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Models of Venus neutral upper atmosphere: Structure and composition

dc.contributor.authorKeating, G. M.en_US
dc.contributor.authorBertaux, J. L.en_US
dc.contributor.authorBougher, Stephenen_US
dc.contributor.authorDickinson, R. E.en_US
dc.contributor.authorCravens, Tom E.en_US
dc.contributor.authorNagy, Andrew F.en_US
dc.contributor.authorHedin, A. E.en_US
dc.contributor.authorKrasnopolsky, V. A.en_US
dc.contributor.authorNicholson, III, J. Y.en_US
dc.date.accessioned2006-04-07T19:12:53Z
dc.date.available2006-04-07T19:12:53Z
dc.date.issued1985en_US
dc.identifier.citationKeating, G. M., Bertaux, J. L., Bougher, S. W., Dickinson, R. E., Cravens, T. E., Nagy, A. F., Hedin, A. E., Krasnopolsky, V. A., Nicholson, III, J. Y. (1985)."Models of Venus neutral upper atmosphere: Structure and composition." Advances in Space Research 5(11): 117-171. <http://hdl.handle.net/2027.42/25840>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6V3S-472BDKD-N0/2/9d8980ee56550d86c23830fe753fd40aen_US
dc.identifier.urihttps://hdl.handle.net/2027.42/25840
dc.description.abstractModels of the Venus neutral upper atmosphere, based on both in-situ and remote sensing measurements, are provided for the height interval from 100 to 3,500 km. The general approach in model formulation was to divide the atmosphere into three regions: 100 to 150 km, 150 to 250 km, and 250 to 3,500 km. Boundary conditions at 150 km are consistent with both drag and mass spectrometer measurements. A paramount consideration was to keep the models simple enough to be used conveniently. Available observations are reviewed. Tables are provided for density, temperature, composition (CO2, O, CO, He, N, N2, and H), derived quantities, and day-to-day variability as a function of solar zenith angle on the day- and nightsides.Estimates are made of other species, including O2 and D. Other tables provide corrections for solar activity effects on temperature, composition, and density. For the exosphere, information is provided on the vertical distribution of normal thermal components (H, O, C, and He) as well as the hot components (H, N, C, O) on the day- and nightsides.en_US
dc.format.extent2625196 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleModels of Venus neutral upper atmosphere: Structure and compositionen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelAtmospheric, Oceanic and Space Sciencesen_US
dc.subject.hlbsecondlevelAerospace Engineeringen_US
dc.subject.hlbtoplevelScienceen_US
dc.subject.hlbtoplevelEngineeringen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumUniversity of Michigan, Ann Arbor, MI, U.S.A.en_US
dc.contributor.affiliationumUniversity of Michigan, Ann Arbor, MI, U.S.A.en_US
dc.contributor.affiliationotherNASA, Langley Research Center, Hampton, VA, U.S.A.en_US
dc.contributor.affiliationotherService d'Aéronomie du CNRS, Verrieres le Buisson, Franceen_US
dc.contributor.affiliationotherNational Center for Atmospheric Research, Boulder, CO, U.S.A.en_US
dc.contributor.affiliationotherNational Center for Atmospheric Research, Boulder, CO, U.S.A.en_US
dc.contributor.affiliationotherNASA, Goddard Space Flight Center, Greenbelt, MD, U.S.A.en_US
dc.contributor.affiliationotherSpace Research Institute, U.S.S.R. Academy of Sciences, Moscow 117810, U.S.S.R.en_US
dc.contributor.affiliationotherSystems and Applied Sciences Corp., Hampton, VA, U.S.A.en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/25840/1/0000403.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0273-1177(85)90200-5en_US
dc.identifier.sourceAdvances in Space Researchen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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