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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3JLE2CH
Repositorysid.inpe.br/mtc-m21b/2015/06.11.16.37   (restricted access)
Last Update2015:07.06.13.37.44 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2015/06.11.16.37.32
Metadata Last Update2021:01.02.03.53.36 (UTC) administrator
DOI10.1002/joc.4038
ISSN0899-8418
Citation KeyViolaMelChaYanGom:2015:AsClCh
TitleAssessing climate change impacts on Upper Grande River Basin hydrology, Southeast Brazil
Year2015
MonthMay
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size1610 KiB
2. Context
Author1 Viola, M. R.
2 Mello, C. R.
3 Chan, Chou Sin
4 Yanagi, S. N.
5 Gomes, Jorge Luis
Resume Identifier1
2
3
4
5 8JMKD3MGP5W/3C9JGRQ
Group1
2
3
4
5 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation1 Universidade Federal do Tocantins (UFTO)
2 Universidade Federal de Lavras (UFLA)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal de Lavras (UFLA)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1
2
3 chou.sinchan@cptec.inpe.br
4
5 jorge.gomes@cptec.inpe.br
JournalInternational Journal of Climatology
Volume35
Number6
Pages1054-1068
Secondary MarkA1_CIÊNCIAS_AGRÁRIAS_I A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_GEOCIÊNCIAS A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
History (UTC)2015-06-11 16:37:32 :: simone -> administrator ::
2021-01-02 03:53:36 :: administrator -> simone :: 2015
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsEta model
hydrological simulation
climate change
A1B scenario
run-off components
LASH model
AbstractBrazilian electric power is mostly based on hydraulics sources through hydropower plant reservoirs that are fed by rivers located in Southeast Brazil. Possible changes in climate can affect the energy supply of the country. The objective of this work is to assess the possible changes in the hydrology of the Upper Grande River Basin (UGRB) under a future climate change scenario, using the Lavras Simulation of Hydrology (LASH) model forced by the outputs of the Eta model, a regional climate model, which was driven by HadCM3 A1B scenario for three time slices in the period between 2011 and 2099. Owing to the surface heterogeneity of the region, the hydrologic model was previously calibrated for four watersheds of the UGRB, which are located in its headwater region and evaluated against observational time series of the present climate period, 1961-1990. In the first future time slice, 2011-2040, the results showed a small reduction in the annual run-off, but for the other time slices, the trend changed to strong increase in most of the watersheds. The water budget in the region calculated from the Eta model agreed with the run-off trends, as water excess reduced in the first time slice and gradually increased towards the end of the century. The run-off components showed intraseasonal variability. The reduction of rains in the end of winter, the dry period in the region, and in the beginning of spring, may cause a change in the dynamics of the groundwater recharge, affecting the base flow, which can extend and intensify the flow recession period, and therefore affect the availability of water resources. On the other hand, the increase of rains during the summer, the rainy season of the region, caused an increase of the direct surface run-off, which can modify the flood regimes of the rivers in the region.
AreaMET
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4. Conditions of access and use
Languageen
Target FileViola_assessing climate.pdf
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Visibilityshown
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Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/43SKC35
Citing Item Listsid.inpe.br/bibdigital/2021/01.01.17.20 1
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
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