Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)

Detalhes bibliográficos
Autor(a) principal: Betancur, Sebastian Balbin [UNESP]
Data de Publicação: 2020
Outros Autores: Gastmans, Didier [UNESP], Vasquez, Katherine Vasquez, Santarosa, Lucas Vituri [UNESP], Santos, Vinicius dos [UNESP], Kirchheim, Roberto Eduardo
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1590/2318-0331.252020190165
http://hdl.handle.net/11449/209569
Resumo: The Atrato river basin is located in the Pacific fringe of Colombia, region with one of the highest precipitation rates in the world. The main purpose of this study is to determine the dominant processes in the hydrological responses along 17 sub-basins within the basin using principal component analysis. Watersheds located at the headwater presented a fast or medium response to the precipitation events, while higher flow homogeneity was observed in watersheds located at the lower portions of the basin. Three principal components were responsible for explaining 85.18% of the total variance. The component PC1 revealed the largest contributions for low flow behavior, being associated to precipitation, characteristic discharge values, compactness index, soil coverage and soil coarse textures. The component PC2 was assigned to the geological variables, fine and average texture soil and the average basin slope. Finally, the component PC3 has shown to be related to high flow patterns (maximum characteristic discharge values Q(5) and Q(1)), igneous rocks and length of the basin. Highest specific discharge was associated to alluvial deposits and forest cover, whereas the slope was considered determinant for the run-off generation.
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spelling Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)Atrato river basinFlow duration curvesPrincipal component analysisColombiaThe Atrato river basin is located in the Pacific fringe of Colombia, region with one of the highest precipitation rates in the world. The main purpose of this study is to determine the dominant processes in the hydrological responses along 17 sub-basins within the basin using principal component analysis. Watersheds located at the headwater presented a fast or medium response to the precipitation events, while higher flow homogeneity was observed in watersheds located at the lower portions of the basin. Three principal components were responsible for explaining 85.18% of the total variance. The component PC1 revealed the largest contributions for low flow behavior, being associated to precipitation, characteristic discharge values, compactness index, soil coverage and soil coarse textures. The component PC2 was assigned to the geological variables, fine and average texture soil and the average basin slope. Finally, the component PC3 has shown to be related to high flow patterns (maximum characteristic discharge values Q(5) and Q(1)), igneous rocks and length of the basin. Highest specific discharge was associated to alluvial deposits and forest cover, whereas the slope was considered determinant for the run-off generation.Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Univ Estadual Paulista, Ctr Estudos Ambientais, Rio Claro, SP, BrazilUniv Sao Paulo, Lab Hidrol Florestal, Piracicaba, SP, BrazilServ Geol Brasil, Sao Paulo, SP, BrazilUniv Estadual Paulista, Ctr Estudos Ambientais, Rio Claro, SP, BrazilFAPESP: 2018/06666-4Assoc Brasileira Recursos Hidricos-abrhUniversidade Estadual Paulista (Unesp)Universidade de São Paulo (USP)Serv Geol BrasilBetancur, Sebastian Balbin [UNESP]Gastmans, Didier [UNESP]Vasquez, Katherine VasquezSantarosa, Lucas Vituri [UNESP]Santos, Vinicius dos [UNESP]Kirchheim, Roberto Eduardo2021-06-25T12:22:37Z2021-06-25T12:22:37Z2020-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article12application/pdfhttp://dx.doi.org/10.1590/2318-0331.252020190165Rbrh-revista Brasileira De Recursos Hidricos. Porte Alegre: Assoc Brasileira Recursos Hidricos-abrh, v. 25, 12 p., 2020.1414-381Xhttp://hdl.handle.net/11449/20956910.1590/2318-0331.252020190165S2318-03312020000100241WOS:000580447000001S2318-03312020000100241.pdfWeb of Sciencereponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengRbrh-revista Brasileira De Recursos Hidricosinfo:eu-repo/semantics/openAccess2024-04-10T19:22:25Zoai:repositorio.unesp.br:11449/209569Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T17:05:11.023014Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
title Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
spellingShingle Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
Betancur, Sebastian Balbin [UNESP]
Atrato river basin
Flow duration curves
Principal component analysis
Colombia
title_short Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
title_full Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
title_fullStr Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
title_full_unstemmed Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
title_sort Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
author Betancur, Sebastian Balbin [UNESP]
author_facet Betancur, Sebastian Balbin [UNESP]
Gastmans, Didier [UNESP]
Vasquez, Katherine Vasquez
Santarosa, Lucas Vituri [UNESP]
Santos, Vinicius dos [UNESP]
Kirchheim, Roberto Eduardo
author_role author
author2 Gastmans, Didier [UNESP]
Vasquez, Katherine Vasquez
Santarosa, Lucas Vituri [UNESP]
Santos, Vinicius dos [UNESP]
Kirchheim, Roberto Eduardo
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (Unesp)
Universidade de São Paulo (USP)
Serv Geol Brasil
dc.contributor.author.fl_str_mv Betancur, Sebastian Balbin [UNESP]
Gastmans, Didier [UNESP]
Vasquez, Katherine Vasquez
Santarosa, Lucas Vituri [UNESP]
Santos, Vinicius dos [UNESP]
Kirchheim, Roberto Eduardo
dc.subject.por.fl_str_mv Atrato river basin
Flow duration curves
Principal component analysis
Colombia
topic Atrato river basin
Flow duration curves
Principal component analysis
Colombia
description The Atrato river basin is located in the Pacific fringe of Colombia, region with one of the highest precipitation rates in the world. The main purpose of this study is to determine the dominant processes in the hydrological responses along 17 sub-basins within the basin using principal component analysis. Watersheds located at the headwater presented a fast or medium response to the precipitation events, while higher flow homogeneity was observed in watersheds located at the lower portions of the basin. Three principal components were responsible for explaining 85.18% of the total variance. The component PC1 revealed the largest contributions for low flow behavior, being associated to precipitation, characteristic discharge values, compactness index, soil coverage and soil coarse textures. The component PC2 was assigned to the geological variables, fine and average texture soil and the average basin slope. Finally, the component PC3 has shown to be related to high flow patterns (maximum characteristic discharge values Q(5) and Q(1)), igneous rocks and length of the basin. Highest specific discharge was associated to alluvial deposits and forest cover, whereas the slope was considered determinant for the run-off generation.
publishDate 2020
dc.date.none.fl_str_mv 2020-01-01
2021-06-25T12:22:37Z
2021-06-25T12:22:37Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1590/2318-0331.252020190165
Rbrh-revista Brasileira De Recursos Hidricos. Porte Alegre: Assoc Brasileira Recursos Hidricos-abrh, v. 25, 12 p., 2020.
1414-381X
http://hdl.handle.net/11449/209569
10.1590/2318-0331.252020190165
S2318-03312020000100241
WOS:000580447000001
S2318-03312020000100241.pdf
url http://dx.doi.org/10.1590/2318-0331.252020190165
http://hdl.handle.net/11449/209569
identifier_str_mv Rbrh-revista Brasileira De Recursos Hidricos. Porte Alegre: Assoc Brasileira Recursos Hidricos-abrh, v. 25, 12 p., 2020.
1414-381X
10.1590/2318-0331.252020190165
S2318-03312020000100241
WOS:000580447000001
S2318-03312020000100241.pdf
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Rbrh-revista Brasileira De Recursos Hidricos
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 12
application/pdf
dc.publisher.none.fl_str_mv Assoc Brasileira Recursos Hidricos-abrh
publisher.none.fl_str_mv Assoc Brasileira Recursos Hidricos-abrh
dc.source.none.fl_str_mv Web of Science
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
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