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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/36KNNB5
Repositóriodpi.inpe.br/plutao@80/2009/12.22.15.05
Última Atualização2010:08.31.17.01.32 (UTC) marciana
Repositório de Metadadosdpi.inpe.br/plutao@80/2009/12.22.15.05.03
Última Atualização dos Metadados2021:01.02.03.52.54 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.5194/acp-10-4977-2010
ISSN1680-7316
Rótulolattes: 9873289111461387 6 MarecalPiRiPoCrFrLo:2009:MoReUp
Chave de CitaçãoMarecalPiRiPoCrFrLo:2010:MoReUp
TítuloModelling the reversible uptake of chemical species in the gas phase by ice particles formed in a convective cloud
Ano2010
Data de Acesso29 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1560 KiB
2. Contextualização
Autor1 Marecal, V
2 Pirre, M
3 Riviere, E D
4 Pouvesle, N.
5 Crowley, J. N.
6 Freitas, Saulo Ribeiro de
7 Longo, K. M.
Identificador de Curriculo1
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3
4
5
6
7
8
9
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11 8JMKD3MGP5W/3C9JJ7M
Grupo1
2
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6 DMD-CPT-INPE-MCT-BR
7 DGE-CEA-INPE-MCT-BR
Afiliação1 1Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS-Universit´e d’Orl´eans, UMR6115, Orl´eans, France
2 1Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS-Universit´e d’Orl´eans, UMR6115, Orl´eans, France
3 Groupe de Spectrom´etrie Mol´eculaire et Atmosph´erique, Universit´e de Reims-CNRS, Reims, France
4 Max-Planck-Institut f¨ur Chemie, Division of Atmospheric Chemistry, Mainz, Germany
5 Max-Planck-Institut f¨ur Chemie, Division of Atmospheric Chemistry, Mainz, Germany
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3
4
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6 saulo.freitas@cptec.inpe.br
Endereço de e-Mailsaulo.freitas@cptec.inpe.br
RevistaAtmospheric Chemistry and Physics
Volume10
Número10
Páginas4977–5000
Nota SecundáriaB4_ENGENHARIAS_II B3_GEOCIÊNCIAS B2_INTERDISCIPLINAR
Histórico (UTC)2009-12-23 14:00:48 :: lattes -> marciana ::
2010-01-06 11:54:49 :: marciana -> administrator ::
2010-01-26 15:36:58 :: administrator -> banon ::
2010-05-11 16:35:19 :: banon -> administrator ::
2010-05-12 02:06:45 :: administrator -> marciana ::
2010-08-31 17:01:32 :: marciana -> administrator :: 2009 -> 2010
2010-12-08 15:19:42 :: administrator -> marciana :: 2010
2011-02-24 19:07:04 :: marciana -> administrator :: 2010
2011-02-27 00:14:49 :: administrator -> marciana :: 2010
2011-05-20 05:50:06 :: marciana -> administrator :: 2010
2012-07-25 15:58:10 :: administrator -> marciana :: 2010
2013-02-04 12:15:35 :: marciana -> administrator :: 2010
2021-01-02 03:52:54 :: administrator -> marciana :: 2010
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 present paper is a preliminary study preparing the introduction of reversible trace gas uptake by ice particles into a 3-D cloud resolving model. For this a 3-D simulation of a tropical deep convection cloud was run with the BRAMS cloud resolving model using a two-moment bulk microphysical parameterization. Trajectories within the convective clouds were computed from these simulation outputs along which the variations of the pristine ice, snow and aggregate mixing ratios and concentrations were extracted. The reversible uptake of 11 trace gases by ice was examined assuming applicability of Langmuir isotherms using recently evaluated (IUPAC) laboratory data. The results show that ice uptake is only significant for HNO3, HCl, CH3COOH and HCOOH. For H2O2, using new results for the partition coefficient results in significant partitioning to the ice phase for this trace gas also. It was also shown that the uptake is largely dependent on the temperature for some species. The adsorption saturation at the ice surface for large gas mixing ratios is generally not a limiting factor except for HNO3 and HCl for gas mixing ratio greater than 1 ppbv. For HNO3, results were also obtained using a trapping theory, resulting in a similar order of magnitude of uptake, although the two approaches are based on different assumptions. The results were compared to those obtained using a BRAMS cloud simulation based on a single-moment microphysical scheme instead of the two moment scheme. We found similar results with a slightly more important uptake when using the singlemoment scheme which is related to slightly higher ice mixing ratios in this simulation. The way to introduce these results in the 3-D cloud model is discussed.
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/J8LNKAN8RW/36KNNB5
URL dos dados zipadoshttp://urlib.net/zip/J8LNKAN8RW/36KNNB5
Idiomaen
Arquivo AlvoFreitas_Modelling.pdf
Grupo de Usuáriosadministrator
banon
lattes
marciana
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.59.52 1
sid.inpe.br/bibdigital/2013/10.01.22.11 1
URL (dados não confiáveis)http://www.atmos-chem-phys-discuss.net/9/24361/2009/acpd-9-24361-2009.html
DivulgaçãoWEBSCI; PORTALCAPES; AGU.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn keywords lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork
7. Controle da descrição
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