Hydrological Modelling in the Ouergha Watershed by Soil and Water Analysis Tool

被引:3
|
作者
Erraioui, Lamia [1 ]
Taia, Soufiane [1 ]
Taj-Eddine, Kamal [2 ]
Chao, Jamal [1 ]
El Mansouri, Bouabid [1 ]
机构
[1] Ibn Tofail Univ, Nat Resources & Sustainable Dev Lab, Campus Maamora, Kenitra 14000, Morocco
[2] Cadi Ayyad Univ, Fac Sci Semlalia, Lab Geosci Semlalia, Marrakech 4000, Morocco
来源
JOURNAL OF ECOLOGICAL ENGINEERING | 2023年 / 24卷 / 04期
关键词
SWAT; Ouergha watershed; hydrological modelling; water balance; FLOW-DURATION CURVES; SWAT MODEL; UNCERTAINTY; CALIBRATION; BASIN; FRAMEWORK;
D O I
10.12911/22998993/161043
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Streamflow modelling is crucial for developing successful long-term management, soil conservation planning, and water resource management strategies. The current work attempts to develop a robust hydrological model that simulates streamflow with the slightest uncertainty in the calibration parameters. A physical-based and semi -distributed hydrological SWAT model was employed to assess the hydrological simulation of the Ouergha water-shed. The monthly simulation of the SWAT model achieved in the time frame from 1990 to 2013 has been split into warm-up (1990-1996), calibration (1997-2005), and validation (2006-2013). The SUFI-2 algorithm's preliminary sensitivity and uncertainty analysis was done to calibrate the model using 11 hydrologic parameters. The model's performance and robustness findings are promising. To evaluate the model, the coefficient of determination (R2), Nash-Sutcliffe efficiency (NSE), and percent of bias (PBIAS) were utilized. The value of R2, NSE, and PBIAS ranged from 0.45-0.77, 0.6-0.89, and +12.72 to +21.89% during calibration and 0.51-0.85, 0.64-0.88, and +8.82 to +22.19% during validation period, respectively. A high correlation between the observed and simulated stream -flow was recorded during the calibration and validation periods. More than 68% of the observation data are encom-passed by the 95PPU across both the calibration and validation intervals, which is excellent in terms of the P-factor and R-factor uncertainty criterion. The projected streamflow matches the observed data well graphically. Accord-ing to the total hydrological water balance study, 29% of precipitation is delivered to streamflow as runoff, whereas 54% of precipitation is lost through evapotranspiration. The recharge to the deep aquifers is 8%, whereas the lateral flow is 10%. The findings of this study will help as a roadmap for the anticipated water management activities for the basin since the management and planning of water resources require temporal and spatial information.
引用
收藏
页码:343 / 356
页数:14
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