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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3RPNMT5
Repositóriosid.inpe.br/mtc-m21c/2018/09.06.15.50
Última Atualização2018:09.06.15.50.03 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2018/09.06.15.50.03
Última Atualização dos Metadados2021:01.03.02.11.20 (UTC) administrator
DOI10.5194/acp-18-10773-2018
ISSN1680-7316
1680-7324
Chave de CitaçãoShillingPFASHLMMSTW:2018:AiObCh
TítuloAircraft observations of the chemical composition and aging of aerosol in the Manaus urban plume during GoAmazon 2014/5
Ano2018
MêsJuly
Data de Acesso29 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho13795 KiB
2. Contextualização
Autor 1 Shilling, John E.
 2 Pekour, Mikhail S.
 3 Fortner, Edward C.
 4 Artaxo, Paulo
 5 Sá, Suzane de
 6 Hubbe, John M.
 7 Longo, Karla Maria
 8 Machado, Luiz Augusto Toledo
 9 Martin, Scot T.
10 Springston, Stephen R.
11 Tomlinson, Jason
12 Wang, Jian
Identificador de Curriculo 1
 2
 3
 4
 5
 6
 7 8JMKD3MGP5W/3C9JHKQ
 8 8JMKD3MGP5W/3C9JHMS
Grupo 1
 2
 3
 4
 5
 6
 7
 8 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação 1 Pacific Northwest National Laboratory
 2 Pacific Northwest National Laboratory
 3 Center for Aerosol and Cloud Chemistry, Aerodyne Research
 4 Universidade de São Paulo (USP)
 5 Harvard University
 6 Pacific Northwest National Laboratory
 7 University Space Research Association
 8 Instituto Nacional de Pesquisas Espaciais (INPE)
 9 Harvard University
10 Brookhaven National Laboratory
11 Pacific Northwest National Laboratory
12 Brookhaven National Laboratory
Endereço de e-Mail do Autor 1
 2
 3
 4
 5
 6
 7
 8 luiz.machado@inpe.br
RevistaAtmospheric Chemistry and Physics
Volume18
Número14
Páginas10773-10797
Nota SecundáriaA1_MEDICINA_II A1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_MATEMÁTICA_/_PROBABILIDADE_E_ESTATÍSTICA A2_ENGENHARIAS_II A2_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2018-09-06 15:50:03 :: simone -> administrator ::
2018-09-06 15:50:04 :: administrator -> simone :: 2018
2018-09-06 15:51:59 :: simone -> administrator :: 2018
2019-01-04 16:57:10 :: administrator -> simone :: 2018
2019-01-07 14:26:05 :: simone -> administrator :: 2018
2021-01-03 02:11:20 :: administrator -> simone :: 2018
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoThe Green Ocean Amazon (GoAmazon 2014/5) campaign, conducted from January 2014 to December 2015 in the vicinity of Manaus, Brazil, was designed to study the aerosol life cycle and aerosol-cloud interactions in both pristine and anthropogenically influenced conditions. As part of this campaign, the U.S. Department of Energy (DOE) Gulfstream 1 (G-1) research aircraft was deployed from 17 February to 25 March 2014 (wet season) and 6 September to 5 October 2014 (dry season) to investigate aerosol and cloud properties aloft. Here, we present results from the G-1 deployments focusing on measurements of the aerosol chemical composition and secondary organic aerosol (SOA) formation and aging. In the first portion of the paper, we provide an overview of the data and compare and contrast the data from the wet and dry season. Organic aerosol (OA) dominates the deploymentaveraged chemical composition, comprising 80%of the nonrefractory PM1 aerosol mass, with sulfate comprising 14 %, nitrate 2 %, and ammonium 4 %. This product distribution was unchanged between seasons, despite the fact that total aerosol loading was significantly higher in the dry season and that regional and local biomass burning was a significant source of OA mass in the dry, but not wet, season. However, the OA was more oxidized in the dry season, with the median of the mean carbon oxidation state increasing from -0:45 in the wet season to -0:02 in the dry season. In the second portion of the paper, we discuss the evolution of the Manaus plume, focusing on 13 March 2014, one of the exemplary days in the wet season. On this flight, we observe a clear increase in OA concentrations in the Manaus plume relative to the background. As the plume is transported downwind and ages, we observe dynamic changes in the OA. The mean carbon oxidation state of the OA increases from -0:6 to -0:45 during the 4-5 h of photochemical aging. Hydrocarbon-like organic aerosol (HOA) mass is lost, with ΔHOA/ΔCO values decreasing from 17.6 μgm-3 ppmv-1 over Manaus to 10.6 μgm-3 ppmv-1 95 km downwind. Loss of HOA is balanced out by formation of oxygenated organic aerosol (OOA), with ΔOOA/ΔCO increasing from 9.2 to 23.1 μgm-3 ppmv-1. Because hydrocarbon-like organic aerosol (HOA) loss is balanced by OOA formation, we observe little change in the net Δorg/ΔCO values; Δorg/ΔCO averages 31 μgm-3 ppmv-1 and does not increase with aging. Analysis of the Manaus plume evolution using data from two additional flights in the wet season showed similar trends in Δorg/ΔCO to the 13 March flight; Δorg/ΔCO values averaged 34 μgm-3 ppmv-1 and showed little change over 4-6.5 h of aging. Our observation of constant Δorg/ΔCO are in contrast to literature studies of the outflow of several North American cities, which report significant increases in Δorg/ΔCO for the first day of plume aging. These observations suggest that SOA formation in the Manaus plume occurs, at least in part, by a different mechanism than observed in urban outflow plumes in most other literature studies. Constant Δorg/ΔCO with plume aging has been observed in many biomass burning plumes, but we are unaware of reports of fresh urban emissions aging in this manner. These observations show that urban pollution emitted from Manaus in the wet season forms less particulate downwind as it ages than urban pollution emitted from North American cities.
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 3
DivulgaçãoWEBSCI; PORTALCAPES; AGU; SCOPUS.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
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