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ECONOMETRICS

Sponsored by a Grant TÁMOP-4.1.2-08/2/A/KMR-2009-0041 Course Material Developed by Department of Economics,

Faculty of Social Sciences, Eötvös Loránd University Budapest (ELTE) Department of Economics, Eötvös Loránd University Budapest

Institute of Economics, Hungarian Academy of Sciences Balassi Kiadó, Budapest

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Authors: Péter Elek, Anikó Bíró Supervised by Péter Elek

June 2010

Week 11

Nonstationary time series Content

Testing nonstationarity: unit root tests Trends and seasonal components

Material: M 613–617., 301–306., 597–602.

Example: estimating the parameter of a random walk the limit distribution of the

t-statistic is not t-distribution!

∆Xt = c + 0·Xt–1 + t

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Testing nonstationary: Dickey-Fuller test

Yt = αYt–1+ t

Equivalent: ∆Yt = (α – 1)Yt–1 + t

H0: α = 1, H1: α<1

Test: the usual t-statistic,

Under H0: the so-called Dickey–Fuller-distribution Asymptotic critical values:

5%: –1,95 (t-critical value: –1,65) 1%: –2,58 (t-critical value: –2,33)

Versions of Dickey–Fuller-test

AR(1) + constant Yt = c + αYt–1 + t

Asympt. critical value: –2,86 (5%), –3,43 (1%) AR(1) + constant + trend

Yt = c + δt + αYt–1 + t

Asympt. critical value: –3,41 (5%), –3,96 (1%) Augmented DF test:

Yt = c + δt + αYt–1 + 1·∆Yt–1 + 2·∆Yt–2 +…+ k·∆Yt–k + t

There are other stationarity tests as well (eg. KPSS)

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Example: is USA GDP difference or trend stationary?

Are the effects of shocks persistent or temporary?

Supply side: random walk (technological shocks)

Demand side: trend stationary Which shocks dominate?

Unit root test for the GDP series

The hypothesis of unit root cannot be rejected.

The conclusions are similar on larger samples, but final decision in the debate cannot be made.

2,000 3,000 4,000 5,000 6,000 7,000

1960 1965 1970 1975 1980 1985 1990 1995

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Why should we bother about stationarity?

Spurious trend in time series

Spurious trend in time series II

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Spurious regression in time series

Two independent random walks:

Xt = Xt–1 + 1t

Yt = Yt–1 + 2t

Regression: Yt = c + βXt+ ut

β = 0 because of independence, but the t-test is significant!

The t-statistic does not have a limit distribution

Reason: ut is nonstationary!

Fitting trends in the trend stationary and the difference stationary case

Simplest trend stationary case yt = β0 + β1t + ut, ut ~ IN

Trend fitting by OLS is consistent and in this case efficient (becaues of the independence of the error term)

Differentiation also yields consistency, but the independence of the error term does not hold any more: yt = β1 + ut – ut–1

Difference stationary case yt = yt–1 + β1 + ut, ut ~ IN

Trend fitting by OLS is inconsistent!

Differentiation yields a consistent (and in this case efficient) estimate:

yt = β1 + ut

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Hodrick–Prescott filter

yt: original time series st: filtered time series

If λ = 0 then yt = st for all t

If λ = ∞ then the linear trend is obtained.

A possible choice for λ: λ = 1600*(i/4)2, where i is the frequency Annual data: λ = 100

Quarterly data: λ = 1600 Monthly data: λ = 14400

Seasonality

Two types of seasonality

deterministic (can be filtered out by using dummy variables) stochastic (can be filtered out by taking seasonal differences) In practice: more difficult filtering methods

(e.g. TRAMO-SEATS)

1

2

2 1 1

1

2 ,...,

, 2

1

min

T

t

t t t

t T

t

t s t

s

s

y s s s s s

T

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Example: daily water discharge

ACF

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Example: wages

Example: seasonality in the quarterly growth rate of private sector wages

ACF of residuals

60000 80000 100000 120000 140000 160000 180000 200000

00 01 02 03 04 05 06 07

közszféra bérei (Ft/hó)

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Seminar

Nonstationary time series

Examples I.: analysis of the import time series of barium-clorid

Choice between trend stationarity and difference stationarity by the inspection of ACF and by a formal test

Fitting a linear trend and filtering by HP-filter

Fitting an AR(1) + trend to the original, and an ARMA(1,1) to the differentiated time series

Testing the uncorrelatedness of the residuals Forecasting from the model

Examples II

Analysis of quarterly macro time series

Fitting a deterministic seasonal component + AR(1) term, and seasonal component + ARMA(1,1) term

Forecasting

Hivatkozások

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