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Aerosol lidar intercomparison in the framework of the EARLINET project. 1. Instruments

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dc.contributor.author Matthais, V en
dc.contributor.author Freudenthaler, V en
dc.contributor.author Amodeo, A en
dc.contributor.author Balin, I en
dc.contributor.author Balis, D en
dc.contributor.author Bosenberg, J en
dc.contributor.author Chaikovsky, A en
dc.contributor.author Chourdakis, G en
dc.contributor.author Comeron, A en
dc.contributor.author Delaval, A en
dc.contributor.author De Tomasi, F en
dc.contributor.author Eixmann, R en
dc.contributor.author Hagard, A en
dc.contributor.author Komguem, L en
dc.contributor.author Kreipl, S en
dc.contributor.author Matthey, R en
dc.contributor.author Rizi, V en
dc.contributor.author Rodrigues, JA en
dc.contributor.author Wandinger, U en
dc.contributor.author Wang, X en
dc.date.accessioned 2014-03-01T01:19:53Z
dc.date.available 2014-03-01T01:19:53Z
dc.date.issued 2004 en
dc.identifier.issn 0003-6935 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/15740
dc.subject.classification Optics en
dc.subject.other Aerosol extinction coefficient en
dc.subject.other Aerosol lidar system en
dc.subject.other Raman lidar measurements en
dc.subject.other Algorithms en
dc.subject.other Atmospheric aerosols en
dc.subject.other Backscattering en
dc.subject.other Boundary layers en
dc.subject.other Elasticity en
dc.subject.other Numerical analysis en
dc.subject.other Photometers en
dc.subject.other Quality control en
dc.subject.other Raman scattering en
dc.subject.other Ultraviolet radiation en
dc.subject.other Optical radar en
dc.title Aerosol lidar intercomparison in the framework of the EARLINET project. 1. Instruments en
heal.type journalArticle en
heal.identifier.primary 10.1364/AO.43.000961 en
heal.identifier.secondary http://dx.doi.org/10.1364/AO.43.000961 en
heal.language English en
heal.publicationDate 2004 en
heal.abstract In the framework of the European Aerosol Research Lidar Network to Establish an Aerosol Climatology (EARLINET), 19 aerosol lidar systems from 11 European countries were compared. Aerosol extinction or backscatter coefficient profiles were measured by at least two systems for each comparison. Aerosol extinction coefficients were derived from Raman lidar measurements in the UV (351 or 355 nm), and aerosol backscatter profiles were calculated from pure elastic backscatter measurements at 351 or 355, 532, or 1064 nm. The results were compared for height ranges with high and low aerosol content. Some systems were additionally compared with sunphotometers and starphotometers. Predefined maximum deviations were used for quality control of the results. Lidar systems with results outside those limits could not meet the quality assurance criterion. The algorithms for deriving aerosol backscatter profiles from elastic lidar measurements were tested separately, and the results are described in Part 2 of this series of papers [Appl. Opt. 43, 977-989 (2004)]. In the end, all systems were quality assured, although some had to be modified to improve their performance. Typical deviations between aerosol backscatter profiles were 10% in the planetary boundary layer and 0.1 X 10(-6) m(-1) sr(-1) in the free troposphere. (C) 2004 Optical Society of America. en
heal.publisher OPTICAL SOC AMER en
heal.journalName Applied Optics en
dc.identifier.doi 10.1364/AO.43.000961 en
dc.identifier.isi ISI:000188510900033 en
dc.identifier.volume 43 en
dc.identifier.issue 4 en
dc.identifier.spage 961 en
dc.identifier.epage 976 en


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