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dc.contributor.authorLines, S
dc.contributor.authorManners, J
dc.contributor.authorMayne, NJ
dc.contributor.authorGoyal, J
dc.contributor.authorCarter, A
dc.contributor.authorBoutle, I
dc.contributor.authorLee, G
dc.contributor.authorHelling, C
dc.contributor.authorDrummond, B
dc.contributor.authorAcreman, D
dc.contributor.authorSing, D
dc.date.accessioned2018-09-05T10:17:52Z
dc.date.issued2018-08-28
dc.description.abstractWe present high-resolution transmission spectra, calculated directly from a 3D radiative hydrodynamic simulation that includes kinetic cloud formation, for HD 209458b. We find that the high opacity of our vertically extensive cloud deck, composed of a large number density of sub- μ m particles, flattens the transmission spectrum and obscures spectral features identified in the observed data. We use the PANDEXO simulator to explore features of our HD 209458b spectrum which may be detectable with the James Webb Space Telescope. We determine that an   8–12 μ m absorption feature attributed to the mixed-composition, predominantly silicate cloud particles is a viable marker for the presence of cloud. Further calculations explore, and trends are identified with, variations in cloud opacity, composition heterogeneity, and artificially scaled gravitational settling on the transmission spectrum. Principally, by varying the upper extent of our cloud decks, rainout is identified to be a key process for the dynamical atmospheres of hot Jupiters and shown to dramatically alter the resulting spectrum. Our synthetic transmission spectra, obtained from the most complete, forward atmosphere simulations to date, allow us to explore the model’s ability to conform with observations. Such comparisons can provide insight into the physical processes either missing or requiring improvement.en_GB
dc.description.sponsorshipS. Lines and J. Goyal are funded by and thankful to the Leverhulme Trust. N. J. Mayne is part funded by a Leverhulme Trust Research Project Grant. J. Manners and I. A. Boutle acknowledge the support of a Met Office Academic Partnership secondment. B. Drummond acknowledges funding from the European Research Council (ERC) under the European Unions Seventh Framework Programme (FP7/2007-2013) / ERC grant agreement no. 336792. G. K. H. Lee acknowledges support from the Universities of Oxford and Bern through the Bernoulli fellowship program. A. L. Carter is funded by a Science and Technology Facilities Council (STFC) studentship. The calculations for this paper were performed on the University of Exeter supercomputer, a Distributed Research using Advanced Computing (DiRAC) facility jointly funded by STFC, the Large Facilities Capital Fund of the Department for Business, Innovation and Skills (BIS), and the University of Exeter.en_GB
dc.identifier.citationVol. 481 (1), pp. 194-205en_GB
dc.identifier.doi10.1093/mnras/sty2275
dc.identifier.urihttp://hdl.handle.net/10871/33916
dc.language.isoenen_GB
dc.publisherOxford University Press (OUP) / Royal Astronomical Societyen_GB
dc.relation.urlhttps://doi.org/10.24378/exe.645en_GB
dc.rights© 2018 The Author(s) Published by Oxford University Press on behalf of the Royal Astronomical Societyen_GB
dc.subjecthydrodynamicsen_GB
dc.subjectradiative transferen_GB
dc.subjectscatteringen_GB
dc.subjectmethods: numericalen_GB
dc.subjectplanets and satellites: atmospheresen_GB
dc.titleExonephology: Transmission spectra from a 3D simulated cloudy atmosphere of HD209458b (article)en_GB
dc.typeArticleen_GB
dc.date.available2018-09-05T10:17:52Z
dc.identifier.issn0035-8711
dc.descriptionThis is the final version of the article. Available from OUP via the DOI in this record.en_GB
dc.descriptionThe dataset associated with this article is located in ORE at https://doi.org/10.24378/exe.645en_GB
dc.identifier.journalMonthly Notices of the Royal Astronomical Societyen_GB


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