2013
DOI: 10.1016/j.pss.2012.07.003
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Dust cloud lightning in extraterrestrial atmospheres

Abstract: Lightning is present in all solar system planets which form clouds in their atmospheres. Cloud formation outside our solar system is possible in objects with much higher temperatures than on Earth or on Jupiter: Brown dwarfs and giant extrasolar gas planets form clouds made of mixed materials and a large spectrum of grain sizes. These clouds are globally neutral obeying dustgas charge equilibrium which is, on short timescales, inconsistent with the observation of stochastic ionization events of the solar syste… Show more

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Cited by 14 publications
(9 citation statements)
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“…Cosmic rays play important effects on the chemistry and ionisation of planetary atmospheres (Helling et al 2013;Rimmer & Helling 2013). They could also be a source of genetic mutations in organisms (Atri & Melott 2012).…”
Section: Galatic Cosmic Raysmentioning
confidence: 99%
“…Cosmic rays play important effects on the chemistry and ionisation of planetary atmospheres (Helling et al 2013;Rimmer & Helling 2013). They could also be a source of genetic mutations in organisms (Atri & Melott 2012).…”
Section: Galatic Cosmic Raysmentioning
confidence: 99%
“…We note that Helling and Woitke (2006) have also presented detailed models for the formation and evolution of clouds in drown dwarf atmospheres. These were subsequently applied to the atmospheric conditions of EGPs in order to investigate the composition and optical properties of clouds in these environments in relation to available observations (Lee et al 2015), the impact of the clouds on the atmospheric structure (Lee et al 2017), and the possible occurrence of lightning in these cloud structures (Helling et al 2013). Instead of the physics of cloud formation, in the current study we focus on the properties of the photochemical aerosols that can form in the upper atmosphere of EGPs.…”
Section: Introductionmentioning
confidence: 99%
“…Rimmer & Helling (2013) demonstrate that cosmic ray irradiation significantly enhances the electron fraction compared to thermal ionisation in the upper atmospheres of brown dwarfs, but the local degree of ionisation does not exceed 10 −7 in these low-density regions. Helling et al (2013) and Rimmer & Helling (2013) do further point out that CRs can affect the upper portion of the mineral clouds that form in brown dwarf atmospheres (Helling & Casewell 2014), an effect that is well established for solar system objects (Helling et al 2016a). The present paper takes the idea of environmental effects on the ionisation of atmospheres of very low-mass, ultra-cool objects one step further.…”
Section: Introductionmentioning
confidence: 93%