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Modern Geomatics Technologies and Applications


             PM 2.5 concentrations in the nearest   Inversion intensity parameter   Meteorological data of synoptic stations
                  two neighbourhoods


                                                                               Generate a raster map for each
                                                                               parameter by Kriging method


                                                                             Determine the parameters at each air
                                                                                 pollution measuring point
                                      Pre-processing of meteorological data
                                      and the concentration of pollutants
                                                        Filling Gap


                                                       Smoothing Data
                                                                                                Time Data

                                              Creating training datasets based on Table 3

                                     Decision Tree algorithm                                   Topographic
                                                                                                  Data
                                           C4.5 Algorithm          CART algorithm



                                       Cross-validation, determining the Overall Accuracy and Kappa
                                                          index

                                               Generate a pollution classification map
                                                  and forecast و یجنسرابتعا

                                                    Fig.1. Proposed method


          The values of inversion intensity and interpretation of these values are shown in Table 1[14]:


                                  Table 1 Inversion intensity values and interpretation of these values
                                     Stability     Division   Range of temperature changes in
                                   classification   classification   the vertical direction (C / 100m◦)

                                    Very unstable    A                    <-1.9
                                                                        ∆  
                                                                        ∆  
                                   Unstable medium   B                -1.9<= <-1.7
                                                                           ∆  
                                                                           ∆  
                                   Slightly unstable   C              -1.7<= <-1.5
                                                                           ∆  
                                                                           ∆  
                                      Neutral        D                -1.5<= <-0.5
                                                                           ∆  
                                                                           ∆  
                                    A little stable   E               -0.5<= <1.5
                                                                           ∆  
                                                                           ∆  
                                    Stable medium    F
                                                                           ∆  
                                                                      1.5<= <0.4
                                                                           ∆  
                                     Very stable     G                       ∆  
                                                                        0.4<=
                                                                             ∆  

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