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Lidar aerosol profile categorisation in são paulo, brazil

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dc.contributor.author Landulfo, E en
dc.contributor.author Papayannis, A en
dc.contributor.author De Sousa, RF en
dc.contributor.author De Freitas, AZ en
dc.date.accessioned 2014-03-01T02:49:48Z
dc.date.available 2014-03-01T02:49:48Z
dc.date.issued 2004 en
dc.identifier.issn 03796566 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/34748
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-3142511169&partnerID=40&md5=d596ef3e6ef71f7ed974d602612e0014 en
dc.subject.other Aerosols en
dc.subject.other Atmospheric optics en
dc.subject.other Backscattering en
dc.subject.other Boundary layers en
dc.subject.other Clouds en
dc.subject.other Condensation en
dc.subject.other Meteorology en
dc.subject.other Petrochemical plants en
dc.subject.other Steel en
dc.subject.other Troposphere en
dc.subject.other Aerosol optical thickness (AOT) en
dc.subject.other Backscatter coefficients en
dc.subject.other Brazil en
dc.subject.other Meteorological conditions en
dc.subject.other Optical radar en
dc.title Lidar aerosol profile categorisation in são paulo, brazil en
heal.type conferenceItem en
heal.publicationDate 2004 en
heal.abstract A backscattering LIDAR system, the first of this kind in Brazil, has been set-up in a suburban area in the city of São Paulo (23°33' S, 46°44' W) to provide the vertical profile of the aerosol backscatter coefficient at 532 nm up to an altitude of 4-6 km above sea level (asl). The measurements have been carried out during the second half of the so-called Brazilian dry season, September and October 2001 and during the first half of the dry season in August and September 2002. The LIDAR data are presented and analysed in synergy with aerosol optical thickness (AOT) measurements in the visible region (532 nm) obtained by a CIMEL sun-tracking photometer (belonging to the AERONET network) for purposes of validation of the data. The LIDAR data were also used to retrieve the Planetary Boundary Layer (PBL) height, aerosol layering and the structure of the lower troposphere over the city of São Paulo, and allowed us to categorise the profiles according to three distinctive patterns followed by the meteorological conditions of each type of categorisation. Here we show these categorisations, how we defined them and their distribution over the period of measurements. en
heal.journalName European Space Agency, (Special Publication) ESA SP en
dc.identifier.volume 1 en
dc.identifier.issue 561 en
dc.identifier.spage 499 en
dc.identifier.epage 502 en


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