The  business  value  is  the  obtained  framework  that 
will  forecast  temperature  fluctuations  observed  in 
the next hour. As previous results have emphasised, 
the  framework  is  adaptable,  which  means  that  it  is 
also  possible  to  indicate  how  much  ahead  can  be 
predicted.  The  AODPF  has  demonstrated  an 
excellent  ability  to  make  automated  prediction 
model  choices  and  shows  how  many  data  points 
need  to  be  selected  to  make  valuable  predictions. 
One  automated  approach  takes  and  gradually 
reduces  the  total  number  of  data  points  until  the 
optimal number of data points is obtained. When this 
happens,  the  number  of  data  points  is  indicated,  a 
forecast is made starting from a specific data  point, 
and an automated forecast is made. As the forecasts 
to  be  made  are  already  known  from  the  data,  the 
AODPF  demonstrates  the  ability  to  perform  the 
calculation  and  adjustment  algorithm  using 
standardised forecasting  methods  such  as  AR,  MA, 
ARMA, and ARIMA. 
The  main  advantage  of  using  the  Kalman  filter 
can  also  be  compared  (see  Fig.  2).  The  green  lines 
(Fig.  2)  indicate  the  original data  used  to  make  the 
predictions. However, the actual data with which the 
forecasts  are  compared  are  already  highlighted  in 
red. Blue colour shows the ARIMA model,  the light 
blue  colour  –  the  ARMA  model,  the  black  colour 
refers to the AR model, while the purple colour 
denotes  the  MA  model.  Parameters  that  are  not 
needed  for  the  respective  models  are  replaced  with 
0. It mainly refers to the AR and MA models. If the 
model  is  not  shown  in  the  figure,  it  will  not  be 
possible to create it; unfortunately, it happens. At the 
bottom,  100  data  points  are  shown  so  that  it  is 
possible  to  see  the  predictions.  The  most  critical 
result  of  RMSE  using  each  method  is  also 
highlighted. 
The  final  results  are  demonstrated  in  Fig.  2, 
which  highlights  all  the  factors  of  the  experiment. 
There  are  seven  different  experiment  situations  in 
the experiment plan. 
First,  all  metrological  stations  with  no  missing 
data  are  used  in  experiment  scenario  #1.  The 
ARIMA forecasting method is  employed by 30  out 
of  54  meteorological  stations  in  Latvia,  and  the 
Kalman  filter  is  not  used;  the  number  of 
observations varies depending on the meteorological 
station,  which  averages  five  observations  every  11 
minutes.  One,  five,  and  10  data  points  are  forecast 
using  five  distinct  forecasting  beginning  points  at 
6:00, 9:00, 12:00, 18:00, and 21:00 in one, five, and 
ten-step  forecasts.  The  first  situation  is  the  one,  in 
which the AODPF framework is not used. 
Second, all  meteorological stations with missing 
data  are  used  in  experiment  scenario  #2.  The 
ARIMA forecasting method is  employed by 30  out 
of  54  meteorological  stations  in  Latvia,  and  the 
Kalman  filter  is  not  used;  the  number  of 
observations varies depending on the meteorological 
station,  which  averages  five  observations  every  11 
minutes.  One,  five,  and  10  data  points  are  forecast 
using  five  distinct  forecasting  beginning  points  at 
6:00, 9:00, 12:00, 18:00, and 21:00 in one, five, and 
ten-step forecasts. Scenario #2 is an experiment with 
the AODPF framework. 
Third,  applying  the  ARIMA  forecasting 
technique and the Kalman filter, experiment scenario 
#3  is  carried  out  using  all  meteorological  stations 
that do not have missing data, accounting for 30 out 
of  54  meteorological  stations  in  Latvia.  One,  five, 
and  10  data  points  are  forecast  using  five  distinct 
forecasting  beginning  points  at  6:00,  9:00,  12:00, 
18:00, and 21:00 in one, five, and ten-step forecasts. 
Fourth,  experiment  scenario  #4  uses  all  54 
meteorological stations, employing the missing data 
filling  methods  for  20  meteorological  stations.  The 
ARIMA  forecasting  method  is  utilised  rather  than 
the Kalman  filter.  One,  five, and 10  data  points are 
forecast  using  five  distinct  forecasting  beginning 
points at 6:00, 9:00, 12:00, 18:00, and 21:00 in one, 
five, and ten-step forecasts. 
Fifth,  experiment  scenario  #5  is  carried  out 
utilising  the  missing  data  filling  methods  for  20 
meteorological  stations,  totalling  54  meteorological 
stations.  Again,  the  Kalman  filter  and  the  ARIMA 
prediction algorithm are used. One, five, and 10 data 
points  are  forecast  with  five  distinct  forecasting 
beginning  points  at  6:00,  9:00,  12:00,  18:00,  and 
21:00 in one, five, and ten-step forecast. 
Sixth, experiment scenario #6 is carried out using 
the  missing  data  filling  methods  for  20 
meteorological  stations,  totalling  54  meteorological 
stations. The ARIMA forecasting method is utilised 
rather than the Kalman filter. A new data source has 
been  added  to  the  Latvian  Environment,  Geology 
and  Meteorology  Centre  (LVGMC)  dataset, 
consisting of 25 additional meteorological stations in 
the city’s central area. One, five, and ten data points 
are  forecast  with  five  different  forecasting  starting 
points at 6:00, 9:00, 12:00, 18:00, and 21:00 in one, 
five, and ten-step forecast. 
Finally, last experiment scenario #7 is performed 
with  all  meteorological  stations,  making  up  54 
meteorological  stations,  using  the  missing  data 
filling  methods  for  20  meteorological  stations.  The 
ARIMA prediction method and the Kalman filter are 
used. Moreover, an additional data source, LVGMC