Characterization of the planetary boundary layer during SAMUM-2 by means of lidar measurements

dc.bibliographicCitation.firstPage695
dc.bibliographicCitation.issue4eng
dc.bibliographicCitation.lastPage705
dc.bibliographicCitation.volume63
dc.contributor.authorGroß, Silke
dc.contributor.authorGasteiger, Josef
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorWiegner, Matthias
dc.contributor.authorGeiß, Alexander
dc.contributor.authorSchladitz, Alexander
dc.contributor.authorToledano, Carlos
dc.contributor.authorKandler, Konrad
dc.contributor.authorTesche, Matthias
dc.contributor.authorAnsmann, Albert
dc.contributor.authorWiedensohler, Alfred
dc.date.accessioned2018-02-02T04:35:25Z
dc.date.available2019-06-26T17:17:04Z
dc.date.issued2017
dc.description.abstractMeasurements with two Raman-depolarization lidars of the Meteorological Institute of the Ludwig-Maximilians- Universit¨at, M¨unchen, Germany, performed during SAMUM-2, were used to characterize the planetary boundary layer (PBL) over Praia, Cape Verde. A novel approach was used to determine the volume fraction of dust υd in the PBL. This approach primarily relies on accurate measurements of the linear depolarization ratio. Comparisons with independent in situ measurements showed the reliability of this approach. Based on our retrievals, two different phases could be distinguished within the measurement period of almost one month. The first (22–31 January 2008) was characterized by high aerosol optical depth (AOD) in the PBL and large υd > 95%. During the second phase, the AOD in the PBL was considerably lower and υd less than ∼40%. These findings were in very good agreement with ground based in situ measurements, when ambient volume fractions are considered that were calculated from the actual measurements of the dry volume fraction. Only in cases when dust was not the dominating aerosol component (second phase), effects due to hygroscopic growth became important.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/833
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/268
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2011.00557.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 63, Issue 4, Page 695-705eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaccuracy assessmenteng
dc.subjectaerosol propertyeng
dc.subjectboundary layereng
dc.subjectdusteng
dc.subjectground-based measurementeng
dc.subjecthygroscopicityeng
dc.subjectin situ measurementeng
dc.subjectlidareng
dc.subject.ddc550eng
dc.titleCharacterization of the planetary boundary layer during SAMUM-2 by means of lidar measurementseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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