2016
DOI: 10.1093/mnras/stw935
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EUV-driven mass-loss of protoplanetary cores with hydrogen-dominated atmospheres: the influences of ionization and orbital distance

Abstract: We investigate the loss rates of the hydrogen atmospheres of terrestrial planets with a range of masses and orbital distances by assuming a stellar extreme ultraviolet (EUV) luminosity that is 100 times stronger than that of the current Sun. We apply a 1D upper atmosphere radiation absorption and hydrodynamic escape model that takes into account ionization, dissociation and recombination to calculate hydrogen mass loss rates. We study the effects of the ionization, dissociation and recombination on the thermal… Show more

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Cited by 100 publications
(89 citation statements)
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“…To model the planetary upper atmosphere and infer the mass-loss rates, we employ an updated version of the 1D hydrodynamical code described in detail in the appendix of Erkaev et al (2016). This model treats the planetary upper atmosphere as a clear hydrogen gas envelope, including the effects of recombination, dissociation, ionization of the hydrogen atoms and molecules, and Ly-α cooling.…”
Section: Physical Modelmentioning
confidence: 99%
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“…To model the planetary upper atmosphere and infer the mass-loss rates, we employ an updated version of the 1D hydrodynamical code described in detail in the appendix of Erkaev et al (2016). This model treats the planetary upper atmosphere as a clear hydrogen gas envelope, including the effects of recombination, dissociation, ionization of the hydrogen atoms and molecules, and Ly-α cooling.…”
Section: Physical Modelmentioning
confidence: 99%
“…Watson et al 1981;Yelle 2004;Murray-Clay et al 2009;Cecchi-Pestellini et al 2009;Owen & Jackson 2012;Shematovich et al 2014;Salz et al 2016). In this work, we follow the considerations of Erkaev et al (2016) and adopt a value of 15%, based on the results of the direct simulation Monte Carlo model calculations of Shematovich et al (2014), which model photolytic and electron impact processes in the thermosphere by solving the kinetic Boltzmann equation.…”
Section: Physical Modelmentioning
confidence: 99%
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“…To study the EUV heating and expansion and to infer the mass-loss rates of the hydrogen-dominated upper atmosphere of the planet, we apply a time-dependent 1D hydrodynamic model described in detail by Erkaev et al (2016). The model solves the absorption of the stellar EUV flux by the thermosphere, the hydrodynamic equations for mass, momentum, and energy conservation, and the continuity equations for neutrals and ions (both atoms and molecules).…”
Section: Hydrodynamic Upper Atmosphere Modelmentioning
confidence: 99%