Aerosol number size distributions from 3 to 500 nm diameter in the arctic marine boundary layer during summer and autumn

dc.bibliographicCitation.firstPage197eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.volume48eng
dc.contributor.authorCovert, D.S.
dc.contributor.authorWiedensohler, A.
dc.contributor.authorAalto, P.
dc.contributor.authorHeintzenberg, J.
dc.contributor.authorMcmurry, P.H.
dc.contributor.authorLeck, C.
dc.date.accessioned2020-08-07T13:48:33Z
dc.date.available2020-08-07T13:48:33Z
dc.date.issued1996
dc.description.abstractAerosol physics measurements made onboard the Swedish icebreaker Oden in the late Summer and early Autumn of 1991 during the International Arctic Ocean Expedition (IAOE-91) have provided the first data on the size distribution of particles in the Arctic marine boundary layer (MBL) that cover both the number and mass modes of the size range from 3 to 500 nm diameter. These measurements were made in conjunction with atmospheric gas and condensed phase chemistry measurements in an effort to understand a part of the ocean-atmosphere sulfur cycle. Analysis of the particle physics data showed that there were three distinct number modes in the submicrometric aerosol in the Arctic MBL. These modes had geometric mean diameters of around 170 nm. 45 nm and 14 nm referred to as accumulation, Aitken and ultrafine modes, respectively. There were clear minima in number concentrations between the modes that appeared at 20 to 30 nm and at 80 to 100 nm. The total number concentration was most frequently between 30 and 60 particles cm-3 with a mean value of around 100 particles cm-3, but the hourly average concentration varied over two to three orders of magnitude during the 70 days of the expedition. On average, the highest concentration was in the accumulation mode that contained about 45% of the total number, while the Aitken mode contained about 40%. The greatest variability was in the ultrafine mode concentration which is indicative of active, earby sources (nucleation from the gas phase) and sinks; the Aitken and accumulation mode concentrations were much less variable. The ultrafine mode was observed about two thirds of the time and was dominant 10% of the time. A detailed description and statistical analysis of the modal aerosol parameters is presented here.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5414
dc.identifier.urihttps://doi.org/10.34657/4043
dc.language.isoengeng
dc.publisherCopenhagen : Blackwell Munksgaardeng
dc.relation.doihttps://doi.org/10.3402/tellusb.v48i2.15886
dc.relation.ispartofseriesTellus, Series B: Chemical and Physical Meteorology 48 (1996), Nr. 2eng
dc.relation.issn0280-6509
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaccumulation modeeng
dc.subjectaerosol sizeeng
dc.subjectaerosolseng
dc.subjectAitken modeeng
dc.subjectIAOEeng
dc.subjectIAOE-91eng
dc.subjectmarine boundary layereng
dc.subjectoceanic boundary layereng
dc.subjectparticle number modeeng
dc.subjectshipborne observationeng
dc.subjectsize distributionseng
dc.subjectstatistical analysiseng
dc.subjectultrafine modeeng
dc.subjectArctic Oceaneng
dc.subject.ddc550eng
dc.titleAerosol number size distributions from 3 to 500 nm diameter in the arctic marine boundary layer during summer and autumneng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus, Series B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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