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High-altitude and high-latitude O+ and H+ outflows: The effect of finite electromagnetic turbulence wavelength

dc.contributor.authorBarghouthi, I.A.
dc.contributor.authorDoudin, N.M.
dc.contributor.authorSaleh, A.A.
dc.contributor.authorPierrard, V.
dc.date2007
dc.date.accessioned2016-09-26T12:14:18Z
dc.date.available2016-09-26T12:14:18Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/4366
dc.languageeng
dc.relation.ispartofseries
dc.titleHigh-altitude and high-latitude O+ and H+ outflows: The effect of finite electromagnetic turbulence wavelength
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.subject.freealtitude
dc.subject.freeelectromagnetic wave
dc.subject.freeheating
dc.subject.freehydroxide
dc.subject.freelatitude
dc.subject.freeMonte Carlo analysis
dc.subject.freeoutflow
dc.subject.freepolar region
dc.subject.freeturbulence
dc.subject.freewave velocity
dc.subject.freewavelength
dc.source.titleAnnales Geophysicae
dc.source.volume25
dc.source.issue10
dc.source.page2195-2202
Orfeo.peerreviewedYes
dc.identifier.doi10.5194/angeo-25-2195-2007
dc.identifier.scopus2-s2.0-36049017413


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