Case Studies
Feb 15, 2022

Application of Regularized Dynamic System Response Curve for Runoff Correction Based on HBV Model: Case Study of Shiquan Catchment, China

Publication: Journal of Hydrologic Engineering
Volume 27, Issue 4

Abstract

Error correction is an important postprocess technique in hydrological modeling. The paper aims to investigate the effectiveness and suitability of a recently proposed error correction method, the regularized dynamic system response curve (RDSRC) method in the Hydrologiska Byråns Vattenbalansavdelning (HBV) model. In the HBV model, the effective precipitation can reflect the error of model inputs so it is used for runoff error correction. Three commonly used statistics [Nash-Sutcliffe efficiency (NSE) coefficient, root-mean-squared error (RMSE), and percent bias (PBIAS)] were used to evaluate the model performance. In this study, the RDSRC method was tested by a synthetic case and a real case. Results of the synthetic case showed that the NSE, RMSE, and PBIAS of runoff simulation before correction were 0.943, 182.73  m3/s, and 0.626%, respectively, while those statistics after correction by the RDSRC method were 1,0.61  m3/s, and 0.002%, respectively. In the real case, the HBV model was used for daily runoff modeling in the Shiquan catchment in China; meanwhile, the RDSRC method and the AR(2) model were compared for runoff error correction. The corrected daily runoff by the RDSRC method had much better accuracy than the second-order autoregressive [AR(2)] model and the HBV model. After correction of the RDSRC method, the NSE of the HBV model increased from 0.83 to 0.946, whereas the RMSE of the HBV model decreased by 43.6%, from 246.37 to 138.96  m3/s. This case study provides two main conclusions: (1) the RDSRC method had better performance in runoff error correction than the AR(2) model, and (2) the RDSRC method is an effective alternative for daily runoff error correction when used for the HBV model.

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Data Availability Statement

Some or all data, models, or codes that support the findings of this study are available from the corresponding author upon reasonable request (models of HBV and RDSRC, rainfall and runoff data of Shiquan catchment).

Acknowledgments

This work was supported by the Postgraduate Research & Practice Innovation Program of Jiangsu Province (KYCX20_0467), the Fundamental Research Funds for the Central Universities (B200203053, B200201027), National Natural Science Foundation of China (51709077), and Open Research Fund of the Yellow River Sediment Key Laboratory of Ministry of Water Resources (201804). The China Scholarship Council (No. 202106710059) is also gratefully acknowledged. The authors would like to thank reviewers for their in-depth reviews and constructive suggestions. The remarks and summary of reviewer comments provided by the editor and reviewers are also greatly appreciated, and facilitated major improvements in this paper.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 27Issue 4April 2022

History

Received: Mar 5, 2021
Accepted: Jan 11, 2022
Published online: Feb 15, 2022
Published in print: Apr 1, 2022
Discussion open until: Jul 15, 2022

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Ph.D. Candidate, College of Hydrology and Water Resources, Hohai Univ., Nanjing 210098, China (corresponding author). Email: [email protected]
Professor, College of Hydrology and Water Resources, Hohai Univ., Nanjing 210098, China. Email: [email protected]
Zhangling Xiao
Ph.D. Candidate, College of Hydrology and Water Resources, Hohai Univ., Nanjing 210098, China.
Wei Si
Associate Professor, College of Hydrology and Water Resources, Hohai Univ., Nanjing 210098, China.
Yiqun Sun, Ph.D.
Postdoc, College of Hydrology and Water Resources, Hohai Univ., Nanjing 210098, China.

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Cited by

  • Objectivity verification experiment of the dynamic system response curve method for streamflow simulation, Journal of Hydrology, 10.1016/j.jhydrol.2022.128969, 617, (128969), (2023).
  • Comprehensive Review: Advancements in Rainfall-Runoff Modelling for Flood Mitigation, Climate, 10.3390/cli10100147, 10, 10, (147), (2022).

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