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Trend and Seasonal
Components
Group Member :
Anna Revin Nadita (2201794750)
Cindy Aprilia (2201788981)
Fitri Andriyani (2201806744)
Prastika Ambarita (2201801983)
Time series with deterministic
components
 Up until now we assumed our time series is generated by a stationary process - either a
white noise, an autoregressive, a moving-average or an ARMA process.
 However, this is not usually the case with real-world data - they are often governed by a
(deterministic) trend and they might have (deterministic) cyclical or seasonal components
in addition to the irregular/remainder (stationary process) component:
Trend component - a long-term increase or decrease in the data which might not be linear.
Sometimes the trend might change direction as time increases.
Cyclical component - exists when data exhibit rises and falls that are not of fixed period. The
average length of cycles is longer than the length of a seasonal pattern. In practice, the
trend component is assumed to include also the cyclical component. Sometimes the trend
and cyclical components together are called as trend-cycle.
Seasonal component - exists when a series exhibits regular fluctuations based on the season
(e.g. every month/quarter/year). Seasonality is always of a fixed and known period.
Irregular component - a stationary process.
In order to remove the deterministic components, we
can decompose our time series into separate stationary
and deterministic components.
Time series decomposition
 The general mathematical representation of the decomposition approach:
Yt = f (Tt , St , Et )
where
) Yt is the time series value (actual data) at period t;
) Tt is a deterministic trend-cycle or general movement component;
) St is a deterministic seasonal component
) Et is the irregular (remainder or residual) (stationary) component.
The exact functional form of f (·) depends on the decomposition method used.
Trend Stationary Time Series
 A common approach is to assume that the equation has an additive
form:
Yt = Tt + St + Et
Trend, seasonal and irregular components are simply added together to give the
observed series.
Alternatively, the multiplicative decomposition has the form:
Yt = Tt · St · Et
Trend, seasonal and irregular components are multiplied together to give the
observed series.
Additive or multiplicative?
 An additive model is appropriate if the magnitude of the seasonal
fluctuations does not vary with the level of time series;
 The multiplicative model is appropriate if the seasonal fluctuations increase
or decrease proportionally with increases and decreases in the level of the
series.
 Multiplicative decomposition is more prevalent with economic series because
most seasonal economic series do have seasonal variations which increase
with the level of the series.
 Rather than choosing either an additive or multiplicative decomposition, we
could transform the data beforehand.
Transforming data of a multiplicative
model
 Very often the transformed series can be modeled additively when the
original data is not additive. In particular, logarithms turn a multiplicative
relationship into an additive relationship:
) if our model is
Yt = Tt · St · Et
) then taking the logarithms of both sides gives us:
log (Yt ) = log(Tt ) + log(St ) + log(Et )
 So, we can fit a multiplicative relationship by fitting a more convenient
additive relationship to the logarithms of the data and then to move back to
the original series by exponentiating.
Basic Steps in Decomposition
 Estimate the trend. Two approaches:
) Using a smoothing procedure;
) Specifying a regression equation for the trend;
 De-trending the series:
) For an additive decomposition, this is done by subtracting the trend estimates
from the series;
) For a multiplicative decomposition, this is done by dividing the series by the
estimated trend values.
 Estimating the seasonal factors from the de-trended series:
) Calculate the mean (or median) values of the de-trended series for each
specific period (for example, for monthly data - to estimate the seasonal effect
of January - average the de-trended values for all January values in the series
etc);
) Alternatively, the seasonal effects could also be estimated along with the trend
by specifying a regression equation.
 The number of seasonal factors is equal to the frequency of the series (e.g.
monthly data = 12 seasonal factors, quarterly data = 4, etc.).
Basic Steps in Decomposition
 The seasonal effects should be normalized:
) For an additive model, seasonal effects are adjusted so that the average of d
seasonal components is 0 (this is equivalent to their sum being equal to 0);
) For a multiplicative model, the d seasonal effects are adjusted so that they
average to 1 (this is equivalent to their sum being equal to d );
 Calculate the irregular component
 Analyze the residual component. Whichever method was used to decompose
the series, the aim is to produce stationary residuals.
 Choose a model to fit the stationary residuals (e.g. see ARMA models).
 Forecasting can be achieved by forecasting the residuals and combining with
the forecasts of the trend and seasonal components.
Estimating the trend, Tt
 There are various ways to estimate the trend Tt at time t but a relatively
simple procedure which does not assume any specific form of Tt is to
calculate a moving average centered on t.
 A moving average is an average of a specific number of time series values
around each value of t in the time series, with the exception of the first few
and last few terms (this procedure is available in R with the decompose
function). This method smoothes the time series.
 The estimation depends on the seasonality of the time series:
) If the time series has no seasonal component;
) If the time series contains a seasonal component;
 Smoothing is usually done to help us better see patterns (like the trend) in
the time series by smoothing out the irregular roughness to see a clearer
signal. For seasonal data, we might smooth out the seasonality so that we
can identify the trend.
Estimating Tt if the time series has no
seasonal component
 In order to estimate the trend, we can take any odd number, for example, if l
= 3, we can estimate an additive model:
 In this case, we are calculating the averages, either:
) centered around t - one element to the left (past) and one element to the
right (future),
) or alternatively - two elements to the left of t (past values at t − 1 and t − 2).
Estimating Tt if the time series contains a
seasonal component
 If the time series contains a seasonal component and we want to average it
out, the length of the moving average must be equal to the seasonal
frequency (for monthly series, we would take l = 12). However, there is a
slight hurdle.
 Suppose, our time series begins in January (t = 1) and we average up to
December (t = 12). This averages corresponds to a time t = 6.5 (time
between June and July).
 When we come to estimate seasonal effects, we need a moving average at
integer times. This can be achieved by averaging the average of January to
December and the average of February (t = 2) up to January
 (t = 13). This average of the two moving averages corresponds to t = 7 and
the process is called centering.
Thank You

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Trend and Seasonal Components

  • 1. Trend and Seasonal Components Group Member : Anna Revin Nadita (2201794750) Cindy Aprilia (2201788981) Fitri Andriyani (2201806744) Prastika Ambarita (2201801983)
  • 2. Time series with deterministic components  Up until now we assumed our time series is generated by a stationary process - either a white noise, an autoregressive, a moving-average or an ARMA process.  However, this is not usually the case with real-world data - they are often governed by a (deterministic) trend and they might have (deterministic) cyclical or seasonal components in addition to the irregular/remainder (stationary process) component: Trend component - a long-term increase or decrease in the data which might not be linear. Sometimes the trend might change direction as time increases. Cyclical component - exists when data exhibit rises and falls that are not of fixed period. The average length of cycles is longer than the length of a seasonal pattern. In practice, the trend component is assumed to include also the cyclical component. Sometimes the trend and cyclical components together are called as trend-cycle. Seasonal component - exists when a series exhibits regular fluctuations based on the season (e.g. every month/quarter/year). Seasonality is always of a fixed and known period. Irregular component - a stationary process.
  • 3. In order to remove the deterministic components, we can decompose our time series into separate stationary and deterministic components.
  • 4. Time series decomposition  The general mathematical representation of the decomposition approach: Yt = f (Tt , St , Et ) where ) Yt is the time series value (actual data) at period t; ) Tt is a deterministic trend-cycle or general movement component; ) St is a deterministic seasonal component ) Et is the irregular (remainder or residual) (stationary) component. The exact functional form of f (·) depends on the decomposition method used.
  • 5. Trend Stationary Time Series  A common approach is to assume that the equation has an additive form: Yt = Tt + St + Et Trend, seasonal and irregular components are simply added together to give the observed series. Alternatively, the multiplicative decomposition has the form: Yt = Tt · St · Et Trend, seasonal and irregular components are multiplied together to give the observed series.
  • 6. Additive or multiplicative?  An additive model is appropriate if the magnitude of the seasonal fluctuations does not vary with the level of time series;  The multiplicative model is appropriate if the seasonal fluctuations increase or decrease proportionally with increases and decreases in the level of the series.  Multiplicative decomposition is more prevalent with economic series because most seasonal economic series do have seasonal variations which increase with the level of the series.  Rather than choosing either an additive or multiplicative decomposition, we could transform the data beforehand.
  • 7. Transforming data of a multiplicative model  Very often the transformed series can be modeled additively when the original data is not additive. In particular, logarithms turn a multiplicative relationship into an additive relationship: ) if our model is Yt = Tt · St · Et ) then taking the logarithms of both sides gives us: log (Yt ) = log(Tt ) + log(St ) + log(Et )  So, we can fit a multiplicative relationship by fitting a more convenient additive relationship to the logarithms of the data and then to move back to the original series by exponentiating.
  • 8. Basic Steps in Decomposition  Estimate the trend. Two approaches: ) Using a smoothing procedure; ) Specifying a regression equation for the trend;  De-trending the series: ) For an additive decomposition, this is done by subtracting the trend estimates from the series; ) For a multiplicative decomposition, this is done by dividing the series by the estimated trend values.  Estimating the seasonal factors from the de-trended series: ) Calculate the mean (or median) values of the de-trended series for each specific period (for example, for monthly data - to estimate the seasonal effect of January - average the de-trended values for all January values in the series etc); ) Alternatively, the seasonal effects could also be estimated along with the trend by specifying a regression equation.  The number of seasonal factors is equal to the frequency of the series (e.g. monthly data = 12 seasonal factors, quarterly data = 4, etc.).
  • 9. Basic Steps in Decomposition  The seasonal effects should be normalized: ) For an additive model, seasonal effects are adjusted so that the average of d seasonal components is 0 (this is equivalent to their sum being equal to 0); ) For a multiplicative model, the d seasonal effects are adjusted so that they average to 1 (this is equivalent to their sum being equal to d );  Calculate the irregular component  Analyze the residual component. Whichever method was used to decompose the series, the aim is to produce stationary residuals.  Choose a model to fit the stationary residuals (e.g. see ARMA models).  Forecasting can be achieved by forecasting the residuals and combining with the forecasts of the trend and seasonal components.
  • 10. Estimating the trend, Tt  There are various ways to estimate the trend Tt at time t but a relatively simple procedure which does not assume any specific form of Tt is to calculate a moving average centered on t.  A moving average is an average of a specific number of time series values around each value of t in the time series, with the exception of the first few and last few terms (this procedure is available in R with the decompose function). This method smoothes the time series.  The estimation depends on the seasonality of the time series: ) If the time series has no seasonal component; ) If the time series contains a seasonal component;  Smoothing is usually done to help us better see patterns (like the trend) in the time series by smoothing out the irregular roughness to see a clearer signal. For seasonal data, we might smooth out the seasonality so that we can identify the trend.
  • 11. Estimating Tt if the time series has no seasonal component  In order to estimate the trend, we can take any odd number, for example, if l = 3, we can estimate an additive model:  In this case, we are calculating the averages, either: ) centered around t - one element to the left (past) and one element to the right (future), ) or alternatively - two elements to the left of t (past values at t − 1 and t − 2).
  • 12. Estimating Tt if the time series contains a seasonal component  If the time series contains a seasonal component and we want to average it out, the length of the moving average must be equal to the seasonal frequency (for monthly series, we would take l = 12). However, there is a slight hurdle.  Suppose, our time series begins in January (t = 1) and we average up to December (t = 12). This averages corresponds to a time t = 6.5 (time between June and July).  When we come to estimate seasonal effects, we need a moving average at integer times. This can be achieved by averaging the average of January to December and the average of February (t = 2) up to January  (t = 13). This average of the two moving averages corresponds to t = 7 and the process is called centering.