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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZGivnJUY/MTaLC
Repositóriosid.inpe.br/mtc-m15@80/2006/10.26.17.50
Última Atualização2007:04.25.13.31.39 (UTC) marciana
Repositório de Metadadossid.inpe.br/mtc-m15@80/2006/10.26.17.50.30
Última Atualização dos Metadados2022:03.26.18.00.47 (UTC) administrator
Chave SecundáriaINPE-14261-PRE/9349
ISSN1680-7316
Chave de CitaçãoMarecalDuLoFrRiPi:2007:TwCaSt
TítuloMesoscale modelling of water vapour in the tropical UTLS: two case studies from the HIBISCUS campaign
Ano2007
Data Secundária20070319
MêsMar.
Data de Acesso05 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1863 KiB
2. Contextualização
Autor1 Marecal, V.
2 Durry, G.
3 Longo, Karla Maria
4 Freitas, Saulo Ribeiro de
5 Riviere, E. D.
6 Pirre, M.
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JHKQ
4 8JMKD3MGP5W/3C9JJ7M
Grupo1 DMA-INPE-MCT-BR
2 DMD-INPE-MCT-BR
3
4 DMD-INPE-MCT-BR
Afiliação1 Laboratoire de Physique et Chimie de l'Environnement/CNRS/Université d'Orléans
2 Instituto Nacional de Pesquisas Espaciais (INPE), Centro de Previsão de Tempo e Estudos Climáticos (CPTEC)
3 Instituto Nacional de Pesquisas Espaciais (INPE), Centro de Previsão de Tempo e Estudos Climáticos (CPTEC)
Endereço de e-Mailatus@cptec.inpe.br
RevistaAtmospheric Chemistry and Physics
Volume7
Número5
Páginas1471-1489
Histórico (UTC)2006-10-26 17:50:30 :: estagiario -> administrator ::
2006-11-17 23:07:27 :: administrator -> estagiario ::
2007-04-25 13:31:40 :: estagiario -> administrator ::
2008-06-10 20:44:48 :: administrator -> estagiario ::
2010-05-11 16:56:37 :: estagiario -> marciana ::
2010-07-08 12:44:48 :: marciana -> administrator ::
2012-11-22 12:12:28 :: administrator -> marciana :: 2007
2013-02-04 10:31:13 :: marciana -> administrator :: 2007
2013-02-04 10:51:20 :: administrator -> marciana :: 2007
2013-02-04 10:51:31 :: marciana -> administrator :: 2007
2013-02-04 12:16:48 :: administrator -> marciana :: 2007
2013-02-04 12:18:55 :: marciana -> administrator :: 2007
2022-03-26 18:00:47 :: administrator -> marciana :: 2007
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoIn this study, we evaluate the ability of the BRAMS (Brazilian Regional Atmospheric Modeling System) mesoscale model compared to ECMWF global analysis to simulate the observed vertical variations of water vapour in the tropical upper troposphere and lower stratosphere (UTLS). The observations are balloon-borne measurements of water vapour mixing ratio and temperature from micro-SDLA (Tunable Diode Laser Spectrometer) instrument. Data from two balloon flights performed during the 2004 HIBISCUS field campaign are used to compare with the mesoscale simulations and to the ECMWF analysis. The observations exhibit fine scale vertical structures of water vapour of a few hundred meters height. The ECMWF vertical resolution (similar to 1 km) is too coarse to capture these vertical structures in the UTLS. With a vertical resolution similar to ECMWF, the mesoscale model performs better than ECMWF analysis for water vapour in the upper troposphere and similarly or slightly worse for temperature. The BRAMS model with 250 m vertical resolution is able to capture more of the observed fine scale vertical variations of water vapour compared to runs with a coarser vertical resolution. This is mainly related to: (i) the enhanced vertical resolution in the UTLS and (ii) to the more detailed microphysical parameterization providing ice supersaturations as in the observations. In near saturated or supersaturated layers, the mesoscale model predicted relative humidity with respect to ice saturation is close to observations provided that the temperature profile is realistic. For temperature, the ECMWF analysis gives good results partly attributed to data assimilation. The analysis of the mesoscale model results showed that the vertical variations of the water vapour profile depends on the dynamics in unsaturated layer while the microphysical processes play a major role in saturated/supersaturated layers. In the lower stratosphere, the ECMWF model and the BRAMS model give very similar water vapour profiles that are significantly drier than micro-SDLA measurements. This similarity comes from the fact that BRAMS is initialised using ECMWF analysis and that no mesoscale process acts in the stratosphere leading to no modification of the BRAMS results with respect to ECMWF analysis.
ÁreaMET
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Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/6qtX3pFwXQZGivnJUY/MTaLC
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/6qtX3pFwXQZGivnJUY/MTaLC
Idiomaen
Arquivo Alvomarecal_2007.pdf
Grupo de Usuáriosadministrator
estagiario
marciana
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Leituraallow from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Edição Anteriorsid.inpe.br/ePrint@80/2006/08.08.19.28
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
8JMKD3MGPCW/46JKC45
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.59.52 1
DivulgaçãoWEBSCI; PORTALCAPES; AGU.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi electronicmailaddress format isbn keywords label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previouslowerunit progress project readergroup rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marciana
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