Hydrological responses in equatorial watersheds indicated by Principal Components Analysis (PCA) - study case in Atrato River Basin (Colombia)
Autor(a) principal: | |
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Data de Publicação: | 2020 |
Outros Autores: | , , , , |
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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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) |
repository.mail.fl_str_mv |
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1808128753635688448 |