Aerosol particle number size distributions and particulate light absorption at the ZOTTO tall tower (Siberia), 2006–2009

dc.bibliographicCitation.firstPage8703eng
dc.bibliographicCitation.issue16eng
dc.bibliographicCitation.lastPage8719eng
dc.bibliographicCitation.volume11
dc.contributor.authorHeintzenberg, J.
dc.contributor.authorBirmili, W.
dc.contributor.authorOtto, R.
dc.contributor.authorAndreae, M.O.
dc.contributor.authorMayer, J.-C.
dc.contributor.authorChi, X.
dc.contributor.authorPanov, A.
dc.date.accessioned2017-11-09T18:30:56Z
dc.date.available2019-06-26T17:17:50Z
dc.date.issued2011
dc.description.abstractThis paper analyses aerosol particle number size distributions, particulate absorption at 570 nm wavelength and carbon monoxide (CO) measured between September 2006 and January 2010 at heights of 50 and 300 m at the Zotino Tall Tower Facility (ZOTTO) in Siberia (60.8° N; 89.35° E). Average number, surface and volume concentrations are broadly comparable to former studies covering shorter observation periods. Fits of multiple lognormal distributions yielded three maxima in probability distribution of geometric mean diameters in the Aitken and accumulation size range and a possible secondary maximum in the nucleation size range below 25 nm. The seasonal cycle of particulate absorption shows maximum concentrations in high winter (December) and minimum concentrations in mid-summer (July). The 90th percentile, however, indicates a secondary maximum in July/August that is likely related to forest fires. The strongly combustion derived CO shows a single winter maximum and a late summer minimum, albeit with a considerably smaller seasonal swing than the particle data due to its longer atmospheric lifetime. Total volume and even more so total number show a more complex seasonal variation with maxima in winter, spring, and summer. A cluster analysis of back trajectories and vertical profiles of the pseudo-potential temperature yielded ten clusters with three levels of particle number concentration: Low concentrations in Arctic air masses (400–500 cm−3), mid-level concentrations for zonally advected air masses from westerly directions between 55° and 65° N (600–800 cm−3), and high concentrations for air masses advected from the belt of industrial and population centers in Siberia and Kazakhstan (1200 cm−3). The observational data is representative for large parts of the troposphere over Siberia and might be particularly useful for the validation of global aerosol transport models.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/753
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/474
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-11-8703-2011
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 11, Issue 16, Page 8703-8719eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectabsorptioneng
dc.subjectadvectioneng
dc.subjectaerosoleng
dc.subjectair masseng
dc.subjectAitken nucleuseng
dc.subjectatmospheric transporteng
dc.subjectcarbon monoxideeng
dc.subjectconcentration (composition)eng
dc.subjectparticle sizeeng
dc.subjectseasonal variationeng
dc.subjectsize distributioneng
dc.subjecttroposphereeng
dc.subjectwavelengtheng
dc.subject.ddc550eng
dc.titleAerosol particle number size distributions and particulate light absorption at the ZOTTO tall tower (Siberia), 2006–2009eng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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