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dc.contributor.authorRobertson, Scott
dc.contributor.authorHorányi, Mihály
dc.contributor.authorKnappmiller, Scott
dc.contributor.authorSternovsky, Zoltan
dc.contributor.authorHolzworth, Robert H.
dc.contributor.authorShimogawa, Michelle M.
dc.contributor.authorFriedrich, Martin
dc.contributor.authorTorkar, Klaus
dc.contributor.authorGumbel, Jörg
dc.contributor.authorMegner, Linda
dc.contributor.authorBaumgarten, Gerd
dc.contributor.authorLatteck, Ralph
dc.contributor.authorRapp, Markus
dc.contributor.authorHoppe, Ulf-Peter
dc.contributor.authorHervig, Mark E.
dc.date.accessioned2017-10-30T12:45:08Z
dc.date.accessioned2017-10-31T08:13:59Z
dc.date.available2017-10-30T12:45:08Z
dc.date.available2017-10-31T08:13:59Z
dc.date.issued2009
dc.identifier.citationRobertson S, Horányi, Knappmiller S, Sternovsky Z, Holzworth, Shimogawa, Friedrich M, Torkar K, Gumbel J, Megner L, Baumgarten G, Latteck R, Rapp M, Hoppe U, Hervig. Mass analysis of charged aerosol particles in NLC and PMSE during the ECOMA/MASS campaign. Annales Geophysicae. 2009;27(3):1213-1232en_GB
dc.identifier.urihttp://hdl.handle.net/20.500.12242/756
dc.identifier.urihttps://ffi-publikasjoner.archive.knowledgearc.net/handle/20.500.12242/756
dc.descriptionRobertson, Scott; Horányi, Mihály; Knappmiller, Scott; Sternovsky, Zoltan; Holzworth, Robert H.; Shimogawa, Michelle M.; Friedrich, Martin; Torkar, Klaus; Gumbel, Jörg; Megner, Linda; Baumgarten, Gerd; Latteck, Ralph; Rapp, Markus; Hoppe, Ulf-Peter; Hervig, Mark E.. Mass analysis of charged aerosol particles in NLC and PMSE during the ECOMA/MASS campaign. Annales Geophysicae 2009 ;Volum 27.(3) s. 1213-1232en_GB
dc.description.abstractMASS (Mesospheric Aerosol Sampling Spectrometer) is a multichannel mass spectrometer for charged aerosol particles, which was flown from the Andoya Rocket Range, Norway, through NLC and PMSE on 3 August 2007 and through PMSE on 6 August 2007. The eight-channel analyzers provided for the first time simultaneous measurements of the charge density residing on aerosol particles in four mass ranges, corresponding to ice particles with radii <0.5 nm (including ions), 0.5-1 nm, 1-2 nm, and >3 nm (approximately). Positive and negative particles were recorded on separate channels. Faraday rotation measurements provided electron density and a means of checking charge density measurements made by the spectrometer. Additional complementary measurements were made by rocket-borne dust impact detectors, electric field booms, a photometer and ground-based radar and lidar. The MASS data from the first flight showed negative charge number densities of 1500 3000 cm(-3) for particles with radii >3 nm from 83-88 km approximately coincident with PMSE observed by the ALWIN radar and NLC observed by the ALOMAR lidar. For particles in the 1-2 nm range, number densities of positive and negative charge were similar in magnitude (similar to 2000 cm(-3)) and for smaller particles, 0.5-1 nm in radius, positive charge was dominant. The occurrence of positive charge on the aerosol particles of the smallest size and predominately negative charge on the particles of largest size suggests that nucleation occurs on positive condensation nuclei and is followed by collection of negative charge during subsequent growth to larger size. Faraday rotation measurements show a bite-out in electron density that increases the time for positive aerosol particles to be neutralized and charged negatively. The larger particles (>3 nm) are observed throughout the NLC region, 83-88 km, and the smaller particles are observed primarily at the high end of the range, 86-88 km. The second flight into PMSE alone at 84-88 km, found only small number densities (similar to 500 cm(-3)) of particles >3 nm in a narrow altitude range, 86.5-87.5 km. Both positive (similar to 2000 cm(-3)) and negative (similar to 4500 cm(-3)) particles with radii 1-2 nm were detected from 85-87.5 km.en_GB
dc.language.isoenen_GB
dc.titleMass analysis of charged aerosol particles in NLC and PMSE during the ECOMA/MASS campaignen_GB
dc.typeArticleen_GB
dc.date.updated2017-10-30T12:45:08Z
dc.identifier.cristinID347831
dc.identifier.cristinID347831
dc.identifier.doi10.5194/angeo-27-1213-2009
dc.source.issn0992-7689
dc.source.issn1432-0576
dc.type.documentJournal article
dc.relation.journalAnnales Geophysicae


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