Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple...

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Forecasting using R 1 Forecasting using R Rob J Hyndman 1.2 The forecaster’s toolbox

Transcript of Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple...

Page 1: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Forecasting using R 1

Forecasting using R

Rob J Hyndman

1.2 The forecaster’s toolbox

Page 2: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

Forecasting using R Forecasting 2

Page 3: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Forecasting

Forecasting is estimating how the sequence ofobservations will continue into the future.

We usually think probabilistically about future samplepathsWhat range of values covers the possible samplepaths with 80% probability?

Forecasting using R Forecasting 3

Page 4: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Australian beer production

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Australian beer production

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1995 2000 2005 2010Time

y

level

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95

Forecasts from ETS(M,N,M)

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Page 6: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

Forecasting using R Some simple forecasting methods 6

Page 7: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methods

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meg

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Australian quarterly beer production

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Can you think of any forecasting methods for these data?

Page 8: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methods

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Australian quarterly beer production

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Can you think of any forecasting methods for these data?

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Some simple forecasting methods

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Number of pigs slaughtered in Victoria

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How would you forecast these data?

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Some simple forecasting methods

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Number of pigs slaughtered in Victoria

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How would you forecast these data?

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Some simple forecasting methods

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Dow−Jones index

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How would you forecast these data?

Page 12: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methods

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Dow−Jones index

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How would you forecast these data?

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Some simple forecasting methodsAverage method

Forecast of all future values is equal to mean of historicaldata {y1, . . . , yT}.Forecasts: yT+h|T = y = (y1 + · · · + yT)/T

Naïve methodForecasts equal to last observed value.Forecasts: yT+h|T = yT.Consequence of efficient market hypothesis.

Seasonal naïve methodForecasts equal to last value from same season.Forecasts: yT+h|T = yT+h−km wherem = seasonal period andk = b(h− 1)/mc+1.

Forecasting using R Some simple forecasting methods 10

Page 14: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methodsAverage method

Forecast of all future values is equal to mean of historicaldata {y1, . . . , yT}.Forecasts: yT+h|T = y = (y1 + · · · + yT)/T

Naïve methodForecasts equal to last observed value.Forecasts: yT+h|T = yT.Consequence of efficient market hypothesis.

Seasonal naïve methodForecasts equal to last value from same season.Forecasts: yT+h|T = yT+h−km wherem = seasonal period andk = b(h− 1)/mc+1.

Forecasting using R Some simple forecasting methods 10

Page 15: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methodsAverage method

Forecast of all future values is equal to mean of historicaldata {y1, . . . , yT}.Forecasts: yT+h|T = y = (y1 + · · · + yT)/T

Naïve methodForecasts equal to last observed value.Forecasts: yT+h|T = yT.Consequence of efficient market hypothesis.

Seasonal naïve methodForecasts equal to last value from same season.Forecasts: yT+h|T = yT+h−km wherem = seasonal period andk = b(h− 1)/mc+1.

Forecasting using R Some simple forecasting methods 10

Page 16: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Some simple forecasting methods

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alitr

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Mean

Naïve

Seasonal Naïve

Forecasts for quarterly beer production

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Some simple forecasting methods

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Dow Jones Index (daily ending 15 Jul 94)

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Some simple forecasting methods

Mean: meanf(y, h=20)Naïve: naive(y, h=20)Seasonal naïve: snaive(y, h=20)Linear trend: forecast(tslm(y ~ trend))Linear trend with seasonal dummies:forecast(tslm(y ~ trend + season))

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Page 19: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

Forecasting using R Forecasting residuals 14

Page 20: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Forecasting residualsResiduals in forecasting: difference between observedvalue and its forecast based on all previous observations:et = yt − yt|t−1.

Assumptions

1 {et} uncorrelated. If they aren’t, then information left inresiduals that should be used in computing forecasts.

2 {et} have mean zero. If they don’t, then forecasts arebiased.

Useful properties (for prediction intervals)

3 {et} have constant variance.4 {et} are normally distributed.

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Page 21: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Forecasting residualsResiduals in forecasting: difference between observedvalue and its forecast based on all previous observations:et = yt − yt|t−1.

Assumptions

1 {et} uncorrelated. If they aren’t, then information left inresiduals that should be used in computing forecasts.

2 {et} have mean zero. If they don’t, then forecasts arebiased.

Useful properties (for prediction intervals)

3 {et} have constant variance.4 {et} are normally distributed.

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Page 22: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Forecasting residualsResiduals in forecasting: difference between observedvalue and its forecast based on all previous observations:et = yt − yt|t−1.

Assumptions

1 {et} uncorrelated. If they aren’t, then information left inresiduals that should be used in computing forecasts.

2 {et} have mean zero. If they don’t, then forecasts arebiased.

Useful properties (for prediction intervals)

3 {et} have constant variance.4 {et} are normally distributed.

Forecasting using R Forecasting residuals 15

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Example: Dow-Jones index

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Page 24: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

Naïve forecast:

yt|t−1 = yt−1

et = yt − yt−1

Note: et are one-step-forecast residuals

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Page 25: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

Naïve forecast:

yt|t−1 = yt−1

et = yt − yt−1

Note: et are one-step-forecast residuals

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Page 26: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

Naïve forecast:

yt|t−1 = yt−1

et = yt − yt−1

Note: et are one-step-forecast residuals

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Page 27: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

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Example: Dow-Jones index

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Page 29: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

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Page 30: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Example: Dow-Jones index

fc <- naive(dj)

res <- residuals(fc)

autoplot(res)

hist(res,breaks="FD")

ggAcf(res,main="")

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Page 31: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

ACF of residuals

We assume that the residuals are white noise(uncorrelated, mean zero, constant variance). If theyaren’t, then there is information left in the residualsthat should be used in computing forecasts.So a standard residual diagnostic is to check the ACFof the residuals of a forecasting method.We expect these to look like white noise.

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Portmanteau testsConsider a whole set of rk values, and develop a test to seewhether the set is significantly different from a zero set.Box-Pierce test

Q = Th∑k=1

r2kwhere h is max lag being considered and T is number ofobservations.

My preferences: h = 10 for non-seasonal data, h = 2mfor seasonal data.If each rk close to zero, Q will be small.If some rk values large (positive or negative), Q will belarge.

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Page 33: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Portmanteau testsConsider a whole set of rk values, and develop a test to seewhether the set is significantly different from a zero set.Box-Pierce test

Q = Th∑k=1

r2kwhere h is max lag being considered and T is number ofobservations.

My preferences: h = 10 for non-seasonal data, h = 2mfor seasonal data.If each rk close to zero, Q will be small.If some rk values large (positive or negative), Q will belarge.

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Page 34: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Portmanteau testsConsider a whole set of rk values, and develop a test to seewhether the set is significantly different from a zero set.Ljung-Box test

Q∗ = T(T + 2)h∑k=1

(T − k)−1r2kwhere h is max lag being considered and T is number ofobservations.

My preferences: h = 10 for non-seasonal data, h = 2mfor seasonal data.Better performance, especially in small samples.

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Page 35: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Portmanteau testsIf data are WN, Q∗ has χ2 distribution with (h− K) degreesof freedom where K = no. parameters in model.When applied to raw data, set K = 0.For the Dow-Jones example,

res <- residuals(naive(dj))

# lag=h and fitdf=K

> Box.test(res, lag=10, fitdf=0)Box-Pierce test

X-squared = 14.0451, df = 10, p-value = 0.1709> Box.test(res, lag=10, fitdf=0, type="Lj")

Box-Ljung testX-squared = 14.4615, df = 10, p-value = 0.153

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Page 36: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

Forecasting using R Lab session 3 26

Page 37: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Lab Session 3

Forecasting using R Lab session 3 27

Page 38: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

Forecasting using R Evaluating forecast accuracy 28

Page 39: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracyLet yt denote the tth observation and yt|t−1 denote itsforecast based on all previous data, where t = 1, . . . , T.Then the following measures are useful.

MAE = T−1T∑t=1|yt − yt|t−1|

MSE = T−1T∑t=1

(yt − yt|t−1)2 RMSE =

√√√√√T−1T∑t=1

(yt − yt|t−1)2

MAPE = 100T−1T∑t=1|yt − yt|t−1|/|yt|

MAE, MSE, RMSE are all scale dependent.MAPE is scale independent but is only sensible ifyt � 0 for all t, and y has a natural zero.

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Page 40: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracyLet yt denote the tth observation and yt|t−1 denote itsforecast based on all previous data, where t = 1, . . . , T.Then the following measures are useful.

MAE = T−1T∑t=1|yt − yt|t−1|

MSE = T−1T∑t=1

(yt − yt|t−1)2 RMSE =

√√√√√T−1T∑t=1

(yt − yt|t−1)2

MAPE = 100T−1T∑t=1|yt − yt|t−1|/|yt|

MAE, MSE, RMSE are all scale dependent.MAPE is scale independent but is only sensible ifyt � 0 for all t, and y has a natural zero.

Forecasting using R Evaluating forecast accuracy 29

Page 41: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracyMean Absolute Scaled Error

MASE = T−1T∑t=1|yt − yt|t−1|/Q

where Q is a stable measure of the scale of the time series{yt}.

Proposed by Hyndman and Koehler (IJF, 2006).For non-seasonal time series,

Q = (T − 1)−1T∑t=2|yt − yt−1|

works well. Then MASE is equivalent to MAE relative to anaïve method.

Forecasting using R Evaluating forecast accuracy 30

Page 42: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracyMean Absolute Scaled Error

MASE = T−1T∑t=1|yt − yt|t−1|/Q

where Q is a stable measure of the scale of the time series{yt}.

Proposed by Hyndman and Koehler (IJF, 2006).For seasonal time series,

Q = (T −m)−1T∑

t=m+1|yt − yt−m|

works well. Then MASE is equivalent to MAE relative to aseasonal naïve method.

Forecasting using R Evaluating forecast accuracy 31

Page 43: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracy

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Mean

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Forecasts for quarterly beer production

Forecasting using R Evaluating forecast accuracy 32

Page 44: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Measures of forecast accuracy

beer3 <- window(ausbeer, start=2006)accuracy(beerfit1, beer3)accuracy(beerfit2, beer3)accuracy(beerfit3, beer3)

RMSE MAE MAPE MASE

Mean method 38.95 34.46 8.33 2.35Naïve method 70.80 63.10 15.71 4.29Seasonal naïve method 13.59 12.20 2.95 0.83

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Page 45: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Training and test sets

Available data

Training set Test set(e.g., 80%) (e.g., 20%)

The test set must not be used for any aspect of modeldevelopment or calculation of forecasts.Forecast accuracy is based only on the test set.

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Page 46: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Training and test sets

beer3 <- window(ausbeer,start=1992,end=c(2005,4))beer4 <- window(ausbeer,start=2006)

fit1 <- meanf(beer3,h=20)fit2 <- naive(beer3,h=20)

accuracy(fit1,beer4)accuracy(fit2,beer4)

In-sample accuracy (one-step forecasts)

accuracy(fit1)accuracy(fit2)

Forecasting using R Evaluating forecast accuracy 35

Page 47: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Training and test sets

beer3 <- window(ausbeer,start=1992,end=c(2005,4))beer4 <- window(ausbeer,start=2006)

fit1 <- meanf(beer3,h=20)fit2 <- naive(beer3,h=20)

accuracy(fit1,beer4)accuracy(fit2,beer4)

In-sample accuracy (one-step forecasts)

accuracy(fit1)accuracy(fit2)

Forecasting using R Evaluating forecast accuracy 35

Page 48: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Beware of over-fittingA model which fits the data well does not necessarilyforecast well.A perfect fit can always be obtained by using a modelwith enough parameters. (Compare R2)Over-fitting a model to data is as bad as failing toidentify the systematic pattern in the data.Problems can be overcome by measuring trueout-of-sample forecast accuracy. That is, total datadivided into “training” set and “test” set. Training setused to estimate parameters. Forecasts are made fortest set.Accuracy measures computed for errors in test setonly.

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Page 49: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Poll: true or false?

1 Good forecast methods should have normallydistributed residuals.

2 A model with small residuals will give good forecasts.3 The best measure of forecast accuracy is MAPE.4 If your model doesn’t forecast well, you should make

it more complicated.5 Always choose the model with the best forecast

accuracy as measured on the test set.

Forecasting using R Evaluating forecast accuracy 37

Page 50: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Outline

1 Forecasting

2 Some simple forecasting methods

3 Forecasting residuals

4 Lab session 3

5 Evaluating forecast accuracy

6 Lab session 4

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Page 51: Forecasting using R - Rob J. Hyndman · 2016. 10. 7. · Forecasting using R Some simple forecasting methods 10. Some simple forecasting methods. 400 450 500 1995 2000 2005 2010.

Lab Session 4

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