HCN-C₆H₆ co-condensed ice cloud in Titan’s stratosphere: Laboratory study of the CIRS-observed HASP cloud
dc.contributor.author | Mvondo, Delphine Nna | |
dc.contributor.author | Anderson, Carrie M | |
dc.contributor.author | Samuelson, Robert E | |
dc.date.accessioned | 2019-10-09T15:04:35Z | |
dc.date.available | 2019-10-09T15:04:35Z | |
dc.date.issued | 2019-09 | |
dc.description | EPSC-DPS Joint Meeting 2019 | en_US |
dc.description.abstract | For thirteen years, the Cassini mission to explore Saturn and its icy moons has provided a large repository of data on Titan’s atmosphere. Ice clouds have been repeatedly observed in Titan's stratosphere by the Cassini Composite InfraRed Spectrometer (CIRS). Pure nitrile ice clouds have been identified but the chemical composition of other observed ice clouds is still undetermined. We propose cocondensation to be a formation mechanism of these other clouds. With the aim to identify the HighAltitude South Polar (HASP) ice cloud, the most recently observed cloud during the early Titan’s southern winter, we have conducted laboratory thin ice film spectroscopy of a series of organic mixed ices and found that a C6H6-HCN co-condensed ice, enriched in benzene, is the best chemical candidate for the HASP cloud. | en_US |
dc.description.sponsorship | D.N.-M acknowledges research funding support by the NASA Postdoctoral Program at NASA GSFC, administered by the USRA; and by the NASA Internal Scientist Funding Model (ISFM) through the Fundamental Laboratory Research (FLaRe) work package. C.M.A. and R.E.S. acknowledge funding from the Cassini Project. | en_US |
dc.description.uri | https://meetingorganizer.copernicus.org/EPSC-DPS2019/EPSC-DPS2019-1005-2.pdf | en_US |
dc.format.extent | 2 pages | en_US |
dc.genre | conference papers and proceedings | en_US |
dc.identifier | doi:10.13016/m2nwnf-6ace | |
dc.identifier.uri | http://hdl.handle.net/11603/14998 | |
dc.language.iso | en_US | en_US |
dc.publisher | EPSC | en_US |
dc.relation.isAvailableAt | The University of Maryland, Baltimore County (UMBC) | |
dc.relation.ispartof | UMBC Center for Space Sciences and Technology | |
dc.relation.ispartof | UMBC Faculty Collection | |
dc.rights | This item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author. | |
dc.rights | Attribution 4.0 International (CC BY 4.0) | * |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | * |
dc.subject | Titan’s atmosphere | en_US |
dc.subject | Pure nitrile ice clouds | en_US |
dc.subject | cocondensation | en_US |
dc.subject | laboratory thin ice film spectroscopy | en_US |
dc.subject | benzene | en_US |
dc.subject | formation mechanism | en_US |
dc.title | HCN-C₆H₆ co-condensed ice cloud in Titan’s stratosphere: Laboratory study of the CIRS-observed HASP cloud | en_US |
dc.type | Text | en_US |
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