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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/adm_conf/2005/10.30.19.43
Última Atualização2006:04.16.17.25.28 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.30.19.43.16
Última Atualização dos Metadados2018:06.05.03.42.51 (UTC) administrator
Chave de CitaçãoSouzaRoch:2006:DiVaRa
TítuloOn the diurnal variability of rainfall in eastern amazonia along atlantic coast during rainy season
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso17 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho565 KiB
2. Contextualização
Autor1 Souza, Everaldo B. De
2 Rocha, Edson J. P. Da
Afiliação1 Divisão de Meteorologia, SIPAM/ATECH, Manaus-AM, Brasil
2 Departamento de Meteorologia, UFPa, Belém-PA, Brasil
Endereço de e-Mail do Autor1 everaldobsouza@yahoo.com.br
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailesouza@atech.br
Nome do EventoInternational Conference on Southern Hemisphere Meteorology and Oceanography, 8 (ICSHMO).
Localização do EventoFoz do Iguaçu
Data24-28 Apr. 2006
Editora (Publisher)American Meteorological Society (AMS)
Cidade da Editora45 Beacon Hill Road, Boston, MA, USA
Páginas1203-1207
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-30 19:43:16 :: esouza@atech.br -> adm_conf ::
2005-12-15 16:48:38 :: adm_conf -> esouza@atech.br ::
2006-03-29 23:38:48 :: esouza@atech.br -> administrator ::
2006-04-18 21:03:57 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:31 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:56:49 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:53 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:52:37 :: administrator -> banon :: 2006
2011-01-02 17:14:53 :: banon -> administrator :: 2006
2018-06-05 03:42:51 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-Chaveeastern Amazonia
diurnal cycle
precipitation
ITCZ
ResumoThe knowledge of variation of precipitation over short timescales, such as the diurnal cycle, is essential in understanding of the physics of tropical atmosphere. The diurnal variability of rainfall in particular over the Amazonia has been previously documented using high temporal resolution data collected in field experiments, like ABRACOS (Anglo Brazilian Climate Observation Study) and LBA (Large-scale Biosphere-Atmosphere Experiment in Amazonia). Previous works that used these data evidenced rainfall maxima in southwest and central Amazonia (Ji-Paraná and Manaus) in late afternoon, while in eastern Amazonia (Marabá) there is a maximum in the morning. On the other hand, there have been few investigations on the diurnal variability of rainfall in particular over eastern Amazonia along Atlantic coast. In the present work, five years (2001-2005) of continuous rainfall data collected by MilênioLBA (Large-scale Biosphere-Atmosphere Experiment in Amazonia) station in Bragança (00º 50' S, 46º 38' W) are used in order to describe coherent diurnal variation of rainfall in eastern Amazonia off Atlantic coast during rainy season (January to May). The 5-yr average of accumulation of rainfall in each 6 h (06:00, 12:00, 18:00 and 24:00 LST) evidenced a maximum peak during morning and a sharp minimum in the afternoon. A significant diurnal cycle related to Intertropical Convergence Zone activity in the equatorial Atlantic is pointed out as the main mechanism regulator of diurnal pluviometric variability in coastal region along Pará and Amapá states. March presents highest frequency of rainy days following by April and February. Furthermore, the frequency distribution of rainfall considering different intensity ranges (0.1 to 5, 5.1 to 10, 10.1 to 25, 25.1 to 50, 50.1 to 75, 75.1 to 100 and > 100 mm) is documented for each month and period of diurnal cycle. An outstanding result evidenced is frequency distribution of events with rainfall less than 5 mm, which explain the largest proportional contribution of the rainfall total observed during rainy season that reach 21.6% in January, 24.5% in May, 29.8% in February, 33.2% in April and 36% in March.
ÁreaMET
TipoMonsoon systems and continental rainfall
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
SouzaRocha.doc 29/03/2006 20:38 404.0 KiB 
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/cptec.inpe.br/adm_conf/2005/10.30.19.43
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/adm_conf/2005/10.30.19.43
Idiomaen
Arquivo Alvo1203-1208.pdf
Grupo de Usuáriosesouza@atech.br
administrator
Visibilidadeshown
5. Fontes relacionadas
Acervo Hospedeirocptec.inpe.br/nobre/2005/06.02.21.14
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Nota1
Campos Vaziosarchivingpolicy archivist callnumber contenttype copyholder copyright creatorhistory descriptionlevel dissemination documentstage doi edition group identifier isbn issn label lineage mirrorrepository nextedition nexthigherunit notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey secondarymark serieseditor session shorttitle sponsor subject tertiarymark url versiontype volume


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