Brazilian coastal region modeling with WRF/SMOKE/CMAQ and atmospheric parameter measurement validation with radio probing, Sodar and Lidar

dc.contributor.authorLORIATO, AYRES G.pt_BR
dc.contributor.authorSALVADOR, NADIRpt_BR
dc.contributor.authorLORIATO, AYRAN A.B.pt_BR
dc.contributor.authorNASCIMENTO, ERIC G.S.pt_BR
dc.contributor.authorMOREIRA, DAVIDSON M.pt_BR
dc.contributor.authorREIS JUNIOR, NEYVAL C.pt_BR
dc.contributor.authorSOKOLOV, ANTONpt_BR
dc.contributor.authorLANDULFO, EDUARDOpt_BR
dc.contributor.authorALBUQUERQUE, TACIANA T. de A.pt_BR
dc.coverageInternacionalpt_BR
dc.date.accessioned2021-02-23T15:55:36Z
dc.date.available2021-02-23T15:55:36Z
dc.date.issued2020pt_BR
dc.description.abstractThis article aims to evaluate and compare data of vertical potential temperature profile, wind velocity and PM10 concentration measured during an experimental campaign on July 2012 by means of radio probing, Sonic Detection And Ranging (SODAR) and Light Detection And Ranging (LIDAR) with those modeled by means of numerical simulation with Weather Research And Forecast Model (WRF), Sparse Matrix Operator Kernel Emissions (SMOKE) and Community Multi-Scale Air Quality (CMAQ). The study has been conducted at Região da Grande Vitória (RGV), a Brazilian coastal region. All data measurements have been done at Universidade Federal do Espírito Santo (UFES), in the city of Vitória, Espírito Santo, Brazil. For numerical simulation, RGV's emissions inventory has been used to model a 61x79km2 grid with spatial resolution of 1 km2 and temporal resolution of 1 hour. Sea breeze is a relevant weather phenomenon along coastal regions, and it has been perceived by both SODAR measurement and WRFmodeling. During the experimental campaign, the most intense sea breeze occurred on July 28, 2012 and, therefore, a thorough analysis of atmospheric and pollution parameters has been done for that day. This analysis showed neutral atmosphere up to 200 meters of altitude and stability beyond that, which has been confirmed by WRFmodeling. Regarding wind data, the comparison between SODAR measurement and WRFmodeling showed similarities regarding wind direction, but wind speed was overestimated by WRF. Lastly, LIDAR measurement and CMAQmodeling showed close values for PM10 pollutant concentration.pt_BR
dc.format.extent1-15pt_BR
dc.identifier.citationLORIATO, AYRES G.; SALVADOR, NADIR; LORIATO, AYRAN A.B.; NASCIMENTO, ERIC G.S.; MOREIRA, DAVIDSON M.; REIS JUNIOR, NEYVAL C.; SOKOLOV, ANTON; LANDULFO, EDUARDO; ALBUQUERQUE, TACIANA T. de A. Brazilian coastal region modeling with WRF/SMOKE/CMAQ and atmospheric parameter measurement validation with radio probing, Sodar and Lidar. <b>International Journal of Research in Engineering and Science</b>, v. 8, n. 12, p. 1-15, 2020. Disponível em: http://repositorio.ipen.br/handle/123456789/31795.
dc.identifier.fasciculo12pt_BR
dc.identifier.issn2320-9356pt_BR
dc.identifier.orcid0000-0002-9691-5306pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-9691-5306
dc.identifier.percentilfiSem Percentilpt_BR
dc.identifier.percentilfiCiteScoreSem Percentil CiteScore
dc.identifier.urihttp://repositorio.ipen.br/handle/123456789/31795
dc.identifier.vol8pt_BR
dc.relation.ispartofInternational Journal of Research in Engineering and Sciencept_BR
dc.rightsopenAccesspt_BR
dc.subjectcoastal regions
dc.subjectair pollution
dc.subjectoptical radar
dc.subjectatmospheres
dc.subjectmeteorology
dc.subjectair quality
dc.titleBrazilian coastal region modeling with WRF/SMOKE/CMAQ and atmospheric parameter measurement validation with radio probing, Sodar and Lidarpt_BR
dc.typeArtigo de periódicopt_BR
dspace.entity.typePublication
ipen.autorEDUARDO LANDULFO
ipen.codigoautor503
ipen.contributor.ipenauthorEDUARDO LANDULFO
ipen.date.recebimento21-02
ipen.identifier.fiSem F.I.pt_BR
ipen.identifier.fiCiteScoreSem CiteScore
ipen.identifier.ipendoc27568pt_BR
ipen.type.genreArtigo
relation.isAuthorOfPublicatione4dff370-e8c1-4437-846a-ef18a3ad606b
relation.isAuthorOfPublication.latestForDiscoverye4dff370-e8c1-4437-846a-ef18a3ad606b
sigepi.autor.atividadeLANDULFO, EDUARDO:503:920:Npt_BR

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