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dc.contributor.authorArdaseva, Aleksandra
dc.contributor.authorRimmer, Paul B.
dc.contributor.authorWaldmann, Ingo
dc.contributor.authorRocchetto, Marco
dc.contributor.authorYurchenko, Sergey N.
dc.contributor.authorHelling, Christiane
dc.contributor.authorTennyson, Jonathan
dc.identifier.citationArdaseva , A , Rimmer , P B , Waldmann , I , Rocchetto , M , Yurchenko , S N , Helling , C & Tennyson , J 2017 , ' Lightning chemistry on Earth-like exoplanets ' , Monthly Notices of the Royal Astronomical Society , vol. 470 , no. 1 , stx1012 , pp. 187-196 .
dc.identifier.otherPURE: 250560472
dc.identifier.otherPURE UUID: 1e563f6f-508e-404b-9b1a-a02b0ee5ea2c
dc.identifier.otherScopus: 85021843287
dc.identifier.otherWOS: 000406842600013
dc.descriptionAA, PBR and ChH gratefully acknowledge the support of the ERC Starting Grant no. 257431. IW, MR, SNY and JT also gratefully acknowledge the support of the STFC (ST/K502406/1), and the ERC projects ExoMol (26719) and ExoLights (617119).en
dc.description.abstractWe present a model for lightning shock-induced chemistry that can be applied to atmospheres of arbitrary H/C/N/O chemistry, hence for extrasolar planets and brown dwarfs. The model couples hydrodynamics and the STAND2015 kinetic gas-phase chemistry. For an exoplanet analogue to the contemporary Earth, our model predicts NO and NO2 yields in agreement with observation. We predict height-dependent mixing ratios during a storm soon after a lightning shock of NO ≈ 10-3 at 40 km and NO2 ≈ 10-4 below 40 km, with O3 reduced to trace quantities (≪10-10). For an Earth-like exoplanet with a CO2/N2 dominated atmosphere and with an extremely intense lightning storm over its entire surface, we predict significant changes in the amount of NO, NO2, O3, H2O, H2 and predict a significant abundance of C2N. We find that, for the Early Earth, O2 is formed in large quantities by lightning but is rapidly processed by the photochemistry, consistent with previous work on lightning. The chemical effect of persistent global lightning storms are predicted to be significant, primarily due to NO2, with the largest spectral features present at ∼3.4 and ∼6.2 μm. The features within the transmission spectrum are on the order of 1 ppm and therefore are not likely detectable with the James Webb Space Telescope. Depending on its spectral properties, C2N could be a key tracer for lightning on Earth-like exoplanets with a N2/CO2 bulk atmosphere, unless destroyed by yet unknown chemical reactions.
dc.relation.ispartofMonthly Notices of the Royal Astronomical Societyen
dc.rights© 2017 The Authors. Published by Oxford University Press on behalf of the Royal Astronomical Society.This work is made available online in accordance with the publisher’s policies. This is the final published version of the work, which was originally published at:
dc.subjectAtmospheric effectsen
dc.subjectMolecular processesen
dc.subjectQB Astronomyen
dc.subjectQC Physicsen
dc.subjectQD Chemistryen
dc.subjectAstronomy and Astrophysicsen
dc.subjectSpace and Planetary Scienceen
dc.titleLightning chemistry on Earth-like exoplanetsen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.St Andrews Centre for Exoplanet Scienceen
dc.contributor.institutionUniversity of St Andrews.School of Physics and Astronomyen
dc.description.statusPeer revieweden

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