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Why the damped trend works. Everette S. Gardner, Jr. Eddie McKenzie. Empirical performance of the damped trend. “The damped trend can reasonably claim to be a benchmark forecasting method for all others to beat.” (Fildes et al., JORS, 2008) - PowerPoint PPT Presentation
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Why the damped trend works
Everette S. Gardner, Jr. Eddie McKenzie
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Empirical performance of the damped trend
“The damped trend can reasonably claim to be a benchmark forecasting method for all others to beat.” (Fildes et al., JORS, 2008)
“The damped trend is a well established forecasting method that should improve accuracy in practical applications.” (Armstrong, IJF, 2006)
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Why the damped trend works Practice
Optimal parameters are often found at the boundaries of the [0, 1] interval. Thus fitting the damped trend is a means of automatic method selection from numerous special cases.
Theory The damped trend and each special case has an
underlying random coefficient state space (RCSS) model that adapts to changes in trend.
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The damped trend method
Recurrence form )()1( 11 tttt by
11 )1(( ) tttt bb
th by ttht )...(ˆ 2
Error-correction form
tttt eb 11
ttt ebb 1
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Special case when ø = 1
1. Holt method )()1( 11 tttt by
11 )1(( ) tttt bb
tbhy ttht ˆ
1 1
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Special cases when β = 02. SES 3. SES with drift (Hyndman and Billah, IJF, 2003)
10 , 1 : by ttt 1)1(
bhy ttht ˆ
4. SES with damped drift
10 , 10 : by ttt 1)1(
by httht )...(ˆ 2
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Fit periods for M3 Annual series # YB067
0
1,000
2,000
3,000
4,000
5,000
1 2 3 4 5 6 7 8 9 10 11 12 13 14
Year
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Special cases when β = 0, continued5. Random walk 6. Random walk with drift
1 , 0 : bytt
bhy ttht ˆ
7. Random walk with damped drift
1 , 10 : bytt
by httht )...(ˆ 2
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Special cases when α = β = 0
8. 1 Linear trend
9. 10 Modified exponential trend
10. 0 Simple average
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Fitting the damped trend to the M3 series Multiplicative seasonal adjustment Initial values for level and trend
Local: Regression on first 5 observations Global: Regression on all fit data
Optimization (Minimum SSE) Parameters only Parameters and initial values (no significant difference
from parameters only)
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M3 mean symmetric APE (Horizons 1-18)Makridakis & Hibon (2000) with backcasted initial values 13.6%
Gardner & McKenzie (2010) with local initial values 13.5 with global initial values 13.8
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Method Local Global
Damped trend 43.0% 27.8%Holt 10.0
1.8
SES w/ damped drift 24.8 23.5 SES w/ drift 2.4 11.6SES 0.8 0.6RW w/ damped drift 7.8 9.6RW w/ drift 2.5 8.4RW 0.0 0.0Modified exp. trend 8.3 8.7Linear trend 0.1 7.9Simple average 0.3 0.0
Methods identified in the M3 time seriesInitial values
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Initial values
Components identified in the M3 time series
Component Local Global
Damped trend 51.3% 36.5%
Damped drift 32.6 33.6
Trend 10.1 9.7
Drift 4.9 20.0
Constant level 1.2 0.6
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Method Ann. Qtr. Mon.Damped trend 25.9% 47.1% 47.5%Holt 17.4
14.2 3.6
SES w/ damped drift 17.7 16.7 33.6 SES w/ drift 3.6 3.7 1.1SES 0.2 0.4 1.5RW w/ damped drift 18.3 9.0 1.9RW w/ drift 7.8 2.1 0.4RW 0.0 0.0 0.0Modified exp. trend 9.1 6.0 10.1Linear trend 0.2 0.1 0.1Simple average 0.0 0.8 0.2
Methods identified by type of data(Local initial values)
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Rationale for the damped trend Brown’s (1963) original thinking:
Parameters are constant only within local segments of the time series
Parameters often change from one segment to the next Change may be sudden or smooth
Such behavior can be captured by a random coefficient state space (RCSS) model
There is an underlying RCSS model for the damped trend and each of its special cases
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SSOE state space models for the damped trend
Constant coefficient Random coefficient tttt by 11 ttttt vbAy 11
tttt hb 111 ttttt vhbA *111
ttt hbb 21 tttt vhbAb *21
{At} are i.i.d. binary random variates White noise innovation processes ε and are different Parameters h and h* are related but usually different
ttttt vbAy 11
v
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Runs of linear trends in the RCSS model
With a strong linear trend, {At } will consist of long runs of 1s with occasional 0s.
With a weak linear trend, {At } will consist of long runs of 0s with occasional 1s.
In between, we get a mixture of models on shorter time scales, i.e. damping.
tttt vhbAb *21
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Advantages of the RCSS model Allows both smooth and sudden changes
in trend.
is a measure of the persistence of the linear trend. The mean run length is thus
and
RCSS prediction intervals are much wider than those of constant coefficient models.
)1/( )1( tAP
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Conclusions Fitting the damped trend is actually a means of
automatic method selection.
There is an underlying RCSS model for the damped trend and each of its special cases.
SES with damped drift was frequently identified in the M3 series and should receive some consideration in empirical research.
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ReferencesPaper and presentation available at:www.bauer.uh.edu/gardner