Please use this identifier to cite or link to this item: https://oa.tib.eu/renate/jspui/handle/123456789/381
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dc.rights.licenseCC BY 4.0 Unporteden
dc.contributor.authorHeintzenberg, Jost
dc.contributor.authorBirmili, Wolfram
dc.contributor.authorTheiss, Detlef
dc.contributor.authorKisilyakhov, Yegor
dc.date.accessioned2018-02-07T16:38:51Z
dc.date.available2019-06-26T17:17:24Z
dc.date.issued2017
dc.identifier.urihttps://oar.tib.eu/jspui/handle/123456789/381
dc.identifier.urihttp://dx.doi.org/10.34657/1313-
dc.description.abstractThis report describes a unique setup for aerosol measurements at the new long-term Tall Tower monitoring facility near Zotino, Siberia (ZOTTO). Through two inlets at 50 and 300 m aerosol particle number size distributions are measured since September 2006 in the size range 15–835 nanometer dry diameter. Until the end of May 2007 total number (N300) concentrations at 300 m height ranged between 400 cm-3 (5%) and 4000 cm-3 (95%) with a median of 1200 cm-3, which is rather high for a nearly uninhabited boreal forest region during the low productivity period of the year. Fitting 1-h average distributions with a maximum of four lognormal functions yielded frequent ultrafine modes below 20 nm at 50 m height than at 300 m, whereas the latter height more frequently showed an aged nucleation mode near 30 nm. The positions of Aitken (≈80 nm) and accumulation modes (≈210 nm) were very similar at both inlet heights, the very sharp latter one being the most frequent of all modes. The encouraging first results let us expect exciting newfindings during the summer period with frequent forest fires and secondary particle sources from vegetation emissions.
dc.formatapplication/pdf
dc.language.isoengen
dc.publisherMilton Park : Taylor & Francis
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 60, Issue 2, Page 276-285en
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en
dc.subjectaerosol
dc.subjectboreal forest
dc.subjectforest fire
dc.subjectnucleation
dc.subjectparticle size
dc.subjectsize distribution
dc.subject.ddc550
dc.titleThe atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower
dc.typearticle-
dc.typeText-
dc.description.versionpublishedVersioneng
local.accessRightsopenAccess-
wgl.contributorTROPOSger
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2007.00335.x
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyen
local.identifier.doihttp://dx.doi.org/10.34657/1313-
Appears in Collections:Geowissenschaften

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Heintzenberg, Jost, Wolfram Birmili, Detlef Theiss and Yegor Kisilyakhov, 2017. The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower. 2017. Milton Park : Taylor & Francis
Heintzenberg, J., Birmili, W., Theiss, D. and Kisilyakhov, Y. (2017) “The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower.” Milton Park : Taylor & Francis. doi: https://doi.org/10.1111/j.1600-0889.2007.00335.x.
Heintzenberg J, Birmili W, Theiss D, Kisilyakhov Y. The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower. Milton Park : Taylor & Francis; 2017.
Heintzenberg, J., Birmili, W., Theiss, D., & Kisilyakhov, Y. (2017). The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower (Version publishedVersion). Version publishedVersion. Milton Park : Taylor & Francis. https://doi.org/https://doi.org/10.1111/j.1600-0889.2007.00335.x
Heintzenberg J, Birmili W, Theiss D, Kisilyakhov Y. The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower. Published online 2017. doi:https://doi.org/10.1111/j.1600-0889.2007.00335.x


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