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1. Identificação
Tipo de ReferênciaVídeo em Evento (Audiovisual Material)
Sitemtc-m16d.sid.inpe.br
Identificador8JMKD3MGPDW34R/43NJ2LP
Repositóriosid.inpe.br/mtc-m16d/2020/12.07.19.29
Última Atualização2020:12.07.19.29.10 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m16d/2020/12.07.19.29.10
Última Atualização dos Metadados2022:03.16.02.24.51 (UTC) administrator
Chave de CitaçãoSousaMareMacaZou:2020:NoWeTi
TítuloNon-linear weather time series explain why the drougth period length 2011 at coast north NEB and semi-arid region NEB are different?
Título CurtoSlides
FormatoOn-line.
Ano2020
Data de Acesso30 jun. 2024
Tipo SecundárioPRE CN
Número de Arquivos1
Tamanho8137 KiB
2. Contextualização
Autor1 Sousa, Natanael Vieira de
2 Marengo, José Antônio
3 Macau, Elbert Einstein Nehrer
4 Zou, Yong
Nome do EventoEncontro dos Alunos de Pós-Graduação em Meteorologia do CPTEC/INPE, 19 (EPGMET)
Localização do EventoOn-line
Data16-19 nov. 2020
Editora (Publisher)Instituto Nacional de Pesquisas Espaciais (INPE)
Cidade da EditoraSão José dos Campos
Título do LivroVídeos
Histórico (UTC)2020-12-07 19:29:10 :: simone -> administrator ::
2020-12-23 19:32:53 :: administrator :: -> 2020
2022-03-16 02:24:51 :: administrator -> simone :: 2020
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveComplexnet
Drougth period length
Northeast Brazil
Rainy season
Teleconnections
ResumoThe NEB region has rainy season depending on teleconnections such as NINO/NINA, Madden-Julian Oscillation and others weather systems (e.g. ITCZ). These weather factors are forced by sea temperature surface, sea level pressure, long wave radiation, relativity humidity and others variables. The goal of this work is development of time series analysis techniques with spatial distribution based on the complex networks formalism with applications for understanding episodes of droughts period length (DPL) in Coast North-Northeast Brazil (NEB) and semi-arid region NEB at 2011. Data: The study period is since 01/01/2011 until 12/31/2011. Time series rainfall daily was obtained by GPCP data base 0.5 degree resolution nat average área as box 2S-9S, 45W-30W. To SST [0.25 d.r.] and SLP [2.5 d.r.]. were applied at average NINO 3.4 region 5N-5S, 120-170W. Tropical North Atlantic SST averaged over the domain 6-22N and 80-15W, to South Atlantic SST average 25S-2N and 35W-10E. Relativity Humidity [2.5 d.r.] area between 40-20W, 15S- 1S. Long Wave Radiation anomaly Hovmoller diagram [1 d.r.] 5N-5S , 20E-120W, in 20-70 days. Methods: First to SPL and after other variables: get the differrentiated series deltaSPL = SPL (t+1) - SPL (t); SPL will be in phase increase is deltaSPL is positive, in contrast SPL will be in phase decrease if deltaSPL is negative, i.e., increase (or decrease) trends in sea level pressure averaged over a one-month M window time. To quantify the changes in spatial difference will use r(m,d), r(d) season metric (ave: Feb., Mar., Apr., May.), were used too r(m,s) to drougth period. As conclusions of this research, the authors wait to get the triggers to DPL based in metorological explications about teleconnections and ITCZ (cause and effect) at rainy season in study regions: Coast NNEB and a central point at semi-arid region (Quixeramobim-CE, 5.29S and 39.40S ).
ÁreaMET
TipoEstudos e Modelagem do Tempo e Clima
Arranjo 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Vídeos > Slides
Arranjo 2urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > XIX EPGMET > Vídeos > Slides
Arranjo 3urlib.net > BDMCI > Fonds > EPGMET > XIX EPGMET > Vídeos > Slides
Arranjo 4urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Non-linear weather time... > Slides
Arranjo 5urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Non-linear weather time... > Slides
Arranjo 6urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Resumos/Pôsteres > Non-linear weather time... > Slides
Arranjo 7urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > XIX EPGMET > Resumos/Pôsteres > Non-linear weather time... > Slides
Arranjo 8urlib.net > BDMCI > Fonds > EPGMET > XIX EPGMET > Resumos/Pôsteres > Non-linear weather time... > Slides
Conteúdo da Pasta docacessar
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGPDW34R/43NJ2LP
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGPDW34R/43NJ2LP
Idiomapt
Arquivo Alvosousa_nonlinear.mp4
Grupo de Usuáriossimone
Visibilidadeshown
Licença de Direitos Autoraisurlib.net/www/2012/11.12.15.19
Detentor dos Direitosoriginalauthor yes
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2010/07.16.16.07
Unidades Imediatamente Superiores8JMKD3MGPDW34R/43QS2JB
8JMKD3MGPDW34R/43MDAUB
Lista de Itens Citandosid.inpe.br/mtc-m16d/2020/12.21.22.27 8
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
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7. Controle da descrição
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