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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/walmeida/2004/12.22.16.17
Última Atualização2004:12.22.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/12.22.16.17.28
Última Atualização dos Metadados2021:02.10.19.04.46 (UTC) administrator
Chave SecundáriaINPE-11874-PRE/7221
Chave de CitaçãoSouzaAmbrKaya:2004:RaAtMe
TítuloThe Autumn Rainy Regime over the Eastern Amazon/Northeast Brazil: Rainfall-Producing Atmospheric Mechanisms on Intraseasonal and Submonthly Timescales
FormatoOn-line
Ano2004
Data de Acesso08 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho1215 KiB
2. Contextualização
Autor1 Souza, Everaldo B. de
2 Ambrizzi, Tercio
3 Kayano, Mary Toshie
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JHST
Grupo1 DMD-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailatus@cptec.inpe.br
Nome do EventoInternational Clivar Science Conference, 1.
Localização do EventoBaltimore
Data21-25 jun.
Tipo TerciárioPosters
Histórico (UTC)2005-01-12 18:35:54 :: fabia -> administrator ::
2008-06-10 21:24:11 :: administrator -> estagiario ::
2010-05-11 16:55:38 :: estagiario -> administrator ::
2021-02-10 19:04:46 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoThe regional precipitation variability within the autumn rainy regime (March to May) over the eastern Amazon (EAM) and northeast Brazil (NEB) is diagnosed by using raingauge-based weekly data from 1982 to 2001. This rainy regime is remarkably modulated by the combined effect of the Pacific and Atlantic SST anomalies. Thus, two extreme and contrasting large-scale climatic scenarios are considered in this study: the unfavorable - UNFAV (favorable - FAV) scenario defined by the simultaneous manifestations of the El Niño (La Niña) in the Pacific and northward (southward) SST gradient in the intertropical Atlantic. UNFAV (FAV) composites for unfiltered data showed remarkable changes in both the Walker and the Hadley cells associated with the Atlantic ITCZ anomalously weakened (enhanced) which in consequence yields deficient (abundant) autumn rainy regime in most of the EAM/NEB. In the context of these scenarios, we have objectively identified the pluviometric variability using empirical orthogonal functions (EOF) analyses performed on the (30-70 day) intraseasonal and (£21 day) submonthly filtered weekly precipitation anomalies for 18 autumn seasons (1983 to 2000). Only the leading EOF mode for these timescales is presented. Strong pluviometric oscillations for both scales during UNFAV and FAV years revealed that, even under extreme climatic conditions prevailing simultaneously in the tropical Pacific and Atlantic, events with anomalously deficient and abundant precipitation over the EAM/NEB occur alternately. Composites based on events with anomalously increased precipitation (selected from principal component series) on intraseasonal and submonthly scales were analyzed separately for the UNFAV and FAV years. It is attempted to isolate and identify the main rainfall-producing atmospheric mechanisms for these scales and regions. These analyses corroborate that during both scenarios UNFAV and FAV the more important rainfall-producing atmospheric mechanism over the EAM/NEB on intraseasonal scale consists in the establishment of deep convective bands organized during sporadic passages of the frontal systems over the northeast Brazil. Such a regional pattern is embedded in large-scale dynamical environment related to the propagation of the MJO convection-active phase over the tropical South America. On the other hand, the main rainfall-producing atmospheric mechanism over the same regions on submonthly scale is the Atlantic ITCZ during FAV years. However,during UNFAV years were observed that the equatorial Atlantic ITCZ activity may be forced by meridionally elongated midlatitude wave trains at upper troposphere.
ÁreaMET
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Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/cptec.inpe.br/walmeida/2004/12.22.16.17
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/walmeida/2004/12.22.16.17
Idiomaen
Arquivo AlvoSouza_Autumn.pdf
Grupo de Usuáriosadministrator
fabia
Visibilidadeshown
Detentor da CópiaSID/SCD
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.56.22 1
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosarchivingpolicy archivist booktitle callnumber copyright creatorhistory descriptionlevel dissemination documentstage doi edition editor electronicmailaddress identifier isbn issn keywords label lineage mark mirrorrepository nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url versiontype volume
7. Controle da descrição
e-Mail (login)marciana
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