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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/3D53L87
Repositóriodpi.inpe.br/plutao/2012/11.28.16.42.41
Última Atualização2013:02.07.16.20.13 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao/2012/11.28.16.42.42
Última Atualização dos Metadados2021:01.03.02.11.05 (UTC) administrator
DOI10.1029/2012JD017723
ISSN0148-0227
2156-2202
Rótulolattes: 7258266163150929 5 YuanRBZAPOGYA:2012:AeInEf
Chave de CitaçãoYuanRBZAPOGYA:2012:AeInEf
TítuloAerosol indirect effect on tropospheric ozone via lightning
Ano2012
Data de Acesso07 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3747 KiB
2. Contextualização
Autor 1 Yuan, Tianle
 2 Remer, Lorraine A.
 3 Bian, Huisheng
 4 Ziemke, Jerald R.
 5 Albrecht, Rachel Ifanger
 6 Pickering, Kenneth E.
 7 Oreopoulos, Lazaros
 8 Goodman, Steven J.
 9 Yu, Hongbin
10 Allen, Dale J.
Grupo 1
 2
 3
 4
 5 DSA-CPT-INPE-MCTI-GOV-BR
Afiliação 1 University of Maryland / Climate and Radiation Laboratory, NASA Goddard Space Flight Center
 2 University of Maryland
 3 University of Maryland / Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center
 4 Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center / Goddard Earth and Sciences Technology and Research, Morgan State University
 5 Instituto Nacional de Pesquisas Espaciais (INPE)
 6 Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center
 7 Climate and Radiation Laboratory, NASA Goddard Space Flight Center
 8 NOAA/NESDIS, NASA Goddard Space Flight Center
 9 Climate and Radiation Laboratory, NASA Goddard Space Flight Center / Earth System Science Interdisciplinary Center, University of Maryland
10 Department of Atmospheric and Oceanic Science, University of Maryland
Endereço de e-Mail do Autor 1 tianle.yuan@nasa.gov
 2
 3
 4
 5 rachel.albrecht@cptec.inpe.br
Endereço de e-Mailrachel.albrecht@cptec.inpe.br
RevistaJournal of Geophysical Research
Volume117
NúmeroD18
PáginasD18213
Nota SecundáriaB1_ASTRONOMIA_/_FÍSICA B2_CIÊNCIA_DA_COMPUTAÇÃO A1_CIÊNCIAS_AGRÁRIAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A2_ENGENHARIAS_II A1_ENGENHARIAS_III A2_ENGENHARIAS_IV A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
Histórico (UTC)2012-11-28 23:06:28 :: lattes -> administrator :: 2012
2013-02-07 16:03:33 :: administrator -> marciana :: 2012
2013-02-07 16:20:13 :: marciana -> administrator :: 2012
2021-01-03 02:11:05 :: administrator -> marciana :: 2012
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chaveaerosol
tropospheric ozone
greenhouse gas
lightning
ResumoTropospheric ozone (O3) is a pollutant and major greenhouse gas and its radiative forcing is still uncertain. Inadequate understanding of processes related to O3 production, in particular those natural ones such as lightning, contributes to this uncertainty. Here we demonstrate a new effect of aerosol particles on O3 production by affecting lightning activity and lightning-generated NOx (LNOx). We find that lightning flash rate increases at a remarkable rate of 30 times or more per unit of aerosol optical depth. We provide observational evidence that indicates the observed increase in lightning activity is caused by the influx of aerosols from a volcano. Satellite data analyses show O3 is increased as a result of aerosol-induced increase in lightning and LNOx, which is supported by modle simulations with prescribed lightning change. O3 production increase from this aerosollightning-ozone link is concentrated in the upper troposphere, where O3 is most efficient as a greenhouse gas. In the face of anthropogenic aerosol increase our findings suggest that lightning activity, LNOx and O3, especially in the upper troposphere, have all increased substantially since preindustrial time due to the proposed aerosol-lightning-ozone link, which implies a stronger O3 historical radiative forcing. Aerosol forcing therefore has a warming component via its effect on O3 production and this component has mostly been ignored in previous studies of climate forcing related to O3 and aerosols. Sensitivity simulations suggest that 48% increase of column tropospheric ozone, mainly in the tropics, is expected if aerosol-lighting-ozone link is parameterized, depending on the background emission scenario. We note, however, substantial uncertainties remain on the exact magnitude of aerosol effect on tropospheric O3 via lightning. The challenges for obtaining a quantitative global estimate of this effect are also discussed. Our results have significant implications for understanding past and projecting future tropospheric O3 forcing as well as wildfire changes and call for integrated investigations of the coupled aerosol-cloud-chemistry system.
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/J8LNKAN8RW/3D53L87
URL dos dados zipadoshttp://urlib.net/zip/J8LNKAN8RW/3D53L87
Idiomaen
Arquivo AlvoYuan_etal2012-JGR.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
DivulgaçãoWEBSCI; AGU; MGA; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
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