Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem

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This study assesses the influence of PM10 on the optical thickness of aerosols in the central Andes of Peru, in addition to analyzing and establishing their circulation patterns from July to October 2017. This particular period is considered herein because the largest biomass burning events are usua...

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Detalles Bibliográficos
Autores: Navarro-Barboza H., Moya-Álvarez A., Luna A., Fashé-Raymundo O.
Formato: artículo
Fecha de Publicación:2020
Institución:Consejo Nacional de Ciencia Tecnología e Innovación
Repositorio:CONCYTEC-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.concytec.gob.pe:20.500.12390/2603
Enlace del recurso:https://hdl.handle.net/20.500.12390/2603
https://doi.org/10.20937/ATM.52711
Nivel de acceso:acceso abierto
Materia:WRF-Chem model
Aerosols
Biomass burning
Dispersion phenomenon
Sun photometer
http://purl.org/pe-repo/ocde/ford#2.04.01
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dc.title.none.fl_str_mv Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
title Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
spellingShingle Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
Navarro-Barboza H.
WRF-Chem model
Aerosols
Biomass burning
Dispersion phenomenon
Sun photometer
http://purl.org/pe-repo/ocde/ford#2.04.01
title_short Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
title_full Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
title_fullStr Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
title_full_unstemmed Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
title_sort Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
author Navarro-Barboza H.
author_facet Navarro-Barboza H.
Moya-Álvarez A.
Luna A.
Fashé-Raymundo O.
author_role author
author2 Moya-Álvarez A.
Luna A.
Fashé-Raymundo O.
author2_role author
author
author
dc.contributor.author.fl_str_mv Navarro-Barboza H.
Moya-Álvarez A.
Luna A.
Fashé-Raymundo O.
dc.subject.none.fl_str_mv WRF-Chem model
topic WRF-Chem model
Aerosols
Biomass burning
Dispersion phenomenon
Sun photometer
http://purl.org/pe-repo/ocde/ford#2.04.01
dc.subject.es_PE.fl_str_mv Aerosols
Biomass burning
Dispersion phenomenon
Sun photometer
dc.subject.ocde.none.fl_str_mv http://purl.org/pe-repo/ocde/ford#2.04.01
description This study assesses the influence of PM10 on the optical thickness of aerosols in the central Andes of Peru, in addition to analyzing and establishing their circulation patterns from July to October 2017. This particular period is considered herein because the largest biomass burning events are usually recorded during these months. The regional meteorological-chemistry transport model WRF-Chem (version 3.7) was used with the Fire Inventory from NCAR (FINN) fire emissions dataset and aerosol optical depth (AOD) data from the Aerosol Robotic Network monitoring network (AERONET), which has a CIMEL sun photometer located at the Huancayo Observatory, the most important city in the central highlands of Peru. The simulation used a single domain with a grid size of 18 km and 32 vertical levels. Results showed an increase in PM10 concentrations with an increase in the number of fire outbreaks and AOD during July, August, and September. In contrast, a slight decrease in PM10 concentrations was recorded for October. Further, the meteorological conditions did not favor the occurrence of fire outbreaks in the Mantaro valley during the entire study period; however, an increase in rainfall reduced aerosol concentrations in October. In addition, although the vertical movements prevailing over the central Andes were ascending, they were descending along the Peruvian coast, thus favoring and hindering the dispersion of aerosols in the first and second cases, respectively. Finally, the authors assessed, analyzed, and confirmed the influence of biomass burning on AOD in the studied region. © 2020 Universidad Nacional Autonoma de Mexico.
publishDate 2020
dc.date.accessioned.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.available.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.issued.fl_str_mv 2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12390/2603
dc.identifier.doi.none.fl_str_mv https://doi.org/10.20937/ATM.52711
dc.identifier.scopus.none.fl_str_mv 2-s2.0-85079015361
url https://hdl.handle.net/20.500.12390/2603
https://doi.org/10.20937/ATM.52711
identifier_str_mv 2-s2.0-85079015361
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv Atmosfera
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.uri.none.fl_str_mv https://creativecommons.org/licenses/by-nc/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc/4.0/
dc.publisher.none.fl_str_mv Universidad Nacional Autonoma de Mexico
publisher.none.fl_str_mv Universidad Nacional Autonoma de Mexico
dc.source.none.fl_str_mv reponame:CONCYTEC-Institucional
instname:Consejo Nacional de Ciencia Tecnología e Innovación
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instname_str Consejo Nacional de Ciencia Tecnología e Innovación
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spelling Publicationrp06692600rp06695600rp06694600rp06693600Navarro-Barboza H.Moya-Álvarez A.Luna A.Fashé-Raymundo O.2024-05-30T23:13:38Z2024-05-30T23:13:38Z2020https://hdl.handle.net/20.500.12390/2603https://doi.org/10.20937/ATM.527112-s2.0-85079015361This study assesses the influence of PM10 on the optical thickness of aerosols in the central Andes of Peru, in addition to analyzing and establishing their circulation patterns from July to October 2017. This particular period is considered herein because the largest biomass burning events are usually recorded during these months. The regional meteorological-chemistry transport model WRF-Chem (version 3.7) was used with the Fire Inventory from NCAR (FINN) fire emissions dataset and aerosol optical depth (AOD) data from the Aerosol Robotic Network monitoring network (AERONET), which has a CIMEL sun photometer located at the Huancayo Observatory, the most important city in the central highlands of Peru. The simulation used a single domain with a grid size of 18 km and 32 vertical levels. Results showed an increase in PM10 concentrations with an increase in the number of fire outbreaks and AOD during July, August, and September. In contrast, a slight decrease in PM10 concentrations was recorded for October. Further, the meteorological conditions did not favor the occurrence of fire outbreaks in the Mantaro valley during the entire study period; however, an increase in rainfall reduced aerosol concentrations in October. In addition, although the vertical movements prevailing over the central Andes were ascending, they were descending along the Peruvian coast, thus favoring and hindering the dispersion of aerosols in the first and second cases, respectively. Finally, the authors assessed, analyzed, and confirmed the influence of biomass burning on AOD in the studied region. © 2020 Universidad Nacional Autonoma de Mexico.Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - ConcytecengUniversidad Nacional Autonoma de MexicoAtmosferainfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc/4.0/WRF-Chem modelAerosols-1Biomass burning-1Dispersion phenomenon-1Sun photometer-1http://purl.org/pe-repo/ocde/ford#2.04.01-1Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Cheminfo:eu-repo/semantics/articlereponame:CONCYTEC-Institucionalinstname:Consejo Nacional de Ciencia Tecnología e Innovacióninstacron:CONCYTEC#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#ORIGINALInfluence evaluation of PM10 produced by the burning of biomass.pdfInfluence evaluation of PM10 produced by the burning of biomass.pdfapplication/pdf7563132https://repositorio.concytec.gob.pe/bitstreams/a9faefc8-1c0d-4bd6-a8b8-234f604fcf34/downloade6cdab3c9357e8ccef8b9956d8157123MD51TEXTInfluence evaluation of PM10 produced by the burning of biomass.pdf.txtInfluence evaluation of PM10 produced by the burning of biomass.pdf.txtExtracted texttext/plain50608https://repositorio.concytec.gob.pe/bitstreams/8f6bbab2-c2f2-4874-a5d4-eb5db037199b/downloadbdaeafb69bea79d8445ba48f230ac4d0MD52THUMBNAILInfluence evaluation of PM10 produced by the burning of biomass.pdf.jpgInfluence evaluation of PM10 produced by the burning of biomass.pdf.jpgGenerated Thumbnailimage/jpeg5325https://repositorio.concytec.gob.pe/bitstreams/c8494fa8-d540-4f52-98fb-0c14da40fac6/download15a5120d20cc6a37e1c867382eb9722cMD5320.500.12390/2603oai:repositorio.concytec.gob.pe:20.500.12390/26032025-01-16 22:00:37.039https://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessopen accesshttps://repositorio.concytec.gob.peRepositorio Institucional CONCYTECrepositorio@concytec.gob.pe#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#<Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="7ddaaaea-326d-4124-b82d-b013e73cdb5a"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>eng</Language> <Title>Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem</Title> <PublishedIn> <Publication> <Title>Atmosfera</Title> </Publication> </PublishedIn> <PublicationDate>2020</PublicationDate> <DOI>https://doi.org/10.20937/ATM.52711</DOI> <SCP-Number>2-s2.0-85079015361</SCP-Number> <Authors> <Author> <DisplayName>Navarro-Barboza H.</DisplayName> <Person id="rp06692" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Moya-Álvarez A.</DisplayName> <Person id="rp06695" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Luna A.</DisplayName> <Person id="rp06694" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Fashé-Raymundo O.</DisplayName> <Person id="rp06693" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Universidad Nacional Autonoma de Mexico</DisplayName> <OrgUnit /> </Publisher> </Publishers> <License>https://creativecommons.org/licenses/by-nc/4.0/</License> <Keyword>WRF-Chem model</Keyword> <Keyword>Aerosols</Keyword> <Keyword>Biomass burning</Keyword> <Keyword>Dispersion phenomenon</Keyword> <Keyword>Sun photometer</Keyword> <Abstract>This study assesses the influence of PM10 on the optical thickness of aerosols in the central Andes of Peru, in addition to analyzing and establishing their circulation patterns from July to October 2017. This particular period is considered herein because the largest biomass burning events are usually recorded during these months. The regional meteorological-chemistry transport model WRF-Chem (version 3.7) was used with the Fire Inventory from NCAR (FINN) fire emissions dataset and aerosol optical depth (AOD) data from the Aerosol Robotic Network monitoring network (AERONET), which has a CIMEL sun photometer located at the Huancayo Observatory, the most important city in the central highlands of Peru. The simulation used a single domain with a grid size of 18 km and 32 vertical levels. Results showed an increase in PM10 concentrations with an increase in the number of fire outbreaks and AOD during July, August, and September. In contrast, a slight decrease in PM10 concentrations was recorded for October. Further, the meteorological conditions did not favor the occurrence of fire outbreaks in the Mantaro valley during the entire study period; however, an increase in rainfall reduced aerosol concentrations in October. In addition, although the vertical movements prevailing over the central Andes were ascending, they were descending along the Peruvian coast, thus favoring and hindering the dispersion of aerosols in the first and second cases, respectively. Finally, the authors assessed, analyzed, and confirmed the influence of biomass burning on AOD in the studied region. © 2020 Universidad Nacional Autonoma de Mexico.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication> -1
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