Study of the planetary boundary layer height in an urban environment using a combination of microwave radiometer and ceilometer

dc.contributor.authorMOREIRA, GREGORI de A.pt_BR
dc.contributor.authorGUERRERO-RASCADO, JUAN L.pt_BR
dc.contributor.authorBRAVO-ARANDA, JUAN A.pt_BR
dc.contributor.authorFOYO-MORENO, INMACULADApt_BR
dc.contributor.authorCAZORLA, ALBERTOpt_BR
dc.contributor.authorALADOS, INMACULADApt_BR
dc.contributor.authorLYAMANI, HASSANpt_BR
dc.contributor.authorLANDULFO, EDUARDOpt_BR
dc.contributor.authorALADOS-ARBOLEDAS, LUCASpt_BR
dc.coverageInternacionalpt_BR
dc.date.accessioned2020-07-22T17:50:54Z
dc.date.available2020-07-22T17:50:54Z
dc.date.issued2020pt_BR
dc.description.abstractThe Planetary Boundary Layer (PBL) is an important part of the atmosphere that is relevant in different atmospheric fields like pollutant dispersion, and weather forecasting. In this study, we analyze four and five-year datasets of measurements gathered with a ceilometer and a microwave radiometer to study the PBL structure respectively, in the mid-latitude urban area of Granada (Spain). The methodologies applied for the PBL Height (PBLH) detection (gradient method for ceilometer and the combination of parcel method and temperature gradient method for microwave radiometer) provided a description in agreement with the literature about the PBL structure under simple scenarios. Then, the PBLH behavior is characterized by a statistical study of the convective and stable situations, so that the PBLH was obtained from microwave radiometer measurements. The analysis of the PBLH statistical study shows some agreement with other PBLH studies such as daily pattern and yearly cycle, and the discrepancies were explained in terms of distinct latitudes, topography and climate conditions. Finally, it was performed a joint long-term analysis of the residual layer (RL) provided by ceilometer and the stable and convective layer heights determined by microwave radiometer, offering a complete picture of the PBL evolution by synergetic combination of remote sensing techniques. The PBL behavior has been used for explaining the daily cycle of Black Carbon (BC) concentration, used as tracer of the pollutants emissions associated to traffic.pt_BR
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)pt_BR
dc.description.sponsorshipIDCNPq: 154320/2018-8pt_BR
dc.format.extent1-15pt_BR
dc.identifier.citationMOREIRA, GREGORI de A.; GUERRERO-RASCADO, JUAN L.; BRAVO-ARANDA, JUAN A.; FOYO-MORENO, INMACULADA; CAZORLA, ALBERTO; ALADOS, INMACULADA; LYAMANI, HASSAN; LANDULFO, EDUARDO; ALADOS-ARBOLEDAS, LUCAS. Study of the planetary boundary layer height in an urban environment using a combination of microwave radiometer and ceilometer. <b>Atmospheric Research</b>, v. 240, p. 1-15, 2020. DOI: <a href="https://dx.doi.org/10.1016/j.atmosres.2020.104932">10.1016/j.atmosres.2020.104932</a>. Disponível em: http://repositorio.ipen.br/handle/123456789/31349.
dc.identifier.doi10.1016/j.atmosres.2020.104932pt_BR
dc.identifier.issn0169-8095pt_BR
dc.identifier.orcid0000-0002-9691-5306pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-9691-5306
dc.identifier.percentilfi83.51pt_BR
dc.identifier.percentilfiCiteScore93.00
dc.identifier.urihttp://repositorio.ipen.br/handle/123456789/31349
dc.identifier.vol240pt_BR
dc.relation.ispartofAtmospheric Researchpt_BR
dc.rightsopenAccesspt_BR
dc.subjectboundary layers
dc.subjecturban areas
dc.subjectatmospheres
dc.subjectclouds
dc.subjectmicrowave radiation
dc.subjectradiometers
dc.subjectweather
dc.subjectcloud cover
dc.subjectremote sensing
dc.subjectclimates
dc.subjectmonitoring
dc.titleStudy of the planetary boundary layer height in an urban environment using a combination of microwave radiometer and ceilometerpt_BR
dc.typeArtigo de periódicopt_BR
dspace.entity.typePublication
ipen.autorEDUARDO LANDULFO
ipen.autorGREGORI DE ARRUDA MOREIRA
ipen.codigoautor503
ipen.codigoautor10204
ipen.contributor.ipenauthorEDUARDO LANDULFO
ipen.contributor.ipenauthorGREGORI DE ARRUDA MOREIRA
ipen.date.recebimento20-07
ipen.identifier.fi5.369pt_BR
ipen.identifier.fiCiteScore8.6
ipen.identifier.ipendoc27123pt_BR
ipen.identifier.iwosWoSpt_BR
ipen.range.fi4.500 - 5.999
ipen.range.percentilfi75.00 - 100.00
ipen.type.genreArtigo
relation.isAuthorOfPublicatione4dff370-e8c1-4437-846a-ef18a3ad606b
relation.isAuthorOfPublication539c9881-45aa-4cc9-aefe-a503026f1567
relation.isAuthorOfPublication.latestForDiscovery539c9881-45aa-4cc9-aefe-a503026f1567
sigepi.autor.atividadeLANDULFO, EDUARDO:503:920:Npt_BR
sigepi.autor.atividadeMOREIRA, GREGORI de A.:10204:920:Spt_BR

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