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CPS1934 Atikur R. K. et al.
                  Category 3: This category is supposed to has a lower degree of RTI episodes
                  and  can  be  defined  as  ( 4  <  () ≤  6 ) ∪ ( () ≤  4  ∩
                   () >  2 ), that is, this category can be defined based on defined rolling
                  statistics as ( 4  <  (|) ≤  6 ) ∪ ( (|) ≤  4  ∩  (|) >  2 ).
                                    ℎ                ℎ              
                      Since RTI episode is a count response variable, we fit panel generalized
                  linear models (PGLM) by using these categories as predictor variables along
                  with  rolling  mean  deviation  of  sea  level  pressure  from  normal  level
                  (−1013.25) and rolling mean for wind speed (). Results shown in
                  Table 1 divulge that a negative binomial model for PGLM over a Poisson model
                  is preferred based on the likelihood ratio test (LRT). The negative binomial
                  model  in  PGLM  reveals  that  the  Category  2  and  Category  3  of  climatic
                  condition is likely to exhibit almost 28% and 20% less RTI episodes compared
                  to the climatic condition under Category 1.
                      We also note that for one unit increase in ( − 1013.25), RTI episodes are
                  likely to increase by 1.6%. When (  −  1013.25) < 0, low pressure in the sea
                  causes rainfall that results in less dust particle in the air. Thus when (  −
                   1013.25) > 0 there are less rainfall events and are likely to have more dust in
                  the air. This little change may be due to regulation of dust and other particles
                  in the air by rainfall. Further, one unit increase in (), eight days rolling
                  mean of wind speed, results in almost 16.51% increase in RTI episodes. This
                  may be due to blowing more dust with increased wind speed, which is likely
                  to  affect  people  with  dust  allergies  and  other  respiratory  diseases  related
                  problems.

                            Table 1. Panel generalized linear model for RTI episodes




















                  Category  1:  reference  category.  Here, ( − 1013.25) and () are
                  rolling mean deviation of sea level pressure from its normal level and rolling
                  mean for wind speed, respectively.

                      We have already explored that the rolling time series statistics of climatic
                  variables have significant effect on RTI episodes. Thus a forecasting exercise


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