First two and a half years of aerosol measurements with an AERONET sunphotometer at the Huancayo Observatory, Peru

Descripción del Articulo

Direct sun measurements with a CIMEL sunphotometer belonging to the AERONET network have been performed in the Huancayo Observatory, Peru, from March 2015 to August 2017, two and a half years, providing for the first time information about aerosols in the specific area. The prevalence of background...

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Detalles Bibliográficos
Autores: Estevan, René, Martínez Castro, Daniel, Suárez Salas, Luis, Moya Álvarez, Aldo Saturnino, Silva Vidal, Yamina
Formato: artículo
Fecha de Publicación:2019
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/4637
Enlace del recurso:http://hdl.handle.net/20.500.12816/4637
https://doi.org/10.1016/j.aeaoa.2019.100037
Nivel de acceso:acceso abierto
Materia:AOD
AERONET
Huancayo observatory
Optical properties
Single scattering albedo
Asymmetry factor
LAMAR
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.09
Descripción
Sumario:Direct sun measurements with a CIMEL sunphotometer belonging to the AERONET network have been performed in the Huancayo Observatory, Peru, from March 2015 to August 2017, two and a half years, providing for the first time information about aerosols in the specific area. The prevalence of background conditions in the measurement site has been determined for the period of study. These conditions, which constitute more than 80% of cases, are occasionally altered, mainly by high aerosols loading, as a consequence of biomass-burning events. Biomass-burning periods cover every year from mid-July to mid-October. The identification of these periods has been possible through the classification of aerosols in 6 subtypes. The month with the maximum AOD monthly average is September, and in 2016, the absolute maximum value of 0.91 was registered. The mean AOD value for the study period is 0.10 ± 0.07 and the alpha mean value is 1.49 ± 0.36, indicating presence, of small size aerosols. Some aerosol optical properties were analyzed in order to validate the aerosol classification. The aerosol size distribution revealed a bimodal character with a slight predominance of the fine mode, related to the two main types of aerosols: continental and biomass.
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