Ionization in Atmospheres of Brown Dwarfs and Extrasolar Planets V: Alfv\'{e}n Ionization
Craig R. Stark, Christiane Helling, Declan A. Diver, Paul B. Rimmer

TL;DR
This paper proposes Alfvén ionization as an efficient mechanism to produce localized plasmas in the atmospheres of low-mass objects like brown dwarfs and exoplanets, explaining observed radio and X-ray emissions.
Contribution
It demonstrates the applicability of Alfvén ionization in low-mass object atmospheres and predicts resulting observable plasma signatures, expanding understanding of atmospheric ionization processes.
Findings
Alfvén ionization can achieve ionization levels of 10^{-6} to 1 in atmospheres.
Most efficient at mid to low pressures where seed plasma is magnetized.
Observable signatures include Bremsstrahlung and spectral lines from plasma ions.
Abstract
Observations of continuous radio and sporadic X-ray emission from low-mass objects suggest they harbour localized plasmas in their atmospheric environments. For low-mass objects, the degree of thermal ionization is insufficient to qualify the ionized component as a plasma, posing the question: what ionization processes can efficiently produce the required plasma that is the source of the radiation? We propose Alfv\'{e}n ionization as a mechanism for producing localized pockets of ionized gas in the atmosphere, having sufficient degrees of ionization () that they constitute plasmas. We outline the criteria required for Alfv\'{e}n ionization and demonstrate it's applicability in the atmospheres of low-mass objects such as giant gas planets, brown dwarfs and M-dwarfs for both solar and sub-solar metallicities. We find that Alfv\'{e}n ionization is most efficient at mid to low…
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