SWAT model application and prediction uncertainty analysis in the Lake Tana Basin, Ethiopia

被引:205
作者
Setegn, Shimelis G. [1 ]
Srinivasan, Ragahavan [2 ]
Melesse, Assefa M. [3 ]
Dargahi, Bijan [1 ]
机构
[1] Royal Inst Technol KTH, Dept Land & Water Resources Engn, Hydraul Engn Div, Stockholm, Sweden
[2] Texas A&M Univ, Spatial Sci Lab, College Stn, TX USA
[3] Florida Int Univ, Dept Environm Sci, Miami, FL 33199 USA
关键词
SWAT; Lake Tana; hydrological modelling; SUFI-2; GLUE; ParaSol; WATER-QUALITY; CHAOHE BASIN; RIVER-BASIN; CALIBRATION; HYDROLOGY; FUTURE; RUNOFF; FLOW;
D O I
10.1002/hyp.7457
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Lake Tana Basin is of significant importance to Ethiopia concerning water resources aspects and the ecological balance of the area. Many years of mismanagement, wetland losses due to urban encroachment and population growth, and droughts are causing its rapid deterioration. The main objective of this study was to assess the performance and applicability of the soil water assessment tool (SWAT) model for prediction of streamflow in the Lake Tana Basin, so that the influence of topography, land use, soil and climatic condition on the hydrology of Lake Tana Basin can be well examined. The physically based SWAT model was calibrated and validated for four tributaries of Lake Tana. Sequential uncertainty fitting (SUFI-2), parameter solution (ParaSol) and generalized likelihood uncertainty estimation (GLUE) calibration and uncertainty analysis methods were compared and used for the set-up of the SWAT model. The model evaluation statistics for streamflows prediction shows that there is a good agreement between the measured and simulated flows that was verified by coefficients of determination and Nash Sutcliffe efficiency greater than 0.5. The hydrological water balance analysis of the basin indicated that baseflow is an important component of the total discharge within the study area that contributes more than the surface runoff. More than 60% of losses in the watershed are through evapotranspiration. Copyright (C) 2009 John Wiley & Sons, Ltd.
引用
收藏
页码:357 / 367
页数:11
相关论文
共 43 条
[1]  
Abbaspour KC, 2005, MODSIM 2005: INTERNATIONAL CONGRESS ON MODELLING AND SIMULATION: ADVANCES AND APPLICATIONS FOR MANAGEMENT AND DECISION MAKING, P2449
[2]   Modelling hydrology and water quality in the pre-alpine/alpine Thur watershed using SWAT [J].
Abbaspour, Karim C. ;
Yang, Jing ;
Maximov, Ivan ;
Siber, Rosi ;
Bogner, Konrad ;
Mieleitner, Johanna ;
Zobrist, Juerg ;
Srinivasan, Raghavan .
JOURNAL OF HYDROLOGY, 2007, 333 (2-4) :413-430
[3]  
Abbaspour KC, 2004, VADOSE ZONE J, V3, P1340
[4]  
[Anonymous], 1972, NAT ENG HDB
[5]  
[Anonymous], 1998, SOIL TERR DAT NE AFR
[6]   Large area hydrologic modeling and assessment - Part 1: Model development [J].
Arnold, JG ;
Srinivasan, R ;
Muttiah, RS ;
Williams, JR .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 1998, 34 (01) :73-89
[7]   A COMPREHENSIVE SURFACE-GROUNDWATER FLOW MODEL [J].
ARNOLD, JG ;
ALLEN, PM ;
BERNHARDT, G .
JOURNAL OF HYDROLOGY, 1993, 142 (1-4) :47-69
[8]   Automated methods for estimating baseflow and ground water recharge from streamflow records [J].
Arnold, JG ;
Allen, PM .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 1999, 35 (02) :411-424
[9]   THE FUTURE OF DISTRIBUTED MODELS - MODEL CALIBRATION AND UNCERTAINTY PREDICTION [J].
BEVEN, K ;
BINLEY, A .
HYDROLOGICAL PROCESSES, 1992, 6 (03) :279-298
[10]  
CHEKOL DA, 2006, MODELING HYDROLOGY S