1. Identificação | |
Tipo de Referência | Artigo em Evento (Conference Proceedings) |
Site | mtc-m16b.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | x6e6X3pFwXQZ3DUS8rS5/Dor6m |
Repositório | cptec.inpe.br/walmeida/2004/09.06.16.03 |
Última Atualização | 2015:11.18.11.10.09 (UTC) marciana |
Repositório de Metadados | cptec.inpe.br/walmeida/2004/09.06.16.03.32 |
Última Atualização dos Metadados | 2022:03.26.18.02.42 (UTC) administrator |
Chave Secundária | INPE-11977-PRE/7323 |
Chave de Citação | MarengoCSBNSDCCSP:2000:EnSiIn |
Título | Ensemble simulation of interannual climate variability using the CPTEC/COLA Global climate model for the period 1982-1991 |
Formato | Papel |
Ano | 2000 |
Data de Acesso | 04 jun. 2024 |
Tipo Secundário | PRE CI |
Número de Arquivos | 1 |
Tamanho | 16 KiB |
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2. Contextualização | |
Autor | 1 Marengo, Jose Antonio 2 Cavalcanti, Iracema Fonseca de Albuquerque 3 Satyamurty, Prakki 4 Bonatti, Jose Paulo 5 Nobre, Carlos Afonso 6 Sampaio, GilvaN 7 D'Almeyda, C. 8 Camargo Jr., Helio 9 Castro, Christopher Alexander Cunningham 10 Sanches, Marcos Barbosa 11 Pezzi, Luciano Ponzi |
Grupo | 1 DMD-INPE-MCT-BR 2 DMD-INPE-MCT-BR 3 DMD-INPE-MCT-BR 4 DMD-INPE-MCT-BR 5 DMA-INPE-MCT-BR 6 DMA-INPE-MCT-BR 7 DOP-INPE-MCT-BR 8 DOP-INPE-MCT-BR 9 DOP-INPE-MCT-BR 10 DMD-INPE-MCT-BR |
Afiliação | 1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil |
Endereço de e-Mail | fabia@cptec.inpe.br |
Nome do Evento | Intrnational Conference Southern Hemisphere Meteorology and Oceanography, 6. |
Localização do Evento | Santiago-Chile |
Data | 3-7 apr. |
Editora (Publisher) | American Meteorology Society |
Páginas | 51-52 |
Título do Livro | Proceedings |
Organização | ASM |
Histórico (UTC) | 2005-01-14 18:15:28 :: Fabia -> administrator :: 2008-06-10 21:15:04 :: administrator -> estagiario :: 2010-05-11 16:54:41 :: estagiario -> administrator :: 2015-05-27 14:38:57 :: administrator -> marciana :: 2000 2015-11-18 11:10:10 :: marciana -> administrator :: 2000 2022-03-26 18:02:42 :: administrator -> marciana :: 2000 |
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3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Tipo de Versão | publisher |
Resumo | Beginning the 1960's, observational and modeling studies of the ocean and atmosphere began to make clear that certain behaviors of the coupled system might be predictable, including EI Nino (see reviews in Mason et ai. 1999). The seasonal mean tropical circulation may be potentially more predictable than the middle latitude circulation as the low-frequency component of the tropical variability is primarily forced by slowly varying boundary conditions, such as sea surface temperature (SST), as supported by observational and modeling work. The ability of an atmospheric model to simulate to observed climate and its variability varies with scale and variable, with the radiative effects of clouds and the land-surface and sea-air interactions remaining an area of difficulty. Given the correct SST dr ice extent, most atmospheric G,CMs can simulate the observed large- scale climate with better skill for some areas as compared to another, and give a use fui indication of some of the observed regional and global interannual climate variations and trends. Even though the ability of a model to reproduce the observed mean interannual variability of climate is an important aspects of its performance, it comes the fact that the abiljty of the model to reproduce specific time sequences of interannual variability, either at regional or global scales, not always is forced (e.g. by SST), and that a parI of this variability may be intemal of the atmosphere and climate system themselves. Climate simulations using specified SST have an extensive history (se e reviews in Brankovic and Palmer 1998), as well as a host of papers derived from the AMIP climate simulations (see reviews in Zwiers 1996 and Gates et ai. 1992). The possibility that the atmosphere's internal dynamics or slowly evolving surface properties, such as soil moisture or snow cover may also generate potentially predictable interannual variability of seasonal mean climate. |
Área | MET |
Arranjo 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Ensemble simulation of... |
Arranjo 2 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > Ensemble simulation of... |
Arranjo 3 | urlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Ensemble simulation of... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
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4. Condições de acesso e uso | |
URL dos dados | http://urlib.net/ibi/x6e6X3pFwXQZ3DUS8rS5/Dor6m |
URL dos dados zipados | http://urlib.net/zip/x6e6X3pFwXQZ3DUS8rS5/Dor6m |
Idioma | en |
Arquivo Alvo | 2000_marengo.pdf |
Grupo de Usuários | Fabia administrator marciana |
Grupo de Leitores | administrator marciana |
Visibilidade | shown |
Detentor da Cópia | SID/SCD |
Permissão de Leitura | allow from all |
Permissão de Atualização | não transferida |
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5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/43SKC35 8JMKD3MGPCW/43SQKNE 8JMKD3MGPCW/46JKC45 |
Lista de Itens Citando | sid.inpe.br/bibdigital/2022/03.26.17.47 2 |
Acervo Hospedeiro | cptec.inpe.br/walmeida/2003/04.25.17.12 |
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6. Notas | |
Campos Vazios | archivingpolicy archivist callnumber copyright creatorhistory descriptionlevel dissemination doi edition editor electronicmailaddress isbn issn keywords label lineage mark mirrorrepository nextedition notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project publisheraddress resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url volume |
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7. Controle da descrição | |
e-Mail (login) | marciana |
atualizar | |
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