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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemarte3.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YCT/H3FQx
Repositóriosid.inpe.br/iris@1905/2005/08.03.23.43
Última Atualização2018:01.04.13.56.15 (UTC) marciana
Repositório de Metadadossid.inpe.br/iris@1905/2005/08.03.23.43.33
Última Atualização dos Metadados2018:06.06.03.55.16 (UTC) administrator
Chave SecundáriaINPE-9323-PRE/4987
Rótulo10242
Chave de CitaçãoHodnettNWJPHGNT:2002:PrStGe
TítuloProcesses of streamflow generation in a headwater catchment in central Amazonia
Ano2002
Data Secundária20021107
Data de Acesso26 jun. 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho26 KiB
2. Contextualização
Autor1 Hodnett, Martin G.
2 Nobre, A. D.
3 Waterloo, M. J.
4 Jans, W. W.
5 Pineda, Cuartas A.
6 Heijmenberg, J. M.
7 Gomes Neto, W.
8 Nascimento, A.
9 Tomasella, J.
Grupo1 CPT-INPE-MCT-BR
Nome do EventoInternational LBA Scientific Conference, 2.
Localização do EventoManaus, Br
Data7-10 July 2002
Histórico (UTC)2015-05-21 18:37:14 :: administrator -> marciana :: 2002
2018-01-04 13:56:16 :: marciana -> administrator :: 2002
2018-06-06 03:55:16 :: administrator -> marciana :: 2002
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveMETEOROLOGIA
ResumoA 5 km2 headwater catchment in terra firme forest close to the Manaus k34 eddyflux tower has been instrumented to measure the components of the water, carbon and nutrient balances. This paper concentrates on the hydrological aspects: the processes by which streamflow is generated, and the routes taken by the water arriving in the stream. The variables being measured are: rainfall (4 locations), evaporation flux, throughfall, soil moisture storage (to 4.8m)and groundwater level along a toposequence, and streamflow. Data collection began in December 2001. The response of streamflow to rainfall is very rapid, indicating that stormflow peaks are generated from the valley floor areas, where the water table is close to the surface. Peaks in DOC concentrations confirm the valley floor as the source of the stormflow - DOC concentrations in the groundwater beneath the hillslope are very low. The groundwater level response to rainfall at different positions in the toposequence changes as the season progresses because the arrival of recharge from the plateau and slope areas is delayed by the travel time through the deep unsaturated zone. Late in the wet season, the discharge of groundwater from beneath the plateau and slope areas begins to dominate the water table behaviour in the valley floor. The water balance is being calculated on a daily basis to attempt to quantify storage in the deep unsaturated zone and groundwater. Data collection is still at an early stage, but important results are emerging. These are important in understanding the carbon balance.
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
URL dos dadoshttp://urlib.net/ibi/6qtX3pFwXQZ3r59YCT/H3FQx
URL dos dados zipadoshttp://urlib.net/zip/6qtX3pFwXQZ3r59YCT/H3FQx
Arquivo Alvo9323.pdf
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Visibilidadeshown
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Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 2
Acervo Hospedeirosid.inpe.br/banon/2001/04.03.15.36
6. Notas
Campos Vaziosaffiliation archivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress format isbn issn language lineage mark mirrorrepository nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress resumeid rightsholder schedulinginformation secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype volume
7. Controle da descrição
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