Abstract Our work presents the analysis of the data following the steps as given below: identification of data set periods, constructing and modelling the empirical semivariogram for single location and using the Kriging mapping function as modelling of TEC maps in mid-latitude during disturbed and quiet days. Based on the semivariogram, weights for the Kriging interpolation are estimated.
Characteristic of modelling spatial processes using geostatistical analysis
Advances in Space Research ; 64 , 2 ; 415-426
2019-04-17
12 pages
Article (Journal)
Electronic Resource
English
Semivariogram , Kriging , Modelling , Geostatistics , TEC
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