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dc.contributor.authorHall, Chris
dc.date.accessioned2007-01-24T10:06:38Z
dc.date.available2007-01-24T10:06:38Z
dc.date.issued2002
dc.description.abstractBy measuring fading times of radar echoes from underdense meteor trails, it is possible to deduce the ambipolar diffusivities of the ions responsible for these radar echoes. It could be anticipated that these diffusivities increase monotonically with height akin to neutral viscosity. In practice, this is not always the case. Here, we investigate the capability of neutral turbulence to affect the meteor trail diffusion rate.en
dc.format.extent205220 bytes
dc.format.mimetypeapplication/pdf
dc.identifier.issn1432-0576 (elektronisk)
dc.identifier.urihttps://hdl.handle.net/10037/562
dc.identifier.urnURN:NBN:no-uit_munin_389
dc.language.isoengen
dc.publisherEuropean Geosciences Unionen
dc.relation.ispartofseriesAnnales Geophysicae 20(2002), pp 1857-1862en
dc.rights.accessRightsopenAccess
dc.subjectmeteorology and atmospheric dynamicsen
dc.subjectmiddle atmosphere dynamicsen
dc.subjectturbulenceen
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453en
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Fysikk: 430en
dc.titleOn the influence of neutral turbulence on ambipolar diffusivities deduced from meteor trail expansion.en
dc.typeJournal articleen
dc.typePeer reviewed
dc.typeTidsskriftartikkelno


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