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Πεδίο DCΤιμήΓλώσσα
dc.contributor.authorPapayannis, Alexandros D.-
dc.contributor.authorZhang, Huaiqing-
dc.contributor.authorAmiridis, Vassilis-
dc.contributor.authorJu, Hongbo-
dc.contributor.authorChourdakis, Giorgos-
dc.contributor.authorGeorgoussis, Georgios-
dc.contributor.authorPérez García-Pando, Carlos-
dc.contributor.authorChen, Hongbin-
dc.contributor.authorGoloub, Philippe-
dc.contributor.authorMamouri, Rodanthi-Elisavet-
dc.contributor.authorKazadzis, Stelios-
dc.contributor.authorParonis, Dimitrios-
dc.contributor.authorTsaknakis, Georgios-
dc.contributor.authorBaldasano, Jose M.-
dc.date.accessioned2019-07-03T06:49:24Z-
dc.date.available2019-07-03T06:49:24Z-
dc.date.issued2007-04-16-
dc.identifier.citationGeophysical Research Letters, 2007, vol. 34, no. 7en_US
dc.identifier.issn00948276-
dc.description.abstractAn extraordinary dust event over Beijing (April 2006) was followed by a synergy of lidar, Sun photometric and satellite measurements. Extreme aerosol optical depth (AOD) values (1-4) were measured by AERONET and MODIS over Beijing. The size distribution of the particles remained close to 2.5 μm and the single scattering albedo was around 0.92 ± 0.5 (440 nm). Coarse particles contributed to more than 60-80% to the AOD values, indicating the presence of very large particles (Ångström exponent <0.3). Coarse particle contribution to total AOD is associated with the free-tropospheric aerosols calculated by lidar profiles (65%). Lidar vertical profiles with AOD values from AERONET were used to estimate a typical lidar ratio for the dust particles (84 sr) during the most intense dust period. The DREAM forecast model was applied for the accurate description of the dust event evolution. Ground-truth data were used for the validation of DREAM over the Beijing area. Copyright 2007 by the American Geophysical Union.en_US
dc.language.isoenen_US
dc.relation.ispartofGeophysical Research Lettersen_US
dc.rights© Wileyen_US
dc.subjectAerosolen_US
dc.subjectDusten_US
dc.subjectDust aerosolsen_US
dc.titleExtraordinary dust event over Beijing, China, during April 2006: Lidar, Sun photometric, satellite observations and model validationen_US
dc.typeArticleen_US
dc.collaborationCyprus University of Technologyen_US
dc.collaborationNational Technical University Of Athensen_US
dc.collaborationChinese Academy of Forestryen_US
dc.collaborationNational Observatory of Athensen_US
dc.collaborationRaymetrics S.Aen_US
dc.collaborationBarcelona Supercomputing Centeren_US
dc.collaborationChinese Academy of Sciencesen_US
dc.collaborationUniversité des Sciences et Technologies de Lilleen_US
dc.collaborationAristotle University of Thessalonikien_US
dc.collaborationUniversitat Politècnica de Catalunyaen_US
dc.subject.categoryCivil Engineeringen_US
dc.journalsSubscriptionen_US
dc.countryCyprusen_US
dc.countryGreeceen_US
dc.countryChinaen_US
dc.countrySpainen_US
dc.countryFranceen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1029/2006GL029125en_US
dc.identifier.scopus2-s2.0-34250782734-
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/34250782734-
dc.relation.issue7en_US
dc.relation.volume34en_US
cut.common.academicyear2006-2007en_US
item.openairetypearticle-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0003-4836-8560-
crisitem.author.parentorgFaculty of Engineering and Technology-
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