[1]LI Yan,ZHU Jun,HU Ya,et al.Comparison Analysis on Different Spatial Interpolation Methods to Simulate Monthly Precipitation in Sichuan Province[J].Research of Soil and Water Conservation,2017,24(01):151-154,160.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
24
Number of periods:
2017 01
Page number:
151-154,160
Column:
Public date:
2017-02-28
- Title:
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Comparison Analysis on Different Spatial Interpolation Methods to Simulate Monthly Precipitation in Sichuan Province
- Author(s):
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LI Yan1, ZHU Jun1,2, HU Ya1,2, ZHANG Heng1,2
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1. Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 611756, China;
2. State-Province Joint Engineering Laboratory of Spatial Information Technology for High-Speed Railway Safety, Southwest Jiaotong University, Chengdu 611756, China
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- Keywords:
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spatial interpolation; precipitation simulation; cross validation; error analysis
- CLC:
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P208;P332
- DOI:
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- Abstract:
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The precipitation information can’t be obtained directly in some areas because the meteorological observation points are few in the western region of China. Using the spatial data interpolation methods to estimate the precipitation in the adjacent areas is one of the important means. For the less observation points in Sichuan Province, we combine with the digital elevation model (DEM) of the spatial resolution of 90 m×90 m, and use the ordinary of inverse distance weighted interpolation (IDW), the inverse distance weighted interpolation of considering each point elevation (IDW), local polynomial interpolation (LPI), the ordinary Kriging interpolation method (OK) and the collaborative Kriging interpolation method (CK) to interpolate the every monthly and annual average precipitation in Sichuan Province. The cross checking method was used to verify the results of interpolation, and the average error (MAE) and the root mean square error (RMS) were used as the criteria for evaluating the five interpolation methods. The results show that the IDW interpolation of considering the points elevation is more precise than the ordinary IDW, can significantly improve the accuracy of interpolation, Kriging average error and root mean square error is smaller than IDW and local polynomial interpolation, the collaborative Kriging has better interpolation results because of considering the influence of digital elevation model on rainfall. Therefore, collaborative Kriging is more suitable for spatial interpolation of rainfall data in mountain area.