Abstract

Radar-rain gauge merging methods have been widely used to produce high-quality precipitation with fine spatial resolution by combing the advantages of the rain gauge observation and the radar quantitative precipitation estimation (QPE). Different merging methods imply a specific choice on the treatment of radar and rain gauge data. In order to improve their applicability, significant studies have focused on evaluating the performances of the merging methods. In this study, a categorization of the radar-rain gauge merging methods was proposed as: (1) Radar bias adjustment category, (2) radar-rain gauge integration category, and (3) rain gauge interpolation category for a total of six commonly used merging methods, i.e., mean field bias (MFB), regression inverse distance weighting (RIDW), collocated co-kriging (CCok), fast Bayesian regression kriging (FBRK), regression kriging (RK), and kriging with external drift (KED). Eight different storm events were chosen from semi-humid and semi-arid areas of Northern China to test the performance of the six methods. Based on the leave-one-out cross validation (LOOCV), conclusions were obtained that the integration category always performs the best, the bias adjustment category performs the worst, and the interpolation category ranks between them. The quality of the merging products can be a function of the merging method that is affected by both the quality of radar QPE and the ability of the rain gauge to capture small-scale rainfall features. In order to further evaluate the applicability of the merging products, they were then used as the input to a rainfall-runoff model, the Hybrid-Hebei model, for flood forecasting. It is revealed that a higher quality of the merging products indicates a better agreement between the observed and the simulated runoff.

Highlights

  • Precipitation is a key driving component for hydrological water cycle processes at regional and global scales

  • We focused on merging rain gauge and radar data, and radar data were considered as the only additional information in this method

  • A value of 2 was given in the regression inverse distance weighting (RIDW) method, and a minimum of three stations were used in the kriging-based methods

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Summary

Introduction

Precipitation is a key driving component for hydrological water cycle processes at regional and global scales. A catchment reacts very to intense rainfall due to its steep slopes and shallow soils, and precipitation data with a high spatial and temporal distribution is critical for forecasting flash flooding events [1]. These events invariably have the characteristics of high intensity and sudden occurrence, and under climate change, the needs for high resolution and accurate rainfall data have increased, because effective hydrological forecasting depends greatly on precipitation accuracy [2,3,4]. High-resolution precipitation based on rain gauge data are usually geometrically interpolated from a limited number of observation points using geographic information systems (GIS)

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