A new method of inferring the size, number density, and charge of mesospheric dust from its in situ collection by the DUSTY probe

dc.bibliographicCitation.firstPage1673eng
dc.bibliographicCitation.issue3eng
dc.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
dc.bibliographicCitation.lastPage1683eng
dc.bibliographicCitation.volume12eng
dc.contributor.authorHavnes, Ove
dc.contributor.authorAntonsen, Tarjei
dc.contributor.authorBaumgarten, Gerd
dc.contributor.authorHartquist, Thomas W.
dc.contributor.authorBiebricher, Alexander
dc.contributor.authorFredriksen, Åshild
dc.contributor.authorFriedrich, Martin
dc.contributor.authorHedin, Jonas
dc.date.accessioned2021-08-19T11:44:39Z
dc.date.available2021-08-19T11:44:39Z
dc.date.issued2019
dc.description.abstractWe present a new method of analyzing measurements of mesospheric dust made with DUSTY rocket-borne Faraday cup probes. It can yield the variation in fundamental dust parameters through a mesospheric cloud with an altitude resolution down to 10 cm or less if plasma probes give the plasma density variations with similar height resolution. A DUSTY probe was the first probe that unambiguously detected charged dust and aerosol particles in the Earth's mesosphere. DUSTY excluded the ambient plasma by various biased grids, which however allowed dust particles with radii above a few nanometers to enter, and it measured the flux of charged dust particles. The flux measurements directly yielded the total ambient dust charge density. We extend the analysis of DUSTY data by using the impact currents on its main grid and the bottom plate as before, together with a dust charging model and a secondary charge production model, to allow the determination of fundamental parameters, such as dust radius, charge number, and total dust density. We demonstrate the utility of the new analysis technique by considering observations made with the DUSTY probes during the MAXIDUSTY rocket campaign in June-July 2016 and comparing the results with those of other instruments (lidar and photometer) also used in the campaign. In the present version we have used monodisperse dust size distributions.© Author(s) 2019.eng
dc.description.fondsLeibniz_Fonds
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6534
dc.identifier.urihttps://doi.org/10.34657/5581
dc.language.isoengeng
dc.publisherKatlenburg-Lindau : Copernicuseng
dc.relation.doihttps://doi.org/10.5194/amt-12-1673-2019
dc.relation.essn1867-8548
dc.relation.issn1867-1381
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otherDUSTYeng
dc.subject.othermesospheric dusteng
dc.subject.othermesospheric cloudeng
dc.titleA new method of inferring the size, number density, and charge of mesospheric dust from its in situ collection by the DUSTY probeeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorIAPeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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