Ionisation and discharge in cloud-forming atmospheres of brown dwarfs and extrasolar planets
Ch. Helling (1), P. B. Rimmer (1), I. M. Rodriguez-Barrera (1),, Kenneth Wood (1), G.B. Robertson (1), C.R. Stark (2) (1 -- University of St, Andrews, 2 -- Abertay University)

TL;DR
This paper investigates ionisation, discharge processes, and magnetic interactions in the atmospheres of brown dwarfs and extrasolar planets, highlighting how these phenomena influence cloud properties and atmospheric chemistry.
Contribution
It provides a comprehensive analysis of ionisation mechanisms, discharge processes, and magnetic effects in ultra-cool atmospheres, combining models of cosmic ray interactions and cloud particle charging.
Findings
Cosmic rays can significantly increase free electrons in atmospheres.
Cloud particles are unlikely to be destroyed by Coulomb explosion.
Electrostatic cloud disruptions are limited to regions with strong gas ionisation.
Abstract
Brown dwarfs and giant gas extrasolar planets have cold atmospheres with a rich chemical compositions from which mineral cloud particles form. Their properties, like particle sizes and material composition, vary with height, and the mineral cloud particles are charged due to triboelectric processes in such dynamic atmospheres. The dynamics of the atmospheric gas is driven by the irradiating host star and/or by the rotation of the objects that changes during its lifetime. Thermal gas ionisation in these ultra-cool but dense atmospheres allows electrostatic interactions and magnetic coupling of a substantial atmosphere volume. Combined with a strong magnetic field , a chromosphere and aurorae might form as suggested by radio and X-ray observations of brown dwarfs. Non-equilibrium processes like cosmic ray ionisation and discharge processes in clouds will increase the…
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