and science of predicting future events. This can be
solved by involving historical data retrieval and
projecting it into the future with a form of
mathematical model
(Heizer & Render, 2009).
2.2 Forecasting Functions and
Purposes
The forecasting function is seen when making a
decision. A good decision is a decision based on
consideration of what will happen when the decision
is implemented. If the prediction is not precise, then
forecasting problems are also a problem that is
always faced (Al Rahamneh, 2017). Forecasting has
the objective to review current and past company
policies and see the extent of influence in the future
(Heizer & Render, 2009).
2.3 Forecasting Techniques
Qualitative forecasting is forecasting techniques
used when past data are not available or available
but the amount is not much. Qualitative techniques
are based on a common sense approach in filtering
information into useful forms. Quantitative
forecasting methods are forecasting that is based on
manipulating available historical data adequately
and without intuition or subjective judgment of the
person making the forecast
(Makridakis et al., 2003).
2.4 Smoothing Method
Smoothing Method is the method of forecasting by
smoothing past data, which is to take an average of
several years take forecast value the next few years
(Hyndman et al., 2002). The general formula of the
exponential smoothing method is:
𝐹
𝛼𝑋
𝑖𝛼
𝐹
(1)
with:
𝐹
= forecast for the next period
𝑋
𝑡
= actual data in t period
𝐹
𝑡
= forecast t period
𝛼
= smoothing parameters
If the general formula is expanded it will change to:
𝐹
𝛼𝑋
𝑖𝛼
𝑋
⋯
𝛼
𝑖𝛼
𝑋
(2)
2.5 Brown’s Double Exponential
Smoothing
According to Makridakis et al., (2003) Brown’s
Double Exponential Smoothing is a linear model
proposed by Brown. This method is used when data
shows a trend. A trend is a smoothed estimate of the
average growth at the end of each period
(Makridakis et al., 2003).
The rationale for Double Exponential Smoothing
from Brown is similar to Double Moving Average
because both Single Smoothing and Double
Smoothing values lag behind the actual data when
there is an element of trend (Noeryanti et al., 2012).
Difference between Single Smoothing value and
Double Smoothing value (𝑆
𝑆
) can be added
with single smoothing value (𝑆
) and adjusted for
trend. This method uses two smoothing stages with
the same parameter, that is α. α values is between 0
and 1. The steps in using Double Exponential
Smoothing from Brown are as follows:
1. Determine single smoothing value (𝑆
)
𝑆
𝛼𝑋
1𝛼
𝑆
(3)
2. Determine double smoothing value (𝑆
)
𝑆
𝛼𝑆
1𝛼
𝑆
(4)
3. Determine the smoothing constant value (𝑎
)
𝑎
2𝑆
𝑆
(5)
4. Determine the smoothing constant value (b
t
)
𝑏
𝛼
1𝛼
𝑆
𝑆
(6)
5. Determine the forecast value for next period
(F
t+m
)
𝐹
𝑎
𝑏
𝑚
(7)
a
t
and b
t
values can be taken at the last
observation value forecast calculation and m is
the number of periods to be predicted.
To be able to use the formula, values 𝑆
and 𝑆
must be available. But when t = 1, these values are
not available. Because these values must be
determined at the beginning of the period, to solved
this problem can be done by setting 𝑆
and 𝑆
same
with X
1
value (actual data)
(Makridakis et al., 2003).
2.6 Measuring Forecasting Accuracy
Mean Absolute Percentage Error
(MAPE)
MAPE or mean absolute percentage error is the
average of the total error percentage (difference)
between the actual data and the result forecasting
data. The formula for calculating MAPE is as
follows:
𝑀𝐴𝑃𝐸
|
𝑃𝐸
|
𝑁
(8)
Percentage error of forecast:
𝑃𝐸
𝑋
𝐹
𝑋
100
(9)
with: