A broad supersaturation scanning (BS2) approach for rapid measurement of aerosol particle hygroscopicity and cloud condensation nuclei activity

dc.bibliographicCitation.firstPage5183eng
dc.bibliographicCitation.issue10eng
dc.bibliographicCitation.lastPage5192eng
dc.bibliographicCitation.volume9
dc.contributor.authorSu, Hang
dc.contributor.authorCheng, Yafang
dc.contributor.authorMa, Nan
dc.contributor.authorWang, Zhibin
dc.contributor.authorWang, Xiaoxiang
dc.contributor.authorPöhlker, Mira L.
dc.contributor.authorNillius, Björn
dc.contributor.authorWiedensohler, Alfred
dc.contributor.authorPöschl, Ulrich
dc.date.accessioned2017-12-09T00:19:21Z
dc.date.available2019-06-26T17:19:56Z
dc.date.issued2016
dc.description.abstractThe activation and hygroscopicity of cloud condensation nuclei (CCN) are key to the understanding of aerosol–cloud interactions and their impact on climate. They can be measured by scanning the particle size and supersaturation in CCN measurements. The scanning of supersaturation is often time-consuming and limits the temporal resolution and performance of CCN measurements. Here we present a new approach, termed the broad supersaturation scanning (BS2) method, in which a range of supersaturation is simultaneously scanned, reducing the time interval between different supersaturation scans. The practical applicability of the BS2 approach is demonstrated with nano-CCN measurements of laboratory-generated aerosol particles. Model simulations show that the BS2 approach may also be applicable for measuring CCN activation of ambient mixed particles. Due to its fast response and technical simplicity, the BS2 approach may be well suited for aircraft and long-term measurements. Since hygroscopicity is closely related to the fraction of organics/inorganics in aerosol particles, a BS2-CCN counter can also serve as a complementary sensor for fast detection/estimation of aerosol chemical compositions.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/723
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/726
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/amt-9-5183-2016
dc.relation.ispartofseriesAtmospheric Measurement Techniques, Volume 9, Issue 10, Page 5183-5192eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaerosoleng
dc.subjectaerosol compositioneng
dc.subjectairborne surveyeng
dc.subjectcloud condensation nucleuseng
dc.subjecthygroscopicityeng
dc.subjectnumerical methodeng
dc.subjectparticle sizeeng
dc.subjectsupersaturationeng
dc.subjectvolcanic cloudeng
dc.subject.ddc550eng
dc.titleA broad supersaturation scanning (BS2) approach for rapid measurement of aerosol particle hygroscopicity and cloud condensation nuclei activityeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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