Abstract

Hydrologic models are essential tools for understanding hydrologic processes, such as precipitation, which is a fundamental component of the water cycle. For an improved understanding and the evaluation of different precipitation datasets, especially their applicability for hydrologic modelling, three kinds of precipitation products, CMADS, TMPA-3B42V7 and gauge-interpolated datasets, are compared. Two hydrologic models (IHACRES and Sacramento) are applied to study the accuracy of the three types of precipitation products on the daily streamflow of the Lijiang River, which is located in southern China. The models are calibrated separately with different precipitation products, with the results showing that the CMADS product performs best based on the Nash–Sutcliffe efficiency, including a much better accuracy and better skill in capturing the streamflow peaks than the other precipitation products. The TMPA-3B42V7 product shows a small improvement on the gauge-interpolated product. Compared to TMPA-3B42V7, CMADS shows better agreement with the ground-observation data through a pixel-to-point comparison. The comparison of the two hydrologic models shows that both the IHACRES and Sacramento models perform well. The IHACRES model however displays less uncertainty and a higher applicability than the Sacramento model in the Lijiang River basin.

Highlights

  • Hydrologic models are essential tools for understanding processes of the hydrologic cycle and provide useful information for sustainable water-resource management [1]

  • Our work presents a comparative analysis for different precipitation datasets and their applicability for hydrologic modelling, including gauge-interpolated datasets, TMPA-3B42V7 and CMADS precipitation products

  • The results show that the IHACRES and Sacramento models demonstrate a good and similar performance in the Lijiang River basin

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Summary

Introduction

Hydrologic models are essential tools for understanding processes of the hydrologic cycle and provide useful information for sustainable water-resource management [1]. Precipitation is the main driving factor of hydrologic processes. Accurate estimation of precipitation is crucial for reliable hydrologic predictions [2]. Precipitation data from a ground observational network have been used as the source of areal precipitation estimates used in watershed modelling. Ground-based precipitation observation networks are sparsely distributed and may be unable to represent the spatial variability of the precipitation completely.

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