Abstract

Selecting an optimum number of calibration sites for hydrological modeling is challenging. Modelers often spend a lot of time and effort on trial and error because there is no guide. We propose a novel entropy method to automate the selection of the optimum combination of calibration sites. To illustrate, the proposed entropy method is applied using discharge data from one river basin in Korea. First, different combinations of discharge-gauging sites were grouped based on the maximum information estimated by the entropy method. Then, a hydrological model was set up for the study basin and was calibrated by estimating optimal parameters using a genetic algorithm at the discharge-gauging sites. The calibration result confirmed that the model’s performance was best when it was calibrated using the site number and combination suggested by the entropy method. In addition, the entropy method was useful in reducing the time and effort of model calibration. Therefore, we suggest and confirm the applicability of the entropy method in selecting calibration sites for hydrological modeling.

Highlights

  • Hydrological models are increasingly used to evaluate the impacts of climate, land use, and crop management practices on the quantity of water resources [1]

  • The applicability of the SWAT model was outstanding in the study basin as the coefficient of correlation (CC), Root-Mean-Square Error (RMSE), and Nash-Sutcliffe efficiency (NSE) were 0.782, 147.4, and 0.482, respectively, even in the case where no calibration was conducted (#0); it was confirmed that the results were improved slightly when the model was calibrated

  • The purpose of this study was to review the applicability of the entropy method in selecting the calibration sites for hydrological modeling

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Summary

Introduction

Hydrological models are increasingly used to evaluate the impacts of climate, land use, and crop management practices on the quantity of water resources [1]. The two main objectives of hydrological modeling are to explore the implications of making certain assumptions about the nature of the real-world system and to predict the system’s behavior under a set of naturally occurring circumstances [2]. The successful application of any hydrological model is dependent on the quality of its calibration [3]. As a result, developing calibration strategies is a requirement for their proper application in hydrological modeling. Model parameters are estimated by minimizing the deviation between the measured and simulated discharges. Researchers have suggested a number of methodologies to improve calibration-related issues [4,5,6,7,8,9,10,11]

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