Near-global aerosol mapping in the upper troposphere and lowermost stratosphere with data from the CARIBIC project

dc.bibliographicCitation.firstPage875
dc.bibliographicCitation.issue5eng
dc.bibliographicCitation.lastPage890
dc.bibliographicCitation.volume63
dc.contributor.authorHeintzenberg, Jost
dc.contributor.authorHermann, Markus
dc.contributor.authorWeigelt, Andreas
dc.contributor.authorKapustin, Vladimir
dc.contributor.authorAnderson, Bruce
dc.contributor.authorThornhill, Kenneth
dc.contributor.authorVan Velthoven, Peter
dc.contributor.authorZahn, Andreas
dc.contributor.authorBrenninkmeijer, Carl
dc.date.accessioned2018-02-02T04:35:24Z
dc.date.available2019-06-26T17:17:03Z
dc.date.issued2017
dc.description.abstractThis study extrapolates aerosol data of the CARIBIC project from 1997 until June 2008 in along trajectories to compose large-scale maps and vertical profiles of submicrometre particle concentrations in the upper troposphere and lowermost stratosphere (UT/LMS). The extrapolation was validated by comparing extrapolated values with CARIBIC data measured near the respective trajectory position and by comparing extrapolated CARIBIC data to measurements by other experiments near the respective trajectory positions. Best agreement between extrapolated and measured data is achieved with particle lifetimes longer than the maximum length of used trajectories. The derived maps reveal regions of strong and frequent new particle formation, namely the Tropical Central and Western Africa with the adjacent Atlantic, South America, the Caribbean and Southeast Asia. These regions of particle formation coincide with those of frequent deep convective clouds. Vertical particle concentration profiles for the troposphere and the stratosphere confirm statistically previous results indicating frequent new particle formation in the tropopause region. There was no statistically significant increase in Aitken mode particle concentration between the first period of CARIBIC operation, 1997–2002, and the second period, 2004–2009. However, a significant increase in concentration occurred within the latter period when considering it in isolation.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1115
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/260
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2011.00578.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 63, Issue 5, Page 875-890eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosoleng
dc.subjectconcentration (composition)eng
dc.subjectconvective cloudeng
dc.subjectmappingeng
dc.subjectstatistical analysiseng
dc.subjectstratosphereeng
dc.subjecttroposphereeng
dc.subject.ddc550eng
dc.titleNear-global aerosol mapping in the upper troposphere and lowermost stratosphere with data from the CARIBIC projecteng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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