SWAT Literature Database for Peer-Reviewed Journal Articles

Title:Stream flow simulation and verification in ungauged zones by coupling hydrological and hydrodynamic models: A case study of the Poyang Lake ungauged zone 
Authors:Zhang, L., J. Lu, X. Chen, D. Liang, X. Fu, S. Sauvage and J.-M. S. Perez 
Year:2017 
Journal:Hydrology and Earth System Sciences 
Volume:21(11) 
Pages:5842-5861 
Article ID: 
DOI:10.5194/hess-21-5847-2017 
URL (non-DOI journals): 
Model:SWAT 
Broad Application Category:hydrologic only 
Primary Application Category:model interface 
Secondary Application Category:hydrologic assessment 
Watershed Description:19,867 km^2 Poyang Lake ungauged zone drainage area, a tributary of the Yangtze River that is located in southeast China. 
Calibration Summary: 
Validation Summary: 
General Comments: 
Abstract:To solve the problem of estimating and verifying stream flow without direct observation data, we estimated stream flow in ungauged zones by coupling a hydrological model with a hydrodynamic model, using the Poyang Lake basin as a test case. To simulate the stream flow of the ungauged zone, we built a soil and water assessment tool (SWAT) model for the entire catchment area covering the upstream gauged area and ungauged zone, and then calibrated the SWAT model using the data in the gauged area. To verify the results, we built two hydrodynamic scenarios (the original and adjusted scenarios) for Poyang Lake using the Delft3D model. In the original scenario, the upstream boundary condition is the observed stream flow from the upstream gauged area, while, in the adjusted scenario, it is the sum of the observed stream flow from the gauged area and the simulated stream flow from the ungauged zone. The experimental results showed that there is a stronger correlation and lower bias (R2 D 0.81, PBIASD10.00 %) between the observed and simulated stream flow in the adjusted scenario compared to that (R2 D 0.77, PBIASD20.10 %) in the original scenario, suggesting the simulated stream flow of the ungauged zone is reasonable. Using this method, we estimated the stream flow of the Poyang Lake ungauged zone as 16.4 (+ or -6.2 billionm3 a-1), representing ~11.24% of the annual total water yield of the entire watershed. Of the annual water yield, 70% (11.48 billion m3 a-1) is concentrated in the wet season, while 30% (4.92 billion m3 a-1) comes from the dry season. The ungauged stream flow significantly improves the water balance with the closing error decreased by 13.48 billion m3 a-1 (10.10% of the total annual water resource) from 30.20 (+ or -9.1 billionm3 a-1) (20.10% of the total annual water resource) to 16.72 (+ or -8.53 billion m3 a-1) (10.00% of the total annual water resource). The method can be extended to other lake, river, or ocean basins where observation data is unavailable. 
Language:English 
Keywords: