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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/3AFLCL7
Repositóriodpi.inpe.br/plutao/2011/09.22.18.55.53   (acesso restrito)
Última Atualização2012:01.03.17.11.13 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao/2011/09.22.18.55.54
Última Atualização dos Metadados2021:02.10.18.35.08 (UTC) administrator
DOI10.1007/s00382-010-0841-z
ISSN0930-7575
Rótulolattes: 4220736028824952 1 ShimizuAlbu:2011:VaPaRo
Chave de CitaçãoShimizuAlbu:2011:VaPaRo
TítuloVariability patterns of Rossby wave source
Ano2011
MêsAug.
Data de Acesso05 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2274 KiB
2. Contextualização
Autor1 Shimizu, Marilia Harumi
2 Albuquerque Cavalcanti, Iracema Fonseca
Grupo1 CPT-CPT-INPE-MCT-BR
2 CPT-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 marilia.shimizu@cptec.inpe.br
Endereço de e-Mailmarilia.shimizu@cptec.inpe.br
RevistaClimate Dynamics
Volume37
Número3-4
Páginas441-454
Nota SecundáriaA1_CIÊNCIAS_BIOLÓGICAS_I A1_ECOLOGIA_E_MEIO_AMBIENTE A1_ENGENHARIAS_I A1_GEOCIÊNCIAS
Histórico (UTC)2011-09-22 18:55:54 :: lattes -> administrator ::
2011-09-23 08:13:28 :: administrator -> lattes :: 2011
2011-09-23 14:11:20 :: lattes -> secretaria.cpa@dir.inpe.br :: 2011
2011-11-07 10:43:52 :: secretaria.cpa@dir.inpe.br -> administrator :: 2011
2011-11-07 15:49:39 :: administrator -> banon :: 2011
2011-11-23 14:03:05 :: banon -> secretaria.cpa@dir.inpe.br :: 2011
2012-01-03 17:11:34 :: secretaria.cpa@dir.inpe.br -> administrator :: 2011
2021-02-10 18:35:08 :: administrator -> marciana :: 2011
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-ChaveSOUTHERN-HEMISPHERE WINTER
ATLANTIC CONVERGENCE ZONE
EMPIRICAL ORTHOGONAL FUNCTIONS
ATMOSPHERIC CIRCULATION
TELECONNECTION PATTERNS
NORTHERN-HEMISPHERE
TROPICAL CONVECTION
GENERALIZED FROSTS
STORM TRACKS
AMERICA
ResumoRossby waves (RW) propagation due to a local forcing is one of the mechanisms responsible for wave trains configurations known as teleconnections. The term teleconnection refers to anomalies patterns that are correlated in several regions of the world, causing large-scale changes in atmospheric waves patterns and temperature and precipitation regimes. The aim of teleconnections studies is to provide a better understanding of atmospheric variability and their mechanisms of action in order to identify patterns that can be tracked and predicted. The purpose of this study was to characterize seasonal and spatial variability of atmospheric RW sources. The RW source at 200 hPa was calculated for the four seasons with reanalysis data of zonal and meridional wind. In the Northern Hemisphere (NH), the RW sources were located on East Asia, North America, North Atlantic and Pacific. The main RW sources in the Southern Hemisphere (SH) were located over Intertropical, South Pacific, South Atlantic and South Indian Convergence Zones. Extratropical regions were also identified, mainly to the south of Australia. The vortex stretching term (S1) and the advection of absolute vorticity by the divergent wind (S2) were analyzed to discuss the physical mechanisms for RW generation. In the NH, the source at East Asia in DJF changed to a sink in JJA, related to the dominance of S1 term in DJF and S2 term in JJA. In the SH, the vortex stretching term had the dominant contribution for RW source located to the south of Australia. The main forcing for RW sources at east of Australia was the advection of absolute vorticity by divergent flow. Over South America, both terms contributed to the source in DJF. The main modes of RW source variability were discussed by using empirical orthogonal functions analysis. RW variability was characterized by wave trains configurations in both hemispheres over regions of jet streams and storm tracks, associated with favorable and unfavorable areas for RW generation.
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
Idiomaen
Arquivo AlvoShimizu-ClimDyn-v37-n3-4-p441-54fulltext[1].pdf
Grupo de Usuáriosadministrator
banon
lattes
secretaria.cpa@dir.inpe.br
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marciana
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