Abstract

Precipitation is considered a crucial component in the hydrological cycle and changes in its spatial pattern directly influence the water resources. We compare different interpolation techniques in predicting the spatial distribution pattern of precipitation in Chongqing. Six interpolation methods, i.e., Inverse Distance Weighting (IDW), Radial Basis Function (RBF), Diffusion Interpolation with Barrier (DIB), Kernel Interpolation with Barrier (KIB), Ordinary Kriging (OK) and Empirical Bayesian Kriging (EBK), were applied to estimate different rainfall patterns. Annual mean, rainy season and dry-season precipitation was calculated from the daily precipitation time series of 34 meteorological stations with a time span of 1991 to 2019, based on Leave-One-Out Cross-Validation (LOOCV), Mean Square Error (MSE), Mean Absolute Error (MAE), Mean Absolute Percentage Error (MAPE), Symmetric Mean Absolute Percentage Error (SMAPE) and Nash–Sutcliffe Efficiency coefficient (NSE) as validation indexes of the applied models for calculating the error degree and accuracy. Correlation test and Spearman coefficient was performed on the estimated and observed values. A method combining Entropy Weight and Technique for Order Preference by Similarity to Ideal Solution (Entropy-Weighted TOPSIS) was introduced to rank the performance of six interpolation methods. The results indicate that interpolation technique performs better in estimating during periods of low precipitation (i.e., dry season, relative to rainy season and mean annual). The performance priorities of the six methods under the combined multiple precipitation distribution patterns are KIB > EBK > OK > RBF > DIB > IDW. Among them, KIB method has the highest accuracy which maps more accurate precipitation surfaces, with the disadvantage that estimation error is prone to outliers. EBK method is the second highest, and IDW method has the lowest accuracy with a high degree of error. This paper provides information for the application of interpolation methods in estimating rainfall spatial pattern and for water resource management of concerned regions.

Highlights

  • Precipitation is the most important climatic variable in hydrology and in water resource management, due to its critical effect on the spatial patterns of water availability [1].The information of precipitation is vital for analyzing of regional water resources, the prediction and management of drought and flood disasters, and the management of the ecological environment [2,3]

  • Statistical analysis shows that approximately 75% of annual precipitation in Chongqing is concentrated in the rainy season (May–October), while approximately 25% is distributed in dry season (November–April)

  • This paper compared the performance of different interpolation methods (IDW, Radial Basis Function (RBF), Diffusion Interpolation with Barrier (DIB), Kernel Interpolation with Barrier (KIB), Ordinary Kriging (OK), Empirical Bayesian Kriging (EBK)) in predicting the spatial distribution pattern of precipitation based on Geographical Information System (GIS) technology applied to three rainfall patterns, i.e., annual mean, rainy-season, and dry-season precipitation

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Summary

Introduction

Precipitation is the most important climatic variable in hydrology and in water resource management, due to its critical effect on the spatial patterns of water availability [1].The information of precipitation is vital for analyzing of regional water resources, the prediction and management of drought and flood disasters, and the management of the ecological environment [2,3]. Precipitation is the most important climatic variable in hydrology and in water resource management, due to its critical effect on the spatial patterns of water availability [1]. Of regional climate dynamics and for evaluating weather and climate models, which possibly helps manage water resources and deals with flood crises as well [8,9,10]. The assessment of the temporal and spatial distribution patterns of precipitation remains a difficult task owing to the availability of a sufficient network of stations and gauges as well as the complex nature of different regions [21]

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