Influence evaluation of PM10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem
Descripción del Articulo
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...
Autores: | , , , |
---|---|
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 instacron:CONCYTEC |
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Consejo Nacional de Ciencia Tecnología e Innovación |
instacron_str |
CONCYTEC |
institution |
CONCYTEC |
reponame_str |
CONCYTEC-Institucional |
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CONCYTEC-Institucional |
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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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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).