Issue |
A&A
Volume 663, July 2022
|
|
---|---|---|
Article Number | A122 | |
Number of page(s) | 11 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202142763 | |
Published online | 22 July 2022 |
Irradiation-driven escape of primordial planetary atmospheres
II. Evaporation efficiency of sub-Neptunes through hot Jupiters
1
Fakultät für Mathematik, Universität Wien,
Oskar-Morgenstern-Platz 1,
1090
Wien, Austria
e-mail: andrea.caldiroli@univie.ac.at
2
Dipartimento di Scienza e Alta Tecnologia, Università degli Studi dell’Insubria,
via Valleggio 11,
22100
Como, Italy
3
INFN, Sezione Milano-Bicocca,
P.za della Scienza 3,
20126
Milano, Italy
4
INAF, Osservatorio Astronomico di Brera,
Via E. Bianchi 46,
23807
Merate, Italy
5
Department of Astronomy, University of Michigan,
1085 S University,
Ann Arbor, MI
48109, USA
Received:
26
November
2021
Accepted:
22
March
2022
Making use of the publicly available 1D photoionization hydrodynamics code ATES we set out to investigate the combined effects of specific planetary gravitational potential energy (ϕp ≡ GMp/Rp) and stellar X-ray and extreme ultraviolet (XUV) irradiation (FXUV) on the evaporation efficiency (η) of moderately-to-highly irradiated gaseous planets, from sub-Neptunes through hot Jupiters. We show that the (known) existence of a threshold potential above which energy-limited thermal escape (i.e., η ≃ 1) is unattainable can be inferred analytically, by means of a balance between the ion binding energy and the volume-averaged mean excess energy. For log ϕp ≳ log ϕpthr ≈ [12.9 − 13.2] (in cgs units), most of the energy absorption occurs within a region where the average kinetic energy acquired by the ions through photo-electron collisions is insufficient for escape. This causes the evaporation efficiency to plummet with increasing ϕp, by up to 4 orders of magnitude below the energy-limited value. Whether or not planets with ϕp ≲ ϕpthr exhibit energy-limited outflows is primarily regulated by the stellar irradiation level. Specifically, for low-gravity planets, above FXUVthr ≃ 104–5 erg cm−2 s−1, Lyα losses overtake adiabatic and advective cooling and the evaporation efficiency of low-gravity planets drops below the energy-limited approximation, albeit remaining largely independent of ϕp. Further, we show that whereas η increases as FXUV increases for planets above ϕpthr, the opposite is true for low-gravity planets (i.e., for sub-Neptunes). This behavior can be understood by examining the relative fractional contributions of advective and radiative losses as a function of atmospheric temperature. This novel framework enables a reliable, physically motivated prediction of the expected evaporation efficiency for a given planetary system; an analytical approximation of the best-fitting η is given in the appendix.
Key words: planets and satellites: atmospheres / planets and satellites: dynamical evolution and stability / planets and satellites: physical evolution
© ESO 2022
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