Profiles of cloud condensation nuclei, dust mass concentration, and ice-nucleating-particle-relevant aerosol properties in the Saharan Air Layer over Barbados from polarization lidar and airborne in situ measurements

dc.bibliographicCitation.firstPage13773eng
dc.bibliographicCitation.issue22eng
dc.bibliographicCitation.lastPage13788eng
dc.bibliographicCitation.volume19eng
dc.contributor.authorHaarig, Moritz
dc.contributor.authorWalser, Adrian
dc.contributor.authorAnsmann, Albert
dc.contributor.authorDollner, Maximilian
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorSauer, Daniel
dc.contributor.authorFarrell, David
dc.contributor.authorWeinzierl, Bernadett
dc.date.accessioned2021-09-30T09:46:34Z
dc.date.available2021-09-30T09:46:34Z
dc.date.issued2019
dc.description.abstractThe present study aims to evaluate lidar retrievals of cloud-relevant aerosol properties by using polarization lidar and coincident airborne in situ measurements in the Saharan Air Layer (SAL) over the Barbados region. Vertical profiles of the number concentration of cloud condensation nuclei (CCN), large particles (diameter d > 500 nm), surface area, mass, and ice-nucleating particle (INP) concentration are derived from the lidar measurements and compared with CCN concentrations and the INP-relevant aerosol properties measured in situ with aircraft. The measurements were performed in the framework of the Saharan Aerosol Longrange Transport and Aerosol-Cloud-Interaction Experiment (SALTRACE) in summer 2013. The CCN number concentrations derived from lidar observations were up to a factor of 2 higher than the ones measured in situ aboard the research aircraft Falcon. Possible reasons for the difference are discussed. The number concentration of particles with a dry radius of more than 250 nm and the surface-area concentration obtained from the lidar observations and used as input for the INP parameterizations agreed well (< 30 %-50 % deviation) with the aircraft measurements. In a pronounced lofted dust layer during summer (10 July 2013), the lidar retrieval yielded 100-300 CCN per cubic centimeter at 0.2 % water supersaturation and 10-200 INPs per liter at-25?C. Excellent agreement was also obtained in the comparison of mass concentration profiles. During the SALTRACE winter campaign (March 2014), the dust layer from Africa was mixed with smoke particles which dominated the CCN number concentration. This example highlights the unique lidar potential to separate smoke and dust contributions to the CCN reservoir and thus to identify the sensitive role of smoke in trade wind cumuli developments over the tropical Atlantic during the winter season. © 2017 Georg Thieme Verlag. All rights reserved.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6952
dc.identifier.urihttps://doi.org/10.34657/5999
dc.language.isoengeng
dc.publisherKatlenburg-Lindau : EGUeng
dc.relation.doihttps://doi.org/10.5194/acp-19-13773-2019
dc.relation.essn1680-7324
dc.relation.ispartofseriesAtmospheric chemistry and physics 19 (2019), Nr. 22eng
dc.relation.issn1680-7316
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosoleng
dc.subjectaerosol propertyeng
dc.subjectcloud condensation nucleuseng
dc.subjectconcentration (composition)eng
dc.subjectdusteng
dc.subjectin situ measurementeng
dc.subjectlidareng
dc.subjectparticulate mattereng
dc.subjectpolarizationeng
dc.subjectBarbadoseng
dc.subjectSaharaeng
dc.subjectFalconidaeeng
dc.subject.ddc550eng
dc.titleProfiles of cloud condensation nuclei, dust mass concentration, and ice-nucleating-particle-relevant aerosol properties in the Saharan Air Layer over Barbados from polarization lidar and airborne in situ measurementseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric chemistry and physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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