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