Do Seasonal Adjustments Induce Noncausal Dynamics in Inflation Rates?
Abstract
:1. Introduction
2. Mixed Causal-Noncausal Models
2.1. Model Representation
2.2. Estimation
3. Seasonal Adjustment Methods
3.1. The Linear X-11 Seasonal Filter
3.2. Properties of Seasonal Adjustment
3.3. Seasonal Adjustment for Mixed Processes
4. Simulation Study
4.1. Purely Causal and Noncausal Processes
4.1.1. Case 1: X-11 Seasonally Adjusted Series
4.1.2. Case 2: Deterministic Seasonal Adjustment
4.2. Mixed Causal-Noncausal Processes
5. Seasonal Adjustment, Noncausality and Inflation Rates
5.1. Data
5.2. Results
5.3. Considerations
6. Conclusions
Acknowledgments
Author Contributions
Conflicts of Interest
Appendix A. Autocovariances and Spectra
Appendix A.1. White Noise with Seasonal Dummies
Appendix A.2. AR(1) with Seasonal Dummies
Appendix B. Graphs
References
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1. | The term ‘approximate’ stems from the fact that the sample used in the likelihood contains only terms. As shown in Breidt et al. (1991), this quantity is only an approximation of the true joint density of the data vector . |
2. | Taking degrees of freedom equal to 1,2,...,5 give similar qualitative results. As shown in Hecq et al. (2016), identification in finite samples becomes more difficult when the degrees of freedom parameter is high. In practice, a value around 10 might already be considered troublesome. |
3. | The height of the peaks in this theoretical spectrum can be controlled by adjusting the autoregressive parameters. Here we chose to obtain a spectrum similar to the process . |
4. | The same simulation exercise has been done based on a seasonal adjustment method called CAMPLET (see Abeln and Jacobs 2015), which is not based on linear filters. Results show that MAR() with are selected in most of the cases. Causality and noncausality is mostly preserved, but not to the same extent as for the X-11. Results are available upon request. |
5. | Simulation results are available upon request. |
6. | In order to conserve space, we only report the models that were selected at least once for any . |
7. | Alternatively, modified () seasonal unit root tests, see e.g., Del Barrio Castro et al. (2017), could be used. It has been shown that these tests have good finite sample size and power properties. However, as we only apply the seasonal unit root test for illustrative purposes, we restrict ourselves to the original HEGY test. |
8. | The package MARX used in this study is freely available in the CRAN package repository. See Hecq et al. (2017) for instructions on how to use the package. |
9. | Since the Jarque-Bera test is based on the sample skewness and kurtosis, which might not exist for fat-tailed processes, we also performed the Kolmogorov-Smirnov and Anderson-Darling test to check for normality. These tests confirmed the reported results for the Jarque-Bera test. |
10. | The same investigation has been done using the TRAMO/SEATS seasonal adjustment method (see Maravall 1997) which is merely used by Eurostat. This method is based on unobserved components decomposition but is not free from filters. In particular, a truncated version of the two-sided, centered, symmetric Wiener-Kolmogorov filter is used to estimate the signal in an observed process (for more details, see e.g., Maravall 2006). As the results are very similar, we do not report them here. |
11. | We performed the one-step method on the raw and seasonally adjusted inflation rates. In many cases, the one- and two-step procedure select the same model. However, the one-step procedure is more sensitive to numerical inaccuracies in the optimization routine, as the number of different models to be estimated heavily increases even when p goes up from e.g., 4 to 8 (from 15 to 45 models). The model selected in the two-step approach is, however, often among the second or third best when ranked by the values of the information criteria. An advantage of the two-step approach is that p is bounded and numerical inaccuracies only play a role for all models estimated within this p. |
Lags/Leads | Lags/Leads | Lags/Leads | |||
---|---|---|---|---|---|
0 | 0.856 | 10 | 0.025 | 20 | |
1 | 0.051 | 11 | 0.012 | 21 | <0.001 |
2 | 0.041 | 12 | 22 | 0.002 | |
3 | 0.050 | 13 | 0.021 | 23 | <0.001 |
4 | 14 | 0.016 | 24 | <0.001 | |
5 | 0.055 | 15 | 25 | <0.001 | |
6 | 0.034 | 16 | 26 | <0.001 | |
7 | 0.029 | 17 | <0.001 | 27 | <0.001 |
8 | 18 | 0.008 | 28 | <0.001 | |
9 | 0.038 | 19 |
MAR(0,0) | 75.5 | 0.0 | 0.0 | 19.5 | 0.0 | 0.0 | 1.9 | 0.0 | 0.0 |
MAR(1,0) | 6.4 | 82.1 | 4.4 | 4.3 | 83.1 | 0.0 | 0.3 | 73.8 | 0.0 |
MAR(0,1) | 5.1 | 5.4 | 82.7 | 3.8 | 0.0 | 84.5 | 0.5 | 0.0 | 72.2 |
MAR(2,0) | 0.6 | 4.1 | 0.2 | 0.2 | 1.8 | 0.0 | 0.0 | 1.9 | 0.0 |
MAR(1,1) | 0.5 | 3.2 | 3.6 | 0.0 | 4.4 | 4.3 | 0.0 | 5.2 | 5.4 |
MAR(0,2) | 0.2 | 0.4 | 3.6 | 0.4 | 0.0 | 1.9 | 0.0 | 0.0 | 1.9 |
MAR(3,0) | 0.6 | 0.8 | 0.0 | 0.0 | 0.6 | 0.0 | 0.0 | 0.2 | 0.0 |
MAR(2,1) | 0.1 | 0.3 | 0.3 | 0.0 | 0.2 | 1.0 | 0.0 | 0.0 | 1.2 |
MAR(1,2) | 0.0 | 0.0 | 0.3 | 0.0 | 0.4 | 0.1 | 0.0 | 0.6 | 0.1 |
MAR(0,3) | 0.1 | 0.0 | 0.7 | 0.0 | 0.0 | 0.8 | 0.0 | 0.0 | 0.7 |
MAR(4,0) | 4.8 | 2.6 | 0.2 | 38.3 | 8.3 | 0.0 | 50.6 | 16.9 | 0.0 |
MAR(3,1) | 0.0 | 0.2 | 0.8 | 0.2 | 0.0 | 0.9 | 0.0 | 0.0 | 1.8 |
MAR(2,2) | 0.7 | 0.3 | 0.3 | 0.0 | 0.0 | 0.1 | 0.0 | 0.1 | 0.0 |
MAR(1,3) | 0.3 | 0.3 | 0.1 | 0.0 | 1.2 | 0.0 | 0.0 | 1.3 | 0.0 |
MAR(0,4) | 5.1 | 0.3 | 2.8 | 33.3 | 0.0 | 6.4 | 46.7 | 0.0 | 16.7 |
MAR(0,0) | 75.5 | 1.6 | 1.3 | 19.5 | 0.0 | 0.0 | 1.9 | 0.0 | 0.0 |
MAR(1,0) | 6.4 | 73.1 | 7.9 | 4.3 | 58.1 | 0.4 | 0.3 | 25.4 | 0.0 |
MAR(0,1) | 5.1 | 9.1 | 75.8 | 3.8 | 0.1 | 58.5 | 0.5 | 0.1 | 26.6 |
MAR(2,0) | 0.6 | 2.5 | 0.5 | 0.2 | 1.2 | 0.0 | 0.0 | 0.7 | 0.0 |
MAR(1,1) | 0.5 | 1.7 | 1.8 | 0.0 | 2.4 | 1.4 | 0.0 | 1.1 | 1.0 |
MAR(0,2) | 0.2 | 0.2 | 1.3 | 0.4 | 0.0 | 1.3 | 0.0 | 0.0 | 0.6 |
MAR(3,0) | 0.6 | 0.3 | 0.1 | 0.0 | 0.1 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(2,1) | 0.1 | 0.3 | 0.2 | 0.0 | 0.1 | 0.4 | 0.0 | 0.2 | 0.4 |
MAR(1,2) | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.2 | 0.0 |
MAR(0,3) | 0.1 | 0.0 | 0.4 | 0.0 | 0.0 | 0.1 | 0.0 | 0.0 | 0.0 |
MAR(4,0) | 4.8 | 7.6 | 1.9 | 38.3 | 36.2 | 0.6 | 50.6 | 71.2 | 0.2 |
MAR(3,1) | 0.0 | 0.1 | 0.4 | 0.2 | 0.0 | 0.7 | 0.0 | 0.0 | 0.5 |
MAR(2,2) | 0.7 | 0.6 | 1.1 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(1,3) | 0.3 | 0.4 | 0.0 | 0.0 | 0.9 | 0.0 | 0.0 | 0.9 | 0.1 |
MAR(0,4) | 5.1 | 2.5 | 7.3 | 33.3 | 0.7 | 36.4 | 46.7 | 0.2 | 70.6 |
MAR(0,0) | 92.9 | 0.0 | 0.0 | 93.9 | 0.0 | 0.0 | 96.6 | 0.0 | 0.0 |
MAR(1,0) | 2.5 | 89.2 | 2.9 | 2.7 | 95.8 | 0.0 | 1.3 | 96.4 | 0.0 |
MAR(0,1) | 3.2 | 3.2 | 90.3 | 2.9 | 0.0 | 96.4 | 1.9 | 0.0 | 97.3 |
MAR(2,0) | 0.3 | 3.6 | 0.1 | 0.2 | 2.1 | 0.0 | 0.1 | 1.5 | 0.0 |
MAR(1,1) | 0.4 | 2.4 | 2.4 | 0.2 | 1.8 | 1.8 | 0.0 | 1.5 | 0.7 |
MAR(0,2) | 0.2 | 0.3 | 2.7 | 0.1 | 0.0 | 1.6 | 0.1 | 0.0 | 1.8 |
MAR(3,0) | 0.1 | 0.5 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | 0.0 |
MAR(2,1) | 0.1 | 0.2 | 0.5 | 0.0 | 0.3 | 0.1 | 0.0 | 0.2 | 0.0 |
MAR(1,2) | 0.1 | 0.2 | 0.3 | 0.0 | 0.0 | 0.1 | 0.0 | 0.2 | 0.0 |
MAR(0,3) | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 |
MAR(4,0) | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(3,1) | 0.0 | 0.0 | 0.1 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(2,2) | 0.0 | 0.2 | 0.1 | 0.0 | 0.0 | 0.0 | 0.0 | 0.1 | 0.0 |
MAR(1,3) | 0.0 | 0.2 | 0.1 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(0,4) | 0.2 | 0.0 | 0.1 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(0,0) | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(1,0) | 9.6 | 2.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(0,1) | 18.2 | 0.4 | 1.9 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 |
MAR(2,0) | 2.4 | 61.7 | 2.8 | 0.0 | 24.5 | 0.0 | 0.0 | 5.0 | 0.0 |
MAR(1,1) | 57.2 | 5.0 | 5.0 | 92.3 | 0.0 | 0.0 | 90.6 | 0.0 | 0.0 |
MAR(0,2) | 4.7 | 2.2 | 62.0 | 0.0 | 0.0 | 26.9 | 0.0 | 0.0 | 6.5 |
MAR(3,0) | 0.6 | 2.3 | 0.2 | 0.0 | 0.2 | 0.0 | 0.0 | 0.1 | 0.0 |
MAR(2,1) | 1.7 | 2.8 | 0.4 | 3.8 | 1.5 | 0.0 | 5.3 | 0.6 | 0.0 |
MAR(1,2) | 2.0 | 0.7 | 2.5 | 2.1 | 0.0 | 1.5 | 3.5 | 0.0 | 0.8 |
MAR(0,3) | 0.9 | 0.1 | 2.6 | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 0.1 |
MAR(4,0) | 0.4 | 16.8 | 1.4 | 0.1 | 72.9 | 0.1 | 0.0 | 94.1 | 0.0 |
MAR(3,1) | 0.3 | 1.4 | 1.4 | 0.3 | 0.5 | 0.4 | 0.4 | 0.1 | 0.0 |
MAR(2,2) | 0.4 | 1.0 | 1.2 | 0.0 | 0.3 | 0.6 | 0.0 | 0.1 | 0.3 |
MAR(1,3) | 0.3 | 2.1 | 1.1 | 0.0 | 0.1 | 0.5 | 0.0 | 0.0 | 0.2 |
MAR(0,4) | 1.3 | 1.3 | 17.3 | 0.4 | 0.0 | 69.6 | 0.2 | 0.0 | 92.1 |
MAR(1,0) | 8.6 | 0.0 | 0.0 | MAR(4,2) | 1.1 | 0.5 | 0.0 |
MAR(0,1) | 11.6 | 0.0 | 0.0 | MAR(3,3) | 0.2 | 0.0 | 0.0 |
MAR(2,0) | 1.5 | 0.0 | 0.0 | MAR(2,4) | 1.0 | 0.3 | 0.0 |
MAR(1,1) | 36.2 | 12.2 | 0.4 | MAR(1,5) | 4.7 | 34.5 | 44.4 |
MAR(0,2) | 3.2 | 0.0 | 0.0 | MAR(0,6) | 1.1 | 0.2 | 0.0 |
MAR(3,0) | 0.2 | 0.0 | 0.0 | MAR(6,1) | 0.1 | 1.7 | 1.7 |
MAR(2,1) | 0.9 | 0.1 | 0.0 | MAR(5,2) | 0.4 | 1.8 | 1.8 |
MAR(1,2) | 3.8 | 0.7 | 0.0 | MAR(4,3) | 0.1 | 0.3 | 0.0 |
MAR(0,3) | 1.5 | 0.0 | 0.0 | MAR(3,4) | 0.1 | 0.1 | 0.0 |
MAR(4,0) | 0.4 | 0.0 | 0.0 | MAR(2,5) | 0.8 | 0.5 | 1.2 |
MAR(3,1) | 0.5 | 0.0 | 0.0 | MAR(1,6) | 1.5 | 4.4 | 3.5 |
MAR(2,2) | 0.4 | 0.0 | 0.0 | MAR(0,7) | 0.3 | 0.0 | 0.0 |
MAR(1,3) | 0.8 | 0.0 | 0.0 | MAR(8,0) | 0.1 | 0.0 | 0.0 |
MAR(0,4) | 0.8 | 0.0 | 0.0 | MAR(7,1) | 0.1 | 0.0 | 0.0 |
MAR(5,0) | 1.1 | 0.0 | 0.0 | MAR(6,2) | 0.1 | 0.0 | 0.0 |
MAR(4,1) | 3.8 | 6.6 | 1.6 | MAR(5,3) | 0.1 | 0.1 | 0.2 |
MAR(2,3) | 0.6 | 0.1 | 0.0 | MAR(4,4) | 0.4 | 0.0 | 0.0 |
MAR(1,4) | 5.5 | 3.2 | 1.0 | MAR(3,5) | 0.2 | 0.1 | 0.2 |
MAR(0,5) | 1.4 | 0.2 | 0.0 | MAR(2,6) | 0.2 | 0.0 | 0.0 |
MAR(6,0) | 0.1 | 0.0 | 0.0 | MAR(1,7) | 1.1 | 1.4 | 0.8 |
MAR(5,1) | 2.2 | 30.6 | 43.0 | MAR(0,8) | 1.2 | 0.4 | 0.2 |
Country | | | | Pseudo Model | Jarque-Bera: : Normality | ARCH-LM: : no-ARCH | MAR() |
---|---|---|---|---|---|---|---|
Canada | −0.91 | −6.39 * | 36.03 * | AR(4) | 9.99 * | 1.35 | MAR(0,4) |
France | −1.51 | −5.80 * | 50.62 * | AR(3) | 40.26 * | 20.42 * | MAR(3,0) |
Germany | −1.05 | −5.85 * | 27.47 * | AR(4) | 6.33 * | 1.77 | MAR(0,4) |
Italy | −0.86 | −9.91 * | 142.52 * | AR(3) | 292.63 * | 66.78 * | MAR(3,0) |
Japan | −1.29 | −3.66 * | 25.94 * | AR(4) | 121.72 * | 10.46 * | MAR(4,0) |
United Kingdom | −1.06 | −6.21 * | 43.70 * | AR(4) | 191.87 * | 17.06 * | MAR(1,3) |
United States | −0.86 | −6.60 * | 33.44 * | AR(4) | 816.86 * | 0.82 | MAR(2,2) |
c.v. (5%) | −3.49 | −2.91 | 6.57 | 5.99 | 3.00 |
Country | ADF-Statistic Unit Root | Pseudo Model | Jarque-Bera: : Normality | ARCH-LM: : no-ARCH | MAR() |
---|---|---|---|---|---|
Canada | AR(3) | 28.11 * | 2.39 | MAR(0,3) | |
France | AR(3) | 166.52 * | 14.21 * | MAR(3,0) | |
Germany | AR(3) | 51.33 * | 0.22 | MAR(0,3) | |
Italy | AR(6) | 754.96 * | 45.54 * | MAR(2,4) | |
Japan | AR(3) | 76.95 * | 23.30 * | MAR(3,0) | |
United Kingdom | AR(2) | 538.86 * | 13.05 * | MAR(0,2) | |
United States | AR(3) | 1320.34 * | 0.64 | MAR(0,3) | |
c.v. (5%) | 5.99 | 3.00 |
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Hecq, A.; Telg, S.; Lieb, L. Do Seasonal Adjustments Induce Noncausal Dynamics in Inflation Rates? Econometrics 2017, 5, 48. https://doi.org/10.3390/econometrics5040048
Hecq A, Telg S, Lieb L. Do Seasonal Adjustments Induce Noncausal Dynamics in Inflation Rates? Econometrics. 2017; 5(4):48. https://doi.org/10.3390/econometrics5040048
Chicago/Turabian StyleHecq, Alain, Sean Telg, and Lenard Lieb. 2017. "Do Seasonal Adjustments Induce Noncausal Dynamics in Inflation Rates?" Econometrics 5, no. 4: 48. https://doi.org/10.3390/econometrics5040048
APA StyleHecq, A., Telg, S., & Lieb, L. (2017). Do Seasonal Adjustments Induce Noncausal Dynamics in Inflation Rates? Econometrics, 5(4), 48. https://doi.org/10.3390/econometrics5040048