Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/1399
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dc.contributor.authorTsaknakis, Georgios-
dc.contributor.authorPapayannis, Alexandros D.-
dc.contributor.authorMamouri, Rodanthi-Elisavet-
dc.contributor.authorKokkalis, Panagiotis-
dc.contributor.authorAmiridis, Vassilis-
dc.contributor.authorKambezidis, Harry D.-
dc.contributor.authorGeorgoussis, Georgios-
dc.contributor.authorAvdikos, Georgios K.-
dc.date.accessioned2013-03-08T13:51:47Zen
dc.date.accessioned2013-05-17T05:22:56Z-
dc.date.accessioned2015-12-02T10:12:14Z-
dc.date.available2013-03-08T13:51:47Zen
dc.date.available2013-05-17T05:22:56Z-
dc.date.available2015-12-02T10:12:14Z-
dc.date.issued2011-06-
dc.identifier.citationAtmospheric Measurement Techniques, 2011, vol. 4, no. 6, pp. 1261-1273en_US
dc.identifier.issn18678548-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/1399-
dc.description.abstractThis study presents an inter-comparison of two active remote sensors (lidar and ceilometer) to determine the mixing layer height and structure of the Planetary Boundary Layer (PBL) and to retrieve tropospheric aerosol vertical profiles over Athens, Greece. This inter-comparison was performed under various strongly different aerosol loads/types (urban air pollution, biomass burning and Saharan dust event), implementing two different lidar systems (one portable Raymetrics S.A. lidar system running at 355 nm and one multi-wavelength Raman lidar system running at 355 nm, 532 nm and 1064 nm) and one CL31 Vaisala S.A. ceilometer (running at 910 nm). Spectral conversions of the ceilometer's data were performed using the Ångström exponent estimated by ultraviolet multi-filter radiometer (UV-MFR) measurements. The inter-comparison was based on two parameters: the mixing layer height determined by the presence of the suspended aerosols and the attenuated backscatter coefficient. Additionally, radiosonde data were used to derive the PBL height. In general, a good agreement was found between the ceilometer and the lidar techniques in both inter-compared parameters in the height range from 500 m to 5000 m, while the limitations of each instrument are also examined.en_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofAtmospheric Measurement Techniquesen_US
dc.rights© Author(s) CC Attribution 3.0 Licenseen_US
dc.subjectCloud Height Indicatoren_US
dc.subjectTroposphereen_US
dc.subjectConvective Boundary Layeren_US
dc.titleInter-comparison of lidar and ceilometer retrievals for aerosol and planetary boundary layer profiling over Athens, Greeceen_US
dc.typeArticleen_US
dc.affiliationNational Technical University Of Athensen
dc.collaborationNational Technical University Of Athensen_US
dc.collaborationNational Observatory of Athensen_US
dc.collaborationRaymetrics S.Aen_US
dc.subject.categoryComputer and Information Sciencesen_US
dc.subject.categoryENGINEERING AND TECHNOLOGYen_US
dc.journalsOpen Accessen_US
dc.countryGreeceen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.5194/amt-4-1261-2011en_US
dc.dept.handle123456789/54en
dc.relation.issue6en_US
dc.relation.volume4en_US
cut.common.academicyear2010-2011en_US
dc.identifier.spage1261en_US
dc.identifier.epage1273en_US
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.openairetypearticle-
item.languageiso639-1en-
crisitem.journal.journalissn1867-8548-
crisitem.journal.publisherCopernicus-
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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