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

被引:7
作者
Betancur, Sebastian Balbin [1 ]
Gastmans, Didier [1 ]
Vasquez, Katherine Vasquez [2 ]
Santarosa, Lucas Vituri [1 ]
dos Santos, Vinicius [1 ]
Kirchheim, Roberto Eduardo [3 ]
机构
[1] Univ Estadual Paulista, Ctr Estudos Ambientais, Rio Claro, SP, Brazil
[2] Univ Sao Paulo, Lab Hidrol Florestal, Piracicaba, SP, Brazil
[3] Serv Geol Brasil, Sao Paulo, SP, Brazil
来源
RBRH-REVISTA BRASILEIRA DE RECURSOS HIDRICOS | 2020年 / 25卷
基金
巴西圣保罗研究基金会;
关键词
Atrato river basin; Flow duration curves; Principal component analysis; Colombia; GROUPING GEOMORPHIC PARAMETERS; FLOW DURATION CURVES; GROUNDWATER RECHARGE; REGIONAL PATTERNS; PHYSICAL CONTROLS; CLIMATE-CHANGE; SURFACE-WATER; STREAMFLOW; IMPACT; COVER;
D O I
10.1590/2318-0331.252020190165
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
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.
引用
收藏
页数:12
相关论文
共 59 条
[1]   Principal component analysis [J].
Abdi, Herve ;
Williams, Lynne J. .
WILEY INTERDISCIPLINARY REVIEWS-COMPUTATIONAL STATISTICS, 2010, 2 (04) :433-459
[2]  
[Anonymous], 2014, ARS CLIM CHANG 2014
[3]  
[Anonymous], 2016, B INVEST MAR COST
[4]  
[Anonymous], 2018, R LANG ENV STAT COMP
[5]   Flow Regime Classification and Hydrological Characterization: A Case Study of Ethiopian Rivers [J].
Berhanu, Belete ;
Seleshi, Yilma ;
Demisse, Solomon S. ;
Melesse, Assefa M. .
WATER, 2015, 7 (06) :3149-3165
[6]  
Best AE, 2003, MODSIM 2003: INTERNATIONAL CONGRESS ON MODELLING AND SIMULATION, VOLS 1-4, P861
[7]   Regionalization of Flow-Duration Curves through Catchment Classification with Streamflow Signatures and Physiographic-Climate Indices [J].
Boscarello, Laura ;
Ravazzani, Giovanni ;
Cislaghi, Alessio ;
Mancini, Marco .
JOURNAL OF HYDROLOGIC ENGINEERING, 2016, 21 (03)
[8]   How does forest cover impact water flows and ecosystem services? Insights from "real-life" catchments in Wallonia (Belgium) [J].
Brogna, D. ;
Vincke, C. ;
Brostaux, Y. ;
Soyeurt, H. ;
Dufrene, M. ;
Dendoncker, N. .
ECOLOGICAL INDICATORS, 2017, 72 :675-685
[9]   A review of paired catchment studies for determining changes in water yield resulting from alterations in vegetation [J].
Brown, AE ;
Zhang, L ;
McMahon, TA ;
Western, AW ;
Vertessy, RA .
JOURNAL OF HYDROLOGY, 2005, 310 (1-4) :28-61
[10]   Impact of forest cover changes on annual streamflow and flow duration curves [J].
Brown, Alice E. ;
Western, Andrew W. ;
McMahon, Thomas A. ;
Zhang, Lu .
JOURNAL OF HYDROLOGY, 2013, 483 :39-50