Submicrometer aerosol particle distributions in the upper troposphere over the mid-latitude North Atlantic - Results from the third route of 'CARIBIC'

dc.bibliographicCitation.firstPage106
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
dc.bibliographicCitation.lastPage117
dc.bibliographicCitation.volume60
dc.contributor.authorHermann, M.
dc.contributor.authorBrenninkmeijer, C.A.M.
dc.contributor.authorSlemr, F.
dc.contributor.authorHeintzenberg, J.
dc.contributor.authorMartinsson, B.G.
dc.contributor.authorSchlager, H.
dc.contributor.authorVan Velthoven, P.F.J.
dc.contributor.authorWiedensohler, A.
dc.contributor.authorZahn, A.
dc.contributor.authorZiereis, H.
dc.date.accessioned2018-02-07T16:38:50Z
dc.date.available2019-06-26T17:17:20Z
dc.date.issued2017
dc.description.abstractParticle number and mass concentrations of submicrometer aerosol particles were determined for the upper troposphere over the mid-latitude North Atlantic within the Civil Aircraft for Regular Investigation of the Atmosphere Based on an Instrument Container project (CARIBIC, http://www.caribic-atmospheric.com). Between May 2001 and April 2002, 22 flights from Germany to the Caribbean were conducted using an automated measurement container on a B767 passenger aircraft. Spatial and seasonal probability distributions for ultrafine and Aitken mode particles as well as mass concentrations of particulate sulphur in 8–12 km altitude are presented. High particle number concentrations (mostly 2500–15 000 particles cm-3 STP) are particularly found in summer over the western North Atlantic Ocean close to the North American continent. The distributions together with an analysis of particle source processes show that deep vertical transport is the dominant process leading to most of the events with high particle number concentrations (8000 particles cm-3 STP) for ultrafine particles as well as for Aitken mode particles. This study emphasizes the importance of deep vertical transport and cloud processing for the concentration of aerosol particles in the upper troposphere.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1285
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/368
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2007.00323.x
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otheraerosoleng
dc.subject.otherconcentration (composition)eng
dc.subject.othermeasurement methodeng
dc.subject.otherprobabilityeng
dc.subject.otherspatial distributioneng
dc.subject.othertransport processeng
dc.subject.othertroposphereeng
dc.titleSubmicrometer aerosol particle distributions in the upper troposphere over the mid-latitude North Atlantic - Results from the third route of 'CARIBIC'eng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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