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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorycptec.inpe.br/walmeida/2004/08.04.11.14
Last Update2007:08.24.12.45.12 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/08.04.11.14.45
Metadata Last Update2022:03.26.18.02.25 (UTC) administrator
Secondary KeyINPE-14836-PRE/9750
Citation KeyHodnettToCuNoWaOlMú:2004:PrStGe
TitleProcesses of streamflow generation in a headwater catchment in central Amazonia
FormatCD-ROM
ProjectLBA
Year2004
Access Date2024, May 16
Secondary TypePRE CN
Number of Files1
Size2612 KiB
2. Context
Author1 Hodnett, Martin George
2 Tomasella, Javier
3 Cuartas, Luz Adriana
4 Nobre, Antonio Donato
5 Waterloo, Maarten
6 Oliveira, Sylvia Mota de
7 Múnera, J.
Resume Identifier1
2 8JMKD3MGP5W/3C9JHE3
Group1 DMA-INPE-MCT-BR
2 DMA-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cachoeira -12630-000-SP-Brasil
e-Mail Addressfabia@cptec.inpe.br
Conference NameConferencia Cientifica do LBA, 3.
Conference LocationBrasilia
Date27-29 jul.
Book TitleAnais
Tertiary TypePosters
OrganizationLBA
History (UTC)2006-11-17 21:45:55 :: administrator -> estagiario ::
2007-11-09 11:41:27 :: estagiario -> administrator ::
2008-06-10 21:19:55 :: administrator -> estagiario ::
2010-05-11 16:54:11 :: estagiario -> administrator ::
2022-03-26 18:02:25 :: administrator -> marciana :: 2004
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractIn 2002 and 2003, runoff from the Asu catchment (6.37 km2) was 1455 mm and 832 mm, of which 45% and 31% was stormflow respectively. Earlier studies in the Barro Branco catchment (1.3 km2) in Reserva Ducke (with similar geology and soils) showed that stormflow was 9% of total runoff in 1981, 1982 and 1983. Other studies in the same catchment suggested that the storm runoff was mainly generated from the valley floor, where the water table is close to the soil surface, leading to saturation excess overland flow (SOF). The Asu data confirm that the valley floor is the source of the storm runoff. The water table in the valley floor is controlled by two factors, (i) in the short-term, local vertical recharge direct to the water table and (ii) in the longer term, the discharge of groundwater from beneath the plateau and slope areas, fed by deep drainage (recharge) from these areas. There is also some evidence that interflow and return flow contribute to storm runoff in very large events. The main reason for the large difference in storm runoff between the catchments is that in the much larger Asu catchment, the proportion of the catchment occupied by valley floor (32%), with a shallow water table, is much greater than in the Barro Branco. In addition, the rainfall was well above average in 2002. These results show that it may not be appropriate to scale up from process studies in very small catchments, because of scale-related changes in processes.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Processes of streamflow...
doc Directory Contentaccess
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agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://mtc-m16b.sid.inpe.br/ibi/cptec.inpe.br/walmeida/2004/08.04.11.14
zipped data URLhttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/walmeida/2004/08.04.11.14
Languageen
Target Filehodnett_processes.pdf
User GroupFabia
administrator
estagiario
Visibilityshown
Copy HolderSID/SCD
5. Allied materials
Next Higher Units8JMKD3MGPCW/46JKC45
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
Empty Fieldsarchivingpolicy archivist callnumber copyright creatorhistory descriptionlevel dissemination documentstage doi edition editor electronicmailaddress identifier isbn issn keywords label lineage mark mirrorrepository nextedition notes numberofvolumes orcid pages parameterlist parentrepositories previousedition previouslowerunit progress publisher publisheraddress readergroup readpermission rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url versiontype volume
7. Description control
e-Mail (login)marciana
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