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  5. Irradiation-driven escape of primordial planetary atmospheres. II. Evaporation efficiency of sub-Neptunes through hot Jupiters.
 

Irradiation-driven escape of primordial planetary atmospheres. II. Evaporation efficiency of sub-Neptunes through hot Jupiters.

Journal
ASTRONOMY & ASTROPHYSICS  
Date Issued
2022
Author(s)
Caldiroli, Andrea
•
HAARDT, FRANCESCO  
•
Gallo, Elena
•
SPINELLI, Riccardo  
•
Malsky, Isaac
•
Rauscher, Emily
DOI
10.1051/0004-6361/202142763
Abstract
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 (Ï p ¡ 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 Ï p log Ïpthr [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 Ï p, by up to 4 orders of magnitude below the energy-limited value. Whether or not planets with Ï p Ï pthr exhibit energy-limited outflows is primarily regulated by the stellar irradiation level. Specifically, for low-gravity planets, above FXUVthr 104-5 erg cm2 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 Ï p. Further, we show that whereas η increases as FXUV increases for planets above Ï pthr, 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.
Volume
663
Start page
A122
Uri
http://hdl.handle.net/20.500.12386/36644
Url
http://dx.doi.org/10.1051/0004-6361/202142763
https://www.aanda.org/articles/aa/full_html/2022/07/aa42763-21/aa42763-21.html
Issn Identifier
0004-6361
Rights
open.access
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