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, Héctor, Moya Álvarez, Aldo Saturnino, Luna, Ana, Fashé-Raymundo, Octavio
Formato: artículo
Fecha de Publicación:2020
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/4743
Enlace del recurso:http://hdl.handle.net/20.500.12816/4743
https://doi.org/10.20937/ATM.52711
Nivel de acceso:acceso abierto
Materia:Dispersion phenomenon
Aerosols
WRF-Chem model
Sun photometer
Biomass burning
LAMAR
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.09
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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, Héctor
Dispersion phenomenon
Aerosols
WRF-Chem model
Sun photometer
Biomass burning
LAMAR
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.09
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, Héctor
author_facet Navarro Barboza, Héctor
Moya Álvarez, Aldo Saturnino
Luna, Ana
Fashé-Raymundo, Octavio
author_role author
author2 Moya Álvarez, Aldo Saturnino
Luna, Ana
Fashé-Raymundo, Octavio
author2_role author
author
author
dc.contributor.author.fl_str_mv Navarro Barboza, Héctor
Moya Álvarez, Aldo Saturnino
Luna, Ana
Fashé-Raymundo, Octavio
dc.subject.none.fl_str_mv Dispersion phenomenon
Aerosols
WRF-Chem model
Sun photometer
Biomass burning
LAMAR
topic Dispersion phenomenon
Aerosols
WRF-Chem model
Sun photometer
Biomass burning
LAMAR
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.09
dc.subject.ocde.none.fl_str_mv http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.09
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.
publishDate 2020
dc.date.accessioned.none.fl_str_mv 2020-01-29T16:56:07Z
dc.date.available.none.fl_str_mv 2020-01-29T16:56:07Z
dc.date.issued.fl_str_mv 2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.none.fl_str_mv Navarro-Barboza, H., Moya-Álvarez, A., Luna, A., & Fashé-Raymundo, O. (2020). Influence evaluation of PM 10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem.==$Atmósfera, 33$==(1), 71-86. https://doi.org/10.20937/ATM.52711
dc.identifier.govdoc.none.fl_str_mv index-oti2018
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/20.500.12816/4743
dc.identifier.journal.none.fl_str_mv Atmósfera
dc.identifier.doi.none.fl_str_mv https://doi.org/10.20937/ATM.52711
identifier_str_mv Navarro-Barboza, H., Moya-Álvarez, A., Luna, A., & Fashé-Raymundo, O. (2020). Influence evaluation of PM 10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem.==$Atmósfera, 33$==(1), 71-86. https://doi.org/10.20937/ATM.52711
index-oti2018
Atmósfera
url http://hdl.handle.net/20.500.12816/4743
https://doi.org/10.20937/ATM.52711
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:0187-6236
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.uri.none.fl_str_mv https://creativecommons.org/licences/by/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licences/by/4.0/
dc.format.none.fl_str_mv application/pdf
dc.coverage.spatial.none.fl_str_mv Huancayo
Perú
dc.publisher.none.fl_str_mv Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera
publisher.none.fl_str_mv Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera
dc.source.none.fl_str_mv reponame:IGP-Institucional
instname:Instituto Geofísico del Perú
instacron:IGP
instname_str Instituto Geofísico del Perú
instacron_str IGP
institution IGP
reponame_str IGP-Institucional
collection IGP-Institucional
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spelling Navarro Barboza, HéctorMoya Álvarez, Aldo SaturninoLuna, AnaFashé-Raymundo, OctavioHuancayoPerú2020-01-29T16:56:07Z2020-01-29T16:56:07Z2020Navarro-Barboza, H., Moya-Álvarez, A., Luna, A., & Fashé-Raymundo, O. (2020). Influence evaluation of PM 10 produced by the burning of biomass in Peru on AOD, using the WRF-Chem.==$Atmósfera, 33$==(1), 71-86. https://doi.org/10.20937/ATM.52711index-oti2018http://hdl.handle.net/20.500.12816/4743Atmósferahttps://doi.org/10.20937/ATM.52711This 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. 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