Transcript
Page 1: Econ 427 lecture 14 slides

Byron Gangnes

Econ 427 lecture 14 slidesEcon 427 lecture 14 slides

Forecasting with MA Models

Page 2: Econ 427 lecture 14 slides

Byron Gangnes

Optimal forecastOptimal forecast• One which, given the available information, has the

smallest average loss. – This will normally be the conditional mean (the mean given that

we are a particular time period, t; i.e. given an “information set”):

E( yT +h |ΩT )

• The best linear forecast will then be the linear approximation to this, called the linear projection,

P( yT +h |ΩT )

Remember the info set will generally be current and past values of y and innovations (epsilons).

Page 3: Econ 427 lecture 14 slides

Byron Gangnes

Optimal forecast for MAOptimal forecast for MA• Like before (Chs. 5 and 6), we calculate the optimal point

forecast by writing down the process at period T+h and then “projecting it” on the information available at time T.– Book’s MA(2) example:

• Write out the process at time T+1:

yt=εt +θ1εt−1 +θ2εt−2

εt∼WN(0,σ 2 )

yT +1 =εT+1 +θ1εT +θ2εT−1

• Projecting this on the time T info set,

(remember that expectations of future innovs are zero)

Page 4: Econ 427 lecture 14 slides

Byron Gangnes

Optimal forecast for MAOptimal forecast for MA• For period T+2:

• Projecting this on the time T info set,

• And so forth… So for periods beyond T+2,

Why is that? an MA(q) process is not forecastable more than q

steps ahead. Why? Recall Autocorr function drops to 0 after q steps

yT +2 =εT+2 +θ1εT+1 +θ2εT

y

T +2,T =θ2εT

y

T +h,T =0, for h> 2

Page 5: Econ 427 lecture 14 slides

Byron Gangnes

Uncertainty around optimal forecastUncertainty around optimal forecast• We would like to know how much uncertainty there will

be around point estimates of forecasts.

• To see that, let’s look at the forecast errors,

Why are errors serially correlated? Why can’t we use this info to improve forecast?

• Same for all forecasts T+h, h>2

e

T +h,T =yT+h −yT+h,T

e

T +1,T = εT+1 +θ1εT +θ2εT−1( )− θ1εT +θ2εT−1( ) =εT+1     (WN)

e

T +2,T = εT+2 +θ1εT+1 +θ2εT( )− θ2εT( )                   =εT+2 +θ1εT+1     (MA(1))

e

T +3,T = εT+3 +θ1εT+3 +θ2εT+1( )− 0( )                       =εT+3 +θ1εT+3 +θ2εT+1     (MA(2))

Page 6: Econ 427 lecture 14 slides

Byron Gangnes

Uncertainty around optimal forecastUncertainty around optimal forecast• forecast error variance is the variance of eT+h,T

We can use these conditional variances to construct confidence intervals. What will they look like?

Notice that the error variance is less than the underlying variability of the series yt for h < q. Note that because of its MA(2) form, the variance of yt equals

σ12 =σ 2

σ 22 =σ 2(1+θ1

2 )

σ h2 =σ 2(1+θ1

2 +θ22 ), h> 2

e

T +1,T =εT+1

e

T +2,T =εT+2 +θ1εT+1    

var( yt) =σ 2(1+θ1

2 +θ22 )


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