| 1. Identificação | |
| Tipo de Referência | Artigo em Revista Científica (Journal Article) |
| Site | plutao.sid.inpe.br |
| Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identificador | J8LNKAN8RW/37NR2NF |
| Repositório | dpi.inpe.br/plutao@80/2010/06.25.16.11.46 (acesso restrito) |
| Última Atualização | 2010:08.12.13.52.00 (UTC) administrator |
| Repositório de Metadados | dpi.inpe.br/plutao@80/2010/06.25.16.11.47 |
| Última Atualização dos Metadados | 2021:01.02.03.52.56 (UTC) administrator |
| Chave Secundária | INPE--PRE/ |
| DOI | 10.1007/s00703-009-0050-7 |
| ISSN | 0177-7971 |
| Rótulo | lattes: 4336175279058172 2 GomesChan:2010:DePaMo |
| Chave de Citação | GomesChan:2010:DePaMo |
| Título | Dependence of partitioning of model implicit and explicit precipitation on horizontal resolution  |
| Ano | 2010 |
| Mês | Feb. |
| Data de Acesso | 02 maio 2024 |
| Tipo Secundário | PRE PI |
| Número de Arquivos | 1 |
| Tamanho | 2283 KiB |
| 2. Contextualização | |
| Autor | 1 Gomes, Jorge Luís 2 Chan, Chou Sin |
| Identificador de Curriculo | 1 2 8JMKD3MGP5W/3C9JGRQ |
| Grupo | 1 DMD-CPT-INPE-MCT-BR 2 DMD-CPT-INPE-MCT-BR |
| Afiliação | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) |
| Endereço de e-Mail do Autor | 1 chou@pesquisador.cnpq.br |
| Endereço de e-Mail | chou@pesquisador.cnpq.br |
| Revista | Meteorology and Atmospheric Physics |
| Volume | 106 |
| Número | 1-2 |
| Páginas | 1-18 |
| Nota Secundária | B1_GEOCIÊNCIAS B1_INTERDISCIPLINAR |
| Histórico (UTC) | 2010-06-29 12:04:21 :: lattes -> marciana :: 2010 2010-07-02 13:02:35 :: marciana -> administrator :: 2010 2010-07-12 17:13:28 :: administrator -> marciana :: 2010 2010-08-12 13:52:00 :: marciana -> administrator :: 2010 2021-01-02 03:52:56 :: administrator -> marciana :: 2010 |
| 3. Conteúdo e estrutura | |
| É a matriz ou uma cópia? | é a matriz |
| Estágio do Conteúdo | concluido |
| Transferível | 1 |
| Tipo do Conteúdo | External Contribution |
| Palavras-Chave | Parametrizacao de Convecao Cumulus Modelo Eta Microfisica de nuvens |
| Resumo | Model precipitation can be produced implicitly through convective parameterization schemes or explicitly through cloud microphysics schemes. These two precipitation production schemes control the spatial and temporal distribution of precipitation and consequently can yield distinct vertical profiles of heating and moistening in the atmosphere. The partition between implicit and explicit precipitation can be different as the model changes resolutions. Within the range of mesoscale resolutions (about 20 km) and cumulus scale, hybrid solutions are suggested, in which cumulus convection parameterization is acting together with the explicit form of representation. In this work, it is proposed that, as resolution increases, the convective scheme should convert less condensed water into precipitation. Part of the condensed water is made available to the cloud microphysics scheme and another part evaporates. At grid sizes smaller than 3 km, the convective scheme is still active in removing convective instability, but precipitation is produced by cloud microphysics. The Eta model version using KF cumulus parameterization was applied in this study. To evaluate the quantitative precipitation forecast, the Eta model with the KF scheme was used to simulate precipitation associated with the South Atlantic Convergence Zone (SACZ) and Cold Front (CF) events. Integrations with increasing horizontal resolutions were carried out for up to 5 days for the SACZ cases and up to 2 days for the CF cases. The precipitation partition showed that most of precipitation was generated by the implicit scheme. As the grid size decreased, the implicit precipitation increased and the explicit decreased. However, as model horizontal resolution increases, it is expected that precipitation be represented more explicitly. In the KF scheme, the fraction of liquid water or ice, generated by the scheme, which is converted into rain or snow is controlled by a parameter S 1. An additional parameter was introduced into KF scheme and the parameter acts to evaporate a fraction of liquid water or ice left in the model grid by S 1 and return moisture to the resolved scale. An F parameter was introduced to combine the effects of S 1 and S 2 parameters. The F parameter gives a measure of the conversion of cloud liquid water or ice to convective precipitation. A function dependent on the horizontal resolution was introduced into the KF scheme to influence the implicit and explicit precipitation partition. The explicit precipitation increased with model resolution. This function reduced the positive precipitation bias at all thresholds and for the studied weather systems. With increased horizontal resolution, the maximum precipitation area was better positioned and the total precipitation became closer to observations. Skill scores for all events at different forecast ranges showed precipitation forecast improvement with the inclusion of the function F. |
| Área | MET |
| Arranjo | Dependence of partitioning... |
| Conteúdo da Pasta doc | acessar |
| Conteúdo da Pasta source | não têm arquivos |
| Conteúdo da Pasta agreement | não têm arquivos |
| 4. Condições de acesso e uso | |
| Idioma | en |
| Arquivo Alvo | gomes.pdf |
| Grupo de Usuários | administrator lattes marciana |
| Visibilidade | shown |
| Política de Arquivamento | denypublisher denyfinaldraft12 |
| Permissão de Leitura | deny from all and allow from 150.163 |
| 5. Fontes relacionadas | |
| Unidades Imediatamente Superiores | 8JMKD3MGPCW/43SKC35 |
| Divulgação | WEBSCI; PORTALCAPES; COMPENDEX. |
| Acervo Hospedeiro | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
| 6. Notas | |
| Notas | Setores de Atividade: Pesquisa e desenvolvimento científico. |
| Campos Vazios | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage format isbn lineage mark mirrorrepository nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype |
| 7. Controle da descrição | |
| e-Mail (login) | marciana |
| atualizar | |