Please use this identifier to cite or link to this item: https://oar.tib.eu/jspui/handle/123456789/455
Full metadata record
DC FieldValueLanguage
dc.rights.licenseCC BY 3.0 Unportedger
dc.contributor.authorHamed, A.
dc.contributor.authorBirmili, W.
dc.contributor.authorJoutsensaari, J.
dc.contributor.authorMikkonen, S.
dc.contributor.authorAsmi, A.
dc.contributor.authorWehner, B.
dc.contributor.authorSpindler, G.
dc.contributor.authorJaatinen, A.
dc.contributor.authorWiedensohler, A.
dc.contributor.authorKorhonen, H.
dc.contributor.authorLehtinen, K. E. J.
dc.contributor.authorLaaksonen, A.
dc.date.accessioned2017-11-08T18:30:43Z
dc.date.available2019-06-26T17:17:43Z
dc.date.issued2010
dc.identifier.urihttps://oar.tib.eu/jspui/handle/123456789/455
dc.identifier.urihttp://dx.doi.org/10.34657/809-
dc.description.abstractIn anthropogenically influenced atmospheres, sulphur dioxide (SO2) is the main precursor of gaseous sulphuric acid (H2SO4), which in turn is a main precursor for atmospheric particle nucleation. As a result of socio-economic changes, East Germany has seen a dramatic decrease in anthropogenic SO2 emissions between 1989 and present, as documented by routine air quality measurements in many locations. We have attempted to evaluate the influence of changing SO2 concentrations on the frequency and intensity of new particle formation (NPF) using two different data sets (1996–1997; 2003–2006) of experimental particle number size distributions (diameter range 3–750 nm) from the atmospheric research station Melpitz near Leipzig, Germany. Between the two periods SO2 concentrations decreased by 65% on average, while the frequency of NPF events dropped by 45%. Meanwhile, the average formation rate of 3 nm particles decreased by 68% on average. The trends were statistically significant and therefore suggest a connection between the availability of anthropogenic SO2 and freshly formed new particles. In contrast to the decrease in new particle formation, we found an increase in the mean growth rate of freshly nucleated particles (+22%), suggesting that particle nucleation and subsequent growth into larger sizes are delineated with respect to their precursor species. Using three basic parameters, the condensation sink for H2SO4, the SO2 concentration, and the global radiation intensity, we were able to define the characteristic range of atmospheric conditions under which particle formation events take place at the Melpitz site. While the decrease in the concentrations and formation rates of the new particles was rather evident, no similar decrease was found with respect to the generation of cloud condensation nuclei (CCN; particle diameter >100 nm) as a result of atmospheric nucleation events. On the contrary, the production of CCN following nucleation events appears to have increased by tens of percents. Our aerosol dynamics model simulations suggest that such an increase can be caused by the increased particle growth rate.
dc.formatapplication/pdf
dc.languageeng
dc.publisherMünchen : European Geopyhsical Union
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 10, Issue 3, Page 1071-1091-
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/ger
dc.subjectaerosol formation
dc.subjectair quality
dc.subjectcloud condensation nucleus
dc.subjectconcentration (composition)
dc.subjectcondensation
dc.subjectgrowth rate
dc.subjectnucleation
dc.subjectparticle size
dc.subjectresearch institution
dc.subjectsize distribution
dc.subjectsulfur dioxide
dc.subjectsulfur emission
dc.subjectsulfuric acid
dc.subject.ddc550
dc.titleChanges in the production rate of secondary aerosol particles in Central Europe in view of decreasing SO2 emissions between 1996 and 2006
dc.typearticle-
dc.typeText-
dc.description.versionpublishedVersioneng
local.accessRightsopenAccess-
wgl.contributorTROPOSger
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
dc.relation.doihttps://doi.org/10.5194/acp-10-1071-2010
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physics-
local.identifier.doihttp://dx.doi.org/10.34657/809-
Appears in Collections:Geowissenschaften

Files in This Item:
File SizeFormat 
acp-10-1071-2010.pdf1.62 MBAdobe PDFView/Open


This item is licensed under a Creative Commons License Creative Commons