Applaying Types of Interpolation Methods for Spatial Analysis and Monitoring of SPI Drought Case study: Khorasan Razavi Province Mohsen Hamidiyanpour Ph.D Student of Natural Geography University of Tarbiyate Moallem Tehran Dr. Mohammad Saligeh Assistant Profesor of Natural Geography University of Tarbiyate Moallem Tehran Gholamabas Falah Ghlhari Ph.D Student of Natural Geography University of Isfahan

Document Type : Research Paper

10.22111/gdij.2014.242

Abstract

Drought is the most complicated natural hazards. This phenomenon has different characteristics which are calculated by different indices, where as these indices are depondant on climatic variables and meteorological stations, therefore their ability for recording is not continuse. On this basis , for estimating the amount of meteorological variables in non-sampled locations and preparing continuse maps, spatial interpolation methods are used . In this paper, fristly by using Standard Precipitation Index(SPI ),the drought severity is calculated, and then for assessment of different interpolation methods, different types of spatial interpolation methods including Kriging, Cokriging, Inverse Distance Weighting (IDW), Local Polynomial, Completely Regularzide Spline, Spline with Tension and Thin Plate Spline were used. Also for comparing interpolation methods, the cross-validation technique and error criterions including MSE,MBA , RMSE and %G were used.
The results indicate that Kriging Ordinery method is the best method for interpolation of drought severity and SPI index,   because it has the  least errors  in most of  months and in 9 months of the year, G% value is calculated as positive. In fact, this method has the least deviation. The most errors of interpolation methods is relevant to Thin Plate Spline method, indeed each of the three evaluation criteria  shows greater  value of error  than the other  methods.  
 

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History

  • Receive Date: 13 March 2013
  • Accept Date: 13 March 2013

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