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Modelling of composition changes during F-region storms: a reassessment

dc.contributor.authorFuller-Rowell, T. J.en_US
dc.contributor.authorRees, D.en_US
dc.contributor.authorRishbeth, H.en_US
dc.contributor.authorBurns, A. G.en_US
dc.contributor.authorKilleen, Timothy L.en_US
dc.contributor.authorRoble, Raymond Geralden_US
dc.date.accessioned2006-04-10T14:42:36Z
dc.date.available2006-04-10T14:42:36Z
dc.date.issued1991en_US
dc.identifier.citationFuller-Rowell, T. J., Rees, D., Rishbeth, H., Burns, A. G., Killeen, T. L., Roble, R. G. (1991)."Modelling of composition changes during F-region storms: a reassessment." Journal of Atmospheric and Terrestrial Physics 53(6-7): 541-550. <http://hdl.handle.net/2027.42/29311>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6VSV-489SG8N-25/2/359ad06678112059b434ebe656702e99en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/29311
dc.description.abstractA recalculation of the global changes of thermospheric gas composition, resulting from strong heat inputs in the auroral ovals, shows that (contrary to some previous suggestions) widespread increases of mean molecular mass are produced at mid-latitudes, in summer and at equinox. Decreases of mean molecular mass occur at mid-latitudes in winter. Similar results are given by both the `UCL' and `NCAR TIGCM' three-dimensional models. The computed composition changes now seem consistent with the local time and seasonal response observed by satellites, and can broadly account for `negative storm effects' in the ionospheric F2-layer at mid-latitudes.en_US
dc.format.extent844402 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleModelling of composition changes during F-region storms: a reassessmenten_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbsecondlevelAtmospheric, Oceanic and Space Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumSpace Physics Research Laboratory, University of Michigan, Ann Arbor, MI 48105, U.S.A.en_US
dc.contributor.affiliationumSpace Physics Research Laboratory, University of Michigan, Ann Arbor, MI 48105, U.S.A.en_US
dc.contributor.affiliationotherDepartment of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, U.K.en_US
dc.contributor.affiliationotherDepartment of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, U.K.en_US
dc.contributor.affiliationotherDepartment of Physics, University of Southampton, Southampton SO9 5NH, U.K.en_US
dc.contributor.affiliationotherNational Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, U.S.A.en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/29311/1/0000375.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0021-9169(91)90081-Hen_US
dc.identifier.sourceJournal of Atmospheric and Terrestrial Physicsen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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