vissapragada, Shreyas
Greklek-McKeon, Michael
Linssen, Dion
MacLeod, Morgan
Thorngren, Daniel P.
Gao, Peter
Knutson, Heather A.
Latham, David W.
López-Morales, Mercedes
Oklopčić, Antonija
González, Jorge Pérez
Saidel, Morgan
Tumborang, Abigail
Yoshida, Stephanie
contents Super-puffs are planets with exceptionally low densities ($ρ\lesssim 0.1$~g~cm$^{-3}$) and core masses ($M_c \lesssim 5 M_\oplus$). Many lower-mass ($M_p\lesssim10M_\oplus$) super-puffs are expected to be unstable to catastrophic mass loss via photoevaporation and/or boil-off, whereas the larger gravitational potentials of higher-mass ($M_p\gtrsim10M_\oplus$) super-puffs should make them more stable to these processes. We test this expectation by studying atmospheric loss in the warm, higher-mass super-puff TOI-1420b ($M = 25.1M_\oplus$, $R = 11.9R_\oplus$, $ρ= 0.08$~g~cm$^{-3}$, $T_\mathrm{eq} = 960$~K). We observed one full transit and one partial transit of this planet using the metastable helium filter on Palomar/WIRC and found that the helium transits were $0.671\pm0.079\%$ (8.5$σ$) deeper than the TESS transits, indicating an outflowing atmosphere. We modeled the excess helium absorption using a self-consistent 1D hydrodynamics code to constrain the thermal structure of the outflow given different assumptions for the stellar XUV spectrum. These calculations then informed a 3D simulation which provided a good match to the observations with a modest planetary mass-loss rate of $10^{10.82}$~g~s$^{-1}$ ($M_p/\dot{M}\approx70$~Gyr). Super-puffs with $M_p\gtrsim10M_\oplus$, like TOI-1420b and WASP-107b, appear perfectly capable of retaining atmospheres over long timescales; therefore, these planets may have formed with the unusually large envelope mass fractions they appear to possess today. Alternatively, tidal circularization could have plausibly heated and inflated these planets, which would bring their envelope mass fractions into better agreement with expectations from core-nucleated accretion.
format Preprint
id arxiv_https___arxiv_org_abs_2403_05614
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Helium in the Extended Atmosphere of the Warm Super-Puff TOI-1420b
Vissapragada, Shreyas
Greklek-McKeon, Michael
Linssen, Dion
MacLeod, Morgan
Thorngren, Daniel P.
Gao, Peter
Knutson, Heather A.
Latham, David W.
López-Morales, Mercedes
Oklopčić, Antonija
González, Jorge Pérez
Saidel, Morgan
Tumborang, Abigail
Yoshida, Stephanie
Earth and Planetary Astrophysics
Super-puffs are planets with exceptionally low densities ($ρ\lesssim 0.1$~g~cm$^{-3}$) and core masses ($M_c \lesssim 5 M_\oplus$). Many lower-mass ($M_p\lesssim10M_\oplus$) super-puffs are expected to be unstable to catastrophic mass loss via photoevaporation and/or boil-off, whereas the larger gravitational potentials of higher-mass ($M_p\gtrsim10M_\oplus$) super-puffs should make them more stable to these processes. We test this expectation by studying atmospheric loss in the warm, higher-mass super-puff TOI-1420b ($M = 25.1M_\oplus$, $R = 11.9R_\oplus$, $ρ= 0.08$~g~cm$^{-3}$, $T_\mathrm{eq} = 960$~K). We observed one full transit and one partial transit of this planet using the metastable helium filter on Palomar/WIRC and found that the helium transits were $0.671\pm0.079\%$ (8.5$σ$) deeper than the TESS transits, indicating an outflowing atmosphere. We modeled the excess helium absorption using a self-consistent 1D hydrodynamics code to constrain the thermal structure of the outflow given different assumptions for the stellar XUV spectrum. These calculations then informed a 3D simulation which provided a good match to the observations with a modest planetary mass-loss rate of $10^{10.82}$~g~s$^{-1}$ ($M_p/\dot{M}\approx70$~Gyr). Super-puffs with $M_p\gtrsim10M_\oplus$, like TOI-1420b and WASP-107b, appear perfectly capable of retaining atmospheres over long timescales; therefore, these planets may have formed with the unusually large envelope mass fractions they appear to possess today. Alternatively, tidal circularization could have plausibly heated and inflated these planets, which would bring their envelope mass fractions into better agreement with expectations from core-nucleated accretion.
title Helium in the Extended Atmosphere of the Warm Super-Puff TOI-1420b
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2403.05614