African smoke particles act as cloud condensation nuclei in the wintertime tropical North Atlantic boundary layer over Barbados

dc.bibliographicCitation.firstPage981
dc.bibliographicCitation.issue2
dc.bibliographicCitation.lastPage998
dc.bibliographicCitation.volume23
dc.contributor.authorRoyer, Haley M.
dc.contributor.authorPöhlker, Mira L.
dc.contributor.authorKrüger, Ovid
dc.contributor.authorBlades, Edmund
dc.contributor.authorSealy, Peter
dc.contributor.authorLata, Nurun Nahar
dc.contributor.authorCheng, Zezhen
dc.contributor.authorChina, Swarup
dc.contributor.authorAult, Andrew P.
dc.contributor.authorQuinn, Patricia K.
dc.contributor.authorZuidema, Paquita
dc.contributor.authorPöhlker, Christopher
dc.contributor.authorPöschl, Ulrich
dc.contributor.authorAndreae, Meinrat
dc.contributor.authorGaston, Cassandra J.
dc.date.accessioned2023-06-02T15:01:19Z
dc.date.available2023-06-02T15:01:19Z
dc.date.issued2023
dc.description.abstractThe number concentration and properties of aerosol particles serving as cloud condensation nuclei (CCN) are important for understanding cloud properties, including in the tropical Atlantic marine boundary layer (MBL), where marine cumulus clouds reflect incoming solar radiation and obscure the low-albedo ocean surface. Studies linking aerosol source, composition, and water uptake properties in this region have been conducted primarily during the summertime dust transport season, despite the region receiving a variety of aerosol particle types throughout the year. In this study, we compare size-resolved aerosol chemical composition data to the hygroscopicity parameter κ derived from size-resolved CCN measurements made during the Elucidating the Role of Clouds-Circulation Coupling in Climate (EUREC4A) and Atlantic Tradewind Ocean-Atmosphere Mesoscale Interaction Campaign (ATOMIC) campaigns from January to February 2020. We observed unexpected periods of wintertime long-range transport of African smoke and dust to Barbados. During these periods, the accumulation-mode aerosol particle and CCN number concentrations as well as the proportions of dust and smoke particles increased, whereas the average κ slightly decreased (κCombining double low line0.46±0.10) from marine background conditions (κCombining double low line0.52±0.09) when the submicron particles were mostly composed of marine organics and sulfate. Size-resolved chemical analysis shows that smoke particles were the major contributor to the accumulation mode during long-range transport events, indicating that smoke is mainly responsible for the observed increase in CCN number concentrations. Earlier studies conducted at Barbados have mostly focused on the role of dust on CCN, but our results show that aerosol hygroscopicity and CCN number concentrations during wintertime long-range transport events over the tropical North Atlantic are also affected by African smoke. Our findings highlight the importance of African smoke for atmospheric processes and cloud formation over the Caribbean.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/12290
dc.identifier.urihttp://dx.doi.org/10.34657/11322
dc.language.isoeng
dc.publisherKatlenburg-Lindau : EGU
dc.relation.doihttps://doi.org/10.5194/acp-23-981-2023
dc.relation.essn1680-7324
dc.relation.ispartofseriesAtmospheric Chemistry and Physics 23 (2023), Nr. 2eng
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectaerosoleng
dc.subjectboundary layereng
dc.subjectchemical compositioneng
dc.subjectcloud condensation nucleuseng
dc.subjectconcentration (composition)eng
dc.subject.ddc550
dc.titleAfrican smoke particles act as cloud condensation nuclei in the wintertime tropical North Atlantic boundary layer over Barbadoseng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physics
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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