Dual-FOV Raman and Doppler lidar studies of aerosol-cloud interactions: Simultaneous profiling of aerosols, warm-cloud properties, and vertical wind

dc.bibliographicCitation.firstPage5512
dc.bibliographicCitation.issue9eng
dc.bibliographicCitation.lastPage5527
dc.bibliographicCitation.volume119
dc.contributor.authorSchmidt, Jörg
dc.contributor.authorAnsmann, Albert
dc.contributor.authorBühl, Johannes
dc.contributor.authorBaars, Holger
dc.contributor.authorWandinger, Ulla
dc.contributor.authorMüller, Detlef
dc.contributor.authorMalinka, Aleksey V.
dc.date.accessioned2018-01-29T18:43:30Z
dc.date.available2019-06-26T17:21:48Z
dc.date.issued2014
dc.description.abstractFor the first time, colocated dual-field of view (dual-FOV) Raman lidar and Doppler lidar observations (case studies) of aerosol and cloud optical and microphysical properties below and within thin layered liquid water clouds are presented together with an updraft and downdraft characterization at cloud base. The goal of this work is to investigate the relationship between aerosol load close to cloud base and cloud characteristics of warm (purely liquid) clouds and the study of the influence of vertical motions and turbulent mixing on this relationship. We further use this opportunity to illustrate the applicability of the novel dual-FOV Raman lidar in this field of research. The dual-FOV lidar combines the well-established multiwavelength Raman lidar technique for aerosol retrievals and the multiple-scattering Raman lidar technique for profiling of the single-scattering extinction coefficient, effective radius, number concentration of the cloud droplets, and liquid water content. Key findings of our 3 year observations are presented in several case studies of optically thin altocumulus layers occurring in the lower free troposphere between 2.5 and 4 km height over Leipzig, Germany, during clean and polluted situations. For the clouds that we observed, the most direct link between aerosol proxy (particle extinction coefficient) and cloud proxy (cloud droplet number concentration) was found at cloud base during updraft periods. Above cloud base, additional processes resulting from turbulent mixing and entrainment of dry air make it difficult to determine the direct impact of aerosols on cloud processes.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/885
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/890
dc.language.isoengeng
dc.publisherHoboken, NJ : Wileyeng
dc.relation.doihttps://doi.org/10.1002/2013JD020424
dc.relation.ispartofseriesJournal of Geophysical Research: Atmospheres, Volume 119, Issue 9, Page 5512-5527eng
dc.rights.licenseCC BY-NC-ND 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/eng
dc.subjectA new lidar technique to derive cloud microphysical properties is appliedeng
dc.subjectA comparison of droplet sizes of two clouds complies with the Twomey effecteng
dc.subjectThe influence of the vertical wind speed on cloud microphysics is investigatedeng
dc.subject.ddc550eng
dc.titleDual-FOV Raman and Doppler lidar studies of aerosol-cloud interactions: Simultaneous profiling of aerosols, warm-cloud properties, and vertical windeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleJournal of Geophysical Research: Atmosphereseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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