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: | 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 |
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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 |
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info:eu-repo/semantics/openAccess |
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https://creativecommons.org/licences/by/4.0/ |
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openAccess |
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https://creativecommons.org/licences/by/4.0/ |
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application/pdf |
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Huancayo Perú |
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Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera |
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Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera |
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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. Finally, the authors assessed, analyzed, and confirmed the influence of biomass burning on AOD in the studied region.Por paresapplication/pdfengUniversidad Nacional Autónoma de México, Centro de Ciencias de la Atmósferaurn:issn:0187-6236info:eu-repo/semantics/openAccesshttps://creativecommons.org/licences/by/4.0/Dispersion phenomenonAerosolsWRF-Chem modelSun photometerBiomass burningLAMARhttp://purl.org/pe-repo/ocde/ford#1.05.00http://purl.org/pe-repo/ocde/ford#1.05.09Influence evaluation of PM₁₀ produced by the burning of biomass in Peru on AOD, using the WRF-Cheminfo:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALNavarro_2020_Atmosfera.pdfNavarro_2020_Atmosfera.pdfapplication/pdf7563132https://repositorio.igp.gob.pe/bitstreams/f57d028f-e95c-4673-aedb-1607138bb83a/downloade6cdab3c9357e8ccef8b9956d8157123MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.igp.gob.pe/bitstreams/74f04d4f-9dff-4d27-8eac-6ace8d183421/download8a4605be74aa9ea9d79846c1fba20a33MD52TEXTNavarro_2020_Atmosfera.pdf.txtNavarro_2020_Atmosfera.pdf.txtExtracted texttext/plain50950https://repositorio.igp.gob.pe/bitstreams/1b319d49-57ab-4640-bc3f-d43830a5e388/downloadfb7264377f66a0251556573eef86600bMD53THUMBNAILNavarro_2020_Atmosfera.pdf.jpgNavarro_2020_Atmosfera.pdf.jpgIM Thumbnailimage/jpeg160621https://repositorio.igp.gob.pe/bitstreams/ce2ff100-1a32-407a-88b3-c33de5324c51/download997093bb6b98cdfc4e9e01db7033aae3MD5420.500.12816/4743oai:repositorio.igp.gob.pe:20.500.12816/47432024-10-01 16:35:58.617https://creativecommons.org/licences/by/4.0/info:eu-repo/semantics/openAccessopen.accesshttps://repositorio.igp.gob.peRepositorio Geofísico Nacionalbiblio@igp.gob.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 |
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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).