Microphysical characterization of long-range transported biomass burning particles from North America at three EARLINET stations

dc.bibliographicCitation.firstPage5931
dc.bibliographicCitation.issue9
dc.bibliographicCitation.journalTitleAtmospheric chemistry and physicseng
dc.bibliographicCitation.lastPage5946
dc.bibliographicCitation.volume17
dc.contributor.authorOrtiz-Amezcua, Pablo
dc.contributor.authorGuerrero-Rascado, Juan Luis
dc.contributor.authorGranados-Muñoz, María José
dc.contributor.authorBenavent-Oltra, José Antonio
dc.contributor.authorBöckmann, Christine
dc.contributor.authorSamaras, Stefanos
dc.contributor.authorStachlewska, Iwona S.
dc.contributor.authorJanicka, Łucja
dc.contributor.authorBaars, Holger
dc.contributor.authorBohlmann, Stephanie
dc.contributor.authorAlados-Arboledas, Lucas
dc.date.accessioned2023-03-07T10:42:54Z
dc.date.available2023-03-07T10:42:54Z
dc.date.issued2017
dc.description.abstractStrong events of long-range transported biomass burning aerosol were detected during July 2013 at three EARLINET (European Aerosol Research Lidar Network) stations, namely Granada (Spain), Leipzig (Germany) and Warsaw (Poland). Satellite observations from MODIS (Moderate Resolution Imaging Spectroradiometer) and CALIOP (Cloud-Aerosol Lidar with Orthogonal Polarization) instruments, as well as modeling tools such as HYSPLIT (Hybrid Single-Particle Lagrangian Integrated Trajectory) and NAAPS (Navy Aerosol Analysis and Prediction System), have been used to estimate the sources and transport paths of those North American forest fire smoke particles. A multiwavelength Raman lidar technique was applied to obtain vertically resolved particle optical properties, and further inversion of those properties with a regularization algorithm allowed for retrieving microphysical information on the studied particles. The results highlight the presence of smoke layers of 1-2 km thickness, located at about 5 km a.s.l. altitude over Granada and Leipzig and around 2.5 km a.s.l. at Warsaw. These layers were intense, as they accounted for more than 30 % of the total AOD (aerosol optical depth) in all cases, and presented optical and microphysical features typical for different aging degrees: Color ratio of lidar ratios (LR532/LR355) around 2, α-related ängström exponents of less than 1, effective radii of 0.3 μm and large values of single scattering albedos (SSA), nearly spectrally independent. The intensive microphysical properties were compared with columnar retrievals form co-located AERONET (Aerosol Robotic Network) stations. The intensity of the layers was also characterized in terms of particle volume concentration, and then an experimental relationship between this magnitude and the particle extinction coefficient was established.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11718
dc.identifier.urihttp://dx.doi.org/10.34657/10751
dc.language.isoeng
dc.publisherKatlenburg-Lindau : EGU
dc.relation.doihttps://doi.org/10.5194/acp-17-5931-2017
dc.relation.essn1680-7324
dc.rights.licenseCC BY 3.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/3.0
dc.subject.ddc550
dc.subject.otheraerosoleng
dc.subject.otheralgorithmeng
dc.subject.otherbiomass burningeng
dc.subject.otherCALIOPeng
dc.subject.otherlidareng
dc.subject.otherlong range transporteng
dc.subject.otherMODISeng
dc.subject.otheroptical deptheng
dc.subject.otherparticulate mattereng
dc.subject.otherNorth Americaeng
dc.titleMicrophysical characterization of long-range transported biomass burning particles from North America at three EARLINET stationseng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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