Comparison of machine learning and process-based SWAT model in simulating streamflow in the Upper Indus Basin

被引:34
|
作者
Rahman, Khalil Ur [1 ]
Quoc Bao Pham [2 ]
Jadoon, Khan Zaib [3 ]
Shahid, Muhammad [4 ]
Kushwaha, Daniel Prakash [5 ]
Duan, Zheng [6 ]
Mohammadi, Babak [6 ]
Khedher, Khaled Mohamed [7 ,8 ]
Duong Tran Anh [9 ]
机构
[1] Tsinghua Univ, Dept Hydraul Engn, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] Thu Dau Mot Univ, Inst Appl Technol, Thu Dau Mot, Binh Duong Prov, Vietnam
[3] Islamic Int Univ, Dept Civil Engn, Islamabad 44000, Pakistan
[4] Natl Univ Sci & Technol NUST, SCEE, NICE, Islamabad 44000, Pakistan
[5] GB Pant Univ Agr & Technol, Coll Technol, Dept Soil & Water Conservat Engn, Pantnagar 263145, Uttar Pradesh, India
[6] Lund Univ, Dept Phys Geog & Ecosyst Sci, Solvegatan 12, SE-22362 Lund, Sweden
[7] King Khalid Univ, Coll Engn, Dept Civil Engn, Abha 61421, Saudi Arabia
[8] High Inst Technol Studies, Dept Civil Engn, Mrezgua Univ Campus, Nabeul 8000, Tunisia
[9] HUTECH Univ, 475A,Ward 25, Ho Chi Minh City, Vietnam
关键词
Hydrological modeling; Glacier; SWAT; MLP; Upper Indus Basin; ARTIFICIAL NEURAL-NETWORK; WATER ASSESSMENT-TOOL; RIVER-BASINS; HYDROLOGICAL MODEL; RUNOFF SIMULATION; NUTRIENT LOADS; SNOW COVER; SCALE; FLOW; CALIBRATION;
D O I
10.1007/s13201-022-01692-6
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This study appraised and compared the performance of process-based hydrological SWAT (soil and water assessment tool) with a machine learning-based multi-layer perceptron (MLP) models for simulating streamflow in the Upper Indus Basin. The study period ranges from 1998 to 2013, where SWAT and MLP models were calibrated/trained and validated/tested for multiple sites during 1998-2005 and 2006-2013, respectively. The performance of both models was evaluated using nash-sutcliffe efficiency (NSE), coefficient of determination (R-2), Percent BIAS (PBIAS), and mean absolute percentage error (MAPE). Results illustrated the relatively poor performance of the SWAT model as compared with the MLP model. NSE, PBIAS, R-2, and MAPE for SWAT (MLP) models during calibration ranged from the minimum of 0.81 (0.90), 3.49 (0.02), 0.80 (0.25) and 7.61 (0.01) to the maximum of 0.86 (0.99), 9.84 (0.12), 0.87 (0.99), and 15.71 (0.267), respectively. The poor performance of SWAT compared with MLP might be influenced by several factors, including the selection of sensitive parameters, selection of snow specific sensitive parameters that might not represent actual snow conditions, potential limitations of the SCS-CN method used to simulate streamflow, and lack of SWAT ability to capture the hydropeaking in Indus River sub-basins (at Shatial bridge and Bisham Qila). Based on the robust performance of the MLP model, the current study recommends to develop and assess machine learning models and merging the SWAT model with machine learning models.
引用
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页数:19
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