Social media as a data source for official statistics; the Dutch Consumer Confidence Index
Section 3. Structural time series modelling of the CCI and the SMI

In this section, univariate and bivariate structural time series models for the CCI and SMI are developed. With a structural time series model, a series is decomposed in a trend component, seasonal component, other cyclic components, regression component and an irregular component. For each component a stochastic model is assumed. This allows the trend, seasonal, and cyclic component but also the regression coefficients to be time dependent. If necessary autoregressive-moving-average (ARMA) components can be added to capture the autocorrelation in the series beyond these structural components. See Harvey (1989) or Durbin and Koopman (2012) for details about structural time series modelling.

The question addressed in this paper is to which extent the SMI follows a similar pattern as the CCI such that the SMI can be used in the estimation procedure of the CCI or, in the most extreme case, even can replace the CCI. This question is addressed by developing a bivariate structural time series model for the CCI and the SMI and modeling the correlation between the disturbance terms of the different components of the structural time series model for both series. The concept of cointegration is used to investigate to which extent the unobserved components of both series are driven by common factors. If e.g., the trends of both series are driven by one underlying common trend an argument can be made that the SMI represents similar evolution of sentiment feelings compared to the CCI. Alternatively, the SMI can be used as an auxiliary series in a model based estimation procedure for the CCI or in a nowcasting procedure to obtain more precise real time estimates.

3.1  Univariate model CCI series

As a first step, a univariate time series model for the CCI series is proposed. With the design-based approach described in Section 2.1, the sample information observed in each separate month is used to obtain an estimate for the CCI in that month. A drawback of this approach is that information observed in preceding periods is not used to obtain more accurate estimates for the CCI. In survey methodology, time series models are frequently applied to develop estimates for periodic surveys. Blight and Scott (1973) and Scott and Smith (1974) proposed to regard the unknown population parameters as a realization of a stochastic process that can be described with a time series model. This introduces relationships between the estimated population parameters at different time points in the case of non-overlapping as well as overlapping samples. The explicit modelling of this relationship between these survey estimates with a time series model can be used to combine sample information observed in the past to improve the precision of estimates obtained with periodic surveys. Some key references to authors that applied the time series approach to repeated survey data to improve the efficiency of survey estimates are Scott, Smith and Jones (1977), Tam (1987), Binder and Dick (1989, 1990), Bell and Hillmer (1990), Tiller (1992), Rao and Yu (1994), Pfeffermann and Burck (1990), Pfeffermann (1991), Pfeffermann and Rubin-Bleuer (1993), Pfeffermann, Feder and Signorelli (1998), Pfeffermann and Tiller (2006), Harvey and Chung (2000), Feder (2001), Lind (2005) and van den Brakel and Krieg (2009, 2015).

Developing a time series model for survey estimates observed with a periodic survey starts with a model, which states that the survey estimate can be decomposed in the value of the population variable and a sampling error:

I t = θ t + e t , ( 3.1 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGjbWdamaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabg2da9iab eI7aX9aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGHRaWkcaWGLb WdamaaBaaaleaapeGaamiDaaWdaeqaaOGaaiilaiaaywW7caaMf8Ua aGzbVlaaywW7caGGOaGaaG4maiaac6cacaaIXaGaaiykaaaa@4A12@

where θ t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH4oqCpaWaaSbaaSqaa8qacaWG0baapaqabaaaaa@3924@ denote the real CCI in month t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamiDaaaa@36F4@ under a complete enumeration of the target population and e t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGLbWdamaaBaaaleaapeGaamiDaaWdaeqaaaaa@3858@ the sampling error.

The CCI is observed at a monthly frequency. Therefore, as a first step, the series of the finite population parameter can be decomposed in a stochastic trend, seasonal component to model systematic deviations from the trend within a year, and a white noise component for the remaining unexplained variation. These considerations lead to the following model for the series of the finite population parameter:

θ t = L t + S t + ξ t , ( 3.2 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH4oqCpaWaaSbaaSqaa8qacaWG0baapaqabaGcpeGaeyypa0Ja amita8aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGHRaWkcaWGtb WdamaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabgUcaRiabe67a49aa daWgaaWcbaWdbiaadshaa8aabeaakiaacYcacaaMf8UaaGzbVlaayw W7caaMf8UaaiikaiaaiodacaGGUaGaaGOmaiaacMcaaaa@4E16@

where L t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGmbWdamaaBaaaleaapeGaamiDaaWdaeqaaaaa@383F@ denotes a stochastic trend, S t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGtbWdamaaBaaaleaapeGaamiDaaWdaeqaaaaa@3846@ a stochastic seasonal component and ξ t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH+oaEpaWaaSbaaSqaa8qacaWG0baapaqabaaaaa@3931@ the unexplained variation of the finite population parameter. Inserting (3.2) into measurement model (3.1) gives

I t = L t + S t + ξ t + e t . ( 3.3 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGjbWdamaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabg2da9iaa dYeapaWaaSbaaSqaa8qacaWG0baapaqabaGcpeGaey4kaSIaam4ua8 aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGHRaWkcqaH+oaEpaWa aSbaaSqaa8qacaWG0baapaqabaGcpeGaey4kaSIaamyza8aadaWgaa WcbaWdbiaadshaa8aabeaakiaac6cacaaMf8UaaGzbVlaaywW7caaM f8UaaiikaiaaiodacaGGUaGaaG4maiaacMcaaaa@506A@

In a cross-sectional survey it is difficult to separate the sampling error from the white noise of the population parameter. Therefore, both components are combined in one disturbance term

υ t = ξ t + e t . ( 3.4 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHfpqDpaWaaSbaaSqaa8qacaWG0baapaqabaGcpeGaeyypa0Ja eqOVdG3damaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabgUcaRiaadw gapaWaaSbaaSqaa8qacaWG0baapaqabaGccaGGUaGaaGzbVlaaywW7 caaMf8UaaGzbVlaacIcacaaIZaGaaiOlaiaaisdacaGGPaaaaa@4B1D@

It is assumed that E ( υ t ) = 0 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGfbWaaeWaaeaacqaHfpqDpaWaaSbaaSqaa8qacaWG0baapaqa baaak8qacaGLOaGaayzkaaGaeyypa0JaaGimaaaa@3D62@ and Var ( υ t ) = σ υ 2 . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaqGwbGaaeyyaiaabkhadaqadaqaaiabew8a19aadaWgaaWcbaWd biaadshaa8aabeaaaOWdbiaawIcacaGLPaaacqGH9aqpcqaHdpWCpa Waa0baaSqaa8qacqaHfpqDa8aabaWdbiaaikdaaaGcpaGaaiOlaaaa @440C@ To allow for nonhomogeneous variance in the sampling errors, Binder and Dick (1990) proposed a measurement error where the disturbance terms υ t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHfpqDpaWaaSbaaSqaa8qacaWG0baapaqabaaaaa@3935@ are proportional to the standard errors of I t , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGjbWdamaaBaaaleaapeGaamiDaaWdaeqaaOGaaiilaaaa@38F6@ i.e.,

υ t = Var ( I t ) υ ˜ t , ( 3.5 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHfpqDpaWaaSbaaSqaa8qacaWG0baapaqabaGcpeGaeyypa0Za aOaaa8aabaWdbiaabAfacaqGHbGaaeOCamaabmaapaqaa8qacaWGjb WdamaaBaaaleaapeGaamiDaaWdaeqaaaGcpeGaayjkaiaawMcaaaWc beaakiaaysW7cuaHfpqDgaaca8aadaWgaaWcbaWdbiaadshaa8aabe aakiaacYcacaaMf8UaaGzbVlaaywW7caaMf8UaaiikaiaaiodacaGG UaGaaGynaiaacMcaaaa@505C@

with E ( υ ˜ t ) = 0 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGfbWaaeWaaeaacuaHfpqDpaGbaGaadaWgaaWcbaWdbiaadsha a8aabeaaaOWdbiaawIcacaGLPaaacqGH9aqpcaaIWaGaaiilaaaa@3E21@ Var ( υ ˜ t ) = σ υ 2 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaqGwbGaaeyyaiaabkhadaqadaqaaiqbew8a19aagaacamaaBaaa leaapeGaamiDaaWdaeqaaaGcpeGaayjkaiaawMcaaiabg2da9iabeo 8aZ9aadaqhaaWcbaWdbiabew8a1bWdaeaapeGaaGOmaaaak8aacaGG Saaaaa@4419@ and where Var ( I t ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaqGwbGaaeyyaiaabkhadaqadaqaaiaadMeapaWaaSbaaSqaa8qa caWG0baapaqabaaak8qacaGLOaGaayzkaaaaaa@3C91@ is defined by (2.3) and is used as a priori information in the time series model. Such a model would be useful if the sampling error dominates the white noise in the population parameter. Initial analyses indicate that in this application the variance of the population white noise is substantial, invalidating (3.5) for this application. In addition, the variance of the sampling error in this application is constant over time. Therefore, it is decided to combine the sampling error with the population white noise and assume a constant variance over time. The question how to account for sampling variance is also an issue in seasonal adjustment variances (Pfeffermann and Sverchkov, 2014). Bell (2005) studied the contribution of the sampling variance in the variance of the estimation error of seasonally adjusted series and in the nonseasonal component. In the case of (rotating) panels, the sampling error can be separated from the population white noise. In cross-sectional repeated surveys, it is difficult to identify the separate components and therefore both terms are combined in one disturbance term that captures both the sampling variance and the unexplained variation of the population parameter.

An extensive model selection showed that a smooth trend model is the most appropriate model to capture the trend and the economic cycle in the CCI series. The smooth trend model is defined as (Durbin and Koopman, 2012):

L t = L t 1 + R t , MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGmbWdamaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabg2da9iaa dYeapaWaaSbaaSqaa8qacaWG0bGaeyOeI0IaaGymaaWdaeqaaOWdbi abgUcaRiaadkfapaWaaSbaaSqaa8qacaWG0baapaqabaGccaGGSaaa aa@410A@

R t = R t 1 + η t , E ( η t ) = 0 , ( 3.6 ) Cov ( η t , η t ) = { σ η 2 if t = t 0 if t t . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrViFD0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qafaqaaeGabaaabaGaamOuamaaBaaaleaacaWG0baabeaakiabg2da 9iaadkfadaWgaaWcbaGaamiDaiabgkHiTiaaigdaaeqaaOGaey4kaS Iaeq4TdG2aaSbaaSqaaiaadshaaeqaaOWdaiaacYcacaaMe8UaaGPa V=qacaqGfbWaaeWaaeaacqaH3oaAdaWgaaWcbaGaamiDaaqabaaaki aawIcacaGLPaaacqGH9aqpcaaIWaGaaiilaiaaywW7caaMf8UaaGzb VlaaywW7caaMf8UaaiikaiaaiodacaGGUaGaaGOnaiaacMcaaeaaca qGdbGaae4BaiaabAhadaqadaWdaeaapeGaeq4TdG2aaSbaaSqaaiaa dshaaeqaaOGaaiilaiabeE7aOnaaBaaaleaaceWG0bGbauaaaeqaaa GccaGLOaGaayzkaaGaeyypa0Zaaiqaa8aabaqbaeaabiGaaaqaa8qa cqaHdpWCpaWaa0baaSqaa8qacqaH3oaAa8aabaWdbiaaikdaaaaak8 aabaWdbiaabMgacaqGMbGaaGjbVlaaykW7caWG0bGaeyypa0JabmiD ayaafaaapaqaa8qacaaIWaaapaqaa8qacaqGPbGaaeOzaiaaysW7ca aMc8UaamiDaiabgcMi5kqadshagaqbaaaapaGaaiOlaaWdbiaawUha aaaaaaa@7C0C@

Adding a random component for the level in (3.6) improves the log-likelihood with five units but results in an overfit of the data in a sense that the smoothed signal almost exactly follows the observed series with a very small measurement error variance. A local level model (random level without a slope) improves the log-likelihood with three units but also intends to overfit the data.

The seasonal component is modelled with a trigonometric model, which is defined as (Durbin and Koopman, 2012):

S t = j = 1 6 γ j t , ( 3.7 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGtbWaaSbaaSqaaiaadshaaeqaaOGaeyypa0ZaaabCaeaacqaH ZoWzdaWgaaWcbaGaamOAaiaadshaaeqaaaqaaiaadQgacqGH9aqpca aIXaaabaGaaGOnaaqdcqGHris5aOGaaiilaiaaywW7caaMf8UaaGzb VlaaywW7caGGOaGaaG4maiaac6cacaaI3aGaaiykaaaa@4D04@

with

γ j t = γ j t 1 cos ( λ j ) + γ ˜ j t 1 sin ( λ j ) + ω j t , γ ˜ j t = γ j t 1 sin ( λ j ) + γ ˜ j t 1 cos ( λ j ) + ω ˜ j t . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqr=jpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qafaqaaeGacaaabaGaeq4SdC2aaSbaaSqaaiaadQgacaWG0baabeaa aOqaaiabg2da9iabeo7aNnaaBaaaleaacaWGQbGaamiDaiabgkHiTi aaigdaaeqaaOGaci4yaiaac+gacaGGZbWaaeWaa8aabaWdbiabeU7a S9aadaWgaaWcbaWdbiaadQgaa8aabeaaaOWdbiaawIcacaGLPaaacq GHRaWkcuaHZoWzpaGbaGaapeWaaSbaaSqaaiaadQgacaWG0bGaeyOe I0IaaGymaaqabaGcciGGZbGaaiyAaiaac6gadaqadaWdaeaapeGaeq 4UdW2damaaBaaaleaapeGaamOAaaWdaeqaaaGcpeGaayjkaiaawMca aiabgUcaRiabeM8a3naaBaaaleaacaWGQbGaamiDaaqabaGcpaGaai ilaaWdbeaacuaHZoWzpaGbaGaapeWaaSbaaSqaaiaadQgacaWG0baa beaaaOqaaiabg2da9iabgkHiTiabeo7aNnaaBaaaleaacaWGQbGaam iDaiabgkHiTiaaigdaaeqaaOGaci4CaiaacMgacaGGUbWaaeWaa8aa baWdbiabeU7aS9aadaWgaaWcbaWdbiaadQgaa8aabeaaaOWdbiaawI cacaGLPaaacqGHRaWkcuaHZoWzpaGbaGaapeWaaSbaaSqaaiaadQga caWG0bGaeyOeI0IaaGymaaqabaGcciGGJbGaai4Baiaacohadaqada WdaeaapeGaeq4UdW2damaaBaaaleaapeGaamOAaaWdaeqaaaGcpeGa ayjkaiaawMcaaiabgUcaRiqbeM8a39aagaaca8qadaWgaaWcbaGaam OAaiaadshaaeqaaOWdaiaac6caaaaaaa@8267@

Here λ j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH7oaBpaWaaSbaaSqaa8qacaWGQbaapaqabaaaaa@3918@ denotes the frequency of the different cycles in radians and is defined as

λ j = 2 π j 12 , for j = 1 , , 6. MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH7oaBpaWaaSbaaSqaa8qacaWGQbaapaqabaGcpeGaeyypa0Za aSaaa8aabaWdbiaaikdacqaHapaCcaWGQbaapaqaa8qacaaIXaGaaG OmaaaacaGGSaGaaGjbVlaaysW7caaMe8UaaeOzaiaab+gacaqGYbGa aGjbVlaaysW7caaMe8UaamOAaiabg2da9iaaigdacaGGSaGaeSOjGS KaaiilaiaaiAdacaGGUaaaaa@52D6@

For the disturbance terms, it is assumed that

E ( ω j t ) = 0 , E ( ω ˜ j t ) = 0 , Cov ( ω t , ω t ) = { σ ω 2 if t = t 0     if t t . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrViFD0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qafaqabeGabaaabaGaamyramaabmaapaqaa8qacqaHjpWDdaWgaaWc baGaamOAaiaadshaaeqaaaGccaGLOaGaayzkaaGaeyypa0JaaGimai aacYcacaaMe8UaaGjbVlaaysW7caWGfbWaaeWaa8aabaWdbiqbeM8a 39aagaaca8qadaWgaaWcbaGaamOAaiaadshaaeqaaaGccaGLOaGaay zkaaGaeyypa0JaaGimaiaacYcaaeaacaqGdbGaae4BaiaabAhadaqa daWdaeaapeGaeqyYdC3aaSbaaSqaaiaadshaaeqaaOGaaiilaiabeM 8a3naaBaaaleaaceWG0bWdayaafaaapeqabaaakiaawIcacaGLPaaa cqGH9aqpdaGabaWdaeaafaqabeGacaaabaWdbiabeo8aZ9aadaqhaa WcbaWdbiabeM8a3bWdaeaapeGaaGOmaaaaaOWdaeaapeGaaeyAaiaa bAgacaaMe8UaaGPaVlaadshacqGH9aqpceWG0bGbauaaa8aabaWdbi aaicdacaGGGcGaaiiOaaWdaeaapeGaaeyAaiaabAgacaaMe8UaaGPa VlaadshacqGHGjsUceWG0bGbauaaaaaacaGL7baacaGGUaaaaaaa@73E0@

For reasons of parsimony, the same variance structure is assumed with the same hyperparameter for ω ˜ j t . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacuaHjpWDpaGbaGaapeWaaSbaaSqaaiaadQgacaWG0baabeaak8aa caGGUaaaaa@3AF5@ Furthermore, it is assumed that ω t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHjpWDdaWgaaWcbaGaamiDaaqabaaaaa@390D@ and ω ˜ t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacuaHjpWDpaGbaGaapeWaaSbaaSqaaiaadshaaeqaaaaa@393B@ are uncorrelated.

After including the stochastic trend component (3.6) and seasonal component (3.7), no additional cycle components are required. The model selection procedure indicated that two level interventions are needed to model sudden jumps in the series. The first one is due to the financial crisis in September 2008, and the second one is due to the economic downturn in September of 2011. Finally, an outlier is required for September 2007. Adding these three components increases the log-likelihood with 15 units. These considerations lead to the following model for the observed CCI series

I t = L t + S t + β 07 δ t 07 + β 08 δ t 08 + β 11 δ t 11 + υ t , ( 3.8 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGjbWdamaaBaaaleaapeGaamiDaaWdaeqaaOWdbiabg2da9iaa dYeapaWaaSbaaSqaa8qacaWG0baapaqabaGcpeGaey4kaSIaam4ua8 aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGHRaWkcqaHYoGypaWa aWbaaSqabeaapeGaaGimaiaaiEdaaaGccqaH0oazpaWaa0baaSqaa8 qacaWG0baapaqaa8qacaaIWaGaaG4naaaakiabgUcaRiabek7aI9aa daahaaWcbeqaa8qacaaIWaGaaGioaaaakiabes7aK9aadaqhaaWcba Wdbiaadshaa8aabaWdbiaaicdacaaI4aaaaOGaey4kaSIaeqOSdi2d amaaCaaaleqabaWdbiaaigdacaaIXaaaaOGaeqiTdq2damaaDaaale aapeGaamiDaaWdaeaapeGaaGymaiaaigdaaaGccqGHRaWkcqaHfpqD paWaaSbaaSqaa8qacaWG0baapaqabaGccaGGSaGaaGzbVlaaywW7ca aMf8UaaGzbVlaacIcacaaIZaGaaiOlaiaaiIdacaGGPaaaaa@67D6@

with

δ t 07 = { 1 if t = 2007 ( 9 ) 0 if t 2007 ( 9 ) , δ t 08 = { 1 if t 2008 ( 9 ) 0 if t < 2008 ( 9 ) , δ t 11 = { 1 if t 2011 ( 9 ) 0 if t < 2011 ( 9 ) , MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrFjpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH0oazpaWaa0baaSqaa8qacaWG0baapaqaa8qacaaIWaGaaG4n aaaakiabg2da9maaceaapaqaauaabeqaciaaaeaacaaIXaaabaWdbi aabMgacaqGMbGaaGjbVlaaykW7caWG0bGaeyypa0JaaGOmaiaaicda caaIWaGaaG4naiaayIW7daqadaWdaeaapeGaaGyoaaGaayjkaiaawM caaaWdaeaacaaIWaaabaWdbiaabMgacaqGMbGaaGjbVlaaykW7caWG 0bGaeyiyIKRaaGOmaiaaicdacaaIWaGaaG4naiaayIW7daqadaWdae aapeGaaGyoaaGaayjkaiaawMcaaaaaaiaawUhaaiaacYcacaaMe8Ua aGjbVlaaysW7cqaH0oazpaWaa0baaSqaa8qacaWG0baapaqaa8qaca aIWaGaaGioaaaakiabg2da9maaceaapaqaauaabeqaciaaaeaacaaI XaaabaWdbiaabMgacaqGMbGaaGjbVlaaykW7caWG0bGaeyyzImRaaG OmaiaaicdacaaIWaGaaGioaiaayIW7daqadaWdaeaapeGaaGyoaaGa ayjkaiaawMcaaaWdaeaacaaIWaaabaWdbiaabMgacaqGMbGaaGjbVl aaykW7caWG0bGaeyipaWJaaGOmaiaaicdacaaIWaGaaGioaiaayIW7 daqadaWdaeaapeGaaGyoaaGaayjkaiaawMcaaaaapaGaaiilaaWdbi aawUhaaiaaysW7caaMe8UaaGjbVlabes7aK9aadaqhaaWcbaWdbiaa dshaa8aabaWdbiaaigdacaaIXaaaaOGaeyypa0Zaaiqaa8aabaqbae qabiGaaaqaaiaaigdaaeaapeGaaeyAaiaabAgacaaMe8UaaGPaVlaa dshacqGHLjYScaaIYaGaaGimaiaaigdacaaIXaGaaGjcVpaabmaapa qaa8qacaaI5aaacaGLOaGaayzkaaaapaqaaiaaicdaaeaapeGaaeyA aiaabAgacaaMe8UaaGPaVlaadshacqGH8aapcaaIYaGaaGimaiaaig dacaaIXaGaaGjcVpaabmaapaqaa8qacaaI5aaacaGLOaGaayzkaaaa aaGaay5EaaGaaiilaaaa@B03E@

and β x MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHYoGypaWaaWbaaSqabeaapeGaamiEaaaaaaa@3905@ the corresponding regression coefficients.

Finally, autoregressive (AR) and moving average (MA) components can be added to the structural time series model (3.8). In this application, there were no indications that such components are required, since there are no clear signs of remaining serial correlation in the standardized innovations. Adding an AR(1) or an MA(1) to (3.8) increases the log-likelihood with 5 and 4.5 units respectively. Adding second-order AR or MA models does not further improve the log-likelihood. Adding an ARMA(1,1) also does not further increases the log-likelihood. An AR(1) or MA(1) slightly improves the correlogram but also increases the standard error of the filtered smoothed signals. Therefore, model (3.8) was finally selected for the CCI series.

State space models assume that the disturbance terms are normally and independently distributed. These assumptions translate into the assumption that the innovations are normally and independently distributed. Table A.1 in the appendix contains an overview of goodness of fit statistics applied to the standardized innovations. The values for skewness, kurtosis and the Bowman-Shenton test do not indicate deviations from normality of the standardized innovations. The values for the Ljung-Box test and Durban-Watson test do not indicate serial correlations in the standardized innovations. This is also confirmed by a correlogram (not shown). In conclusion, these diagnostics indicate that (3.8) fits the series of the CCI reasonably well.

3.2  Bivariate model CCI and SMI series

The next step is to combine the univariate model for the CCI with the series for the SMI. Before combining CCI and SMI in a bivariate model, a univariate model for the SMI is developed with the purpose to better understand the behaviour of this series. A model selection procedure, similar to the one conducted for the CCI series in Subsection 3.1, indicated that the observed series for the SMI can be modelled with a smooth trend model and a white noise component for the unexplained variation. No significant seasonal component or business cycle is established. There are no signs for outliers or level shifts. AR(1) and MA(1) components are not included since there is no serial correlation in the standardized innovations. These considerations led to a bivariate model for the CCI and SMI where the CCI contains a trend and a seasonal component and the SMI a trend component.

Tables A.2 and A.3 in the appendix contain an overview of goodness of fit statistics for the standardized innovations of the CCI and SMI respectively. There are no indications that the standardized innovations of both series deviate from a normal distributions. The null hypothesis of no serial correlation in the standardized innovations could not be rejected. The correlogram of the innovations for the SMI, however, show a non-significant seasonal pattern (not shown). The innovations of the SMI, also contain heteroscedasticity.

The disturbance terms of the trend of both series are correlated. Since the series for the SMI is available from June 2010, the model for the CCI also contains the last intervention for September 2011, but not the outlier in September 2007 and the intervention in September 2008. As a result the following bivariate model is obtained:

( I t X t ) = ( L t I L t X ) + ( S t I 0 ) + ( β 11 δ t 11 0 ) + ( υ t I υ t X ) , ( 3.9 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qadaqadaWdaeaafaqabeGabaaabaWdbiaadMeadaWgaaWcbaGaamiD aaqabaaak8aabaWdbiaadIfapaWaaSbaaSqaa8qacaWG0baapaqaba aaaaGcpeGaayjkaiaawMcaaiabg2da9maabmaapaqaauaabeqaceaa aeaapeGaamita8aadaqhaaWcbaWdbiaadshaa8aabaWdbiaadMeaaa aak8aabaWdbiaadYeapaWaa0baaSqaa8qacaWG0baapaqaa8qacaWG ybaaaaaaaOGaayjkaiaawMcaaiabgUcaRmaabmaapaqaauaabeqace aaaeaapeGaam4ua8aadaqhaaWcbaWdbiaadshaa8aabaWdbiaadMea aaaak8aabaWdbiaaicdaaaaacaGLOaGaayzkaaGaey4kaSYaaeWaa8 aabaqbaeqabiqaaaqaa8qacqaHYoGypaWaaWbaaSqabeaapeGaaGym aiaaigdaaaGccqaH0oazpaWaa0baaSqaa8qacaWG0baapaqaa8qaca aIXaGaaGymaaaaaOWdaeaapeGaaGimaaaaaiaawIcacaGLPaaacqGH RaWkdaqadaWdaeaafaqabeGabaaabaWdbiabew8a19aadaqhaaWcba Wdbiaadshaa8aabaWdbiaadMeaaaaak8aabaWdbiabew8a19aadaqh aaWcbaWdbiaadshaa8aabaWdbiaadIfaaaaaaaGccaGLOaGaayzkaa GaaiilaiaaywW7caaMf8UaaGzbVlaaywW7caGGOaGaaG4maiaac6ca caaI5aGaaiykaaaa@6C61@

with L t I MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGmbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaamysaaaaaaa@391E@ and L t X MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGmbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaamiwaaaaaaa@392D@ the smooth trend model as defined in (3.6) with covariance structure

Cov ( η t I , η t I ) = { σ η I 2 if t = t 0 if t t , Cov ( η t X , η t X ) = { σ η X 2 if t = t 0 if t t , Cov ( η t I , η t X ) = { σ η I σ η X ρ η if t = t 0 if t t . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qafaqaaeWacaaabiqacahccaWLjaGaae4qaiaab+gacaqG2bWaaeWa a8aabaWdbiabeE7aO9aadaqhaaWcbaWdbiaadshaa8aabaWdbiaadM eaaaGcpaGaaGzaV=qacaGGSaGaeq4TdG2damaaDaaaleaapeGabmiD a8aagaqbaaqaa8qacaWGjbaaaaGccaGLOaGaayzkaaaabaGaeyypa0 Zaaiqaa8aabaqbaeaabiWaaaqaa8qacqaHdpWCpaWaa0baaSqaa8qa cqaH3oaAcaWGjbaapaqaa8qacaaIYaaaaaGcpaqaciaaOgVaGwWdbi aaxMaacaqGPbGaaeOzaaWdaeGabmWzb8qacaWG0bGaeyypa0JabmiD ayaafaaapaqaaiaaicdaaeGabiaOf8qacaWLjaGaaeyAaiaabAgaa8 aabiqad8vapeGaamiDaiabgcMi5kqadshagaqbaaaaaiaawUhaaiaa cYcaaeGabiaCiiaaxMaacaqGdbGaae4BaiaabAhadaqadaWdaeaape Gaeq4TdG2damaaDaaaleaapeGaamiDaaWdaeaapeGaamiwaaaak8aa caaMb8+dbiaacYcacqaH3oaApaWaa0baaSqaa8qaceWG0bWdayaafa aabaWdbiaadIfaaaaakiaawIcacaGLPaaaaeaacqGH9aqpdaGabaWd aeaafaqaaeGadaaabaWdbiabeo8aZ9aadaqhaaWcbaWdbiabeE7aOj aadIfaa8aabaWdbiaaikdaaaaak8aabiGaaGA8cGvbpeGaaCzcaiaa bMgacaqGMbaapaqaa8qacaWG0bGaeyypa0JabmiDayaafaaapaqaai aaicdaaeGacaaQXlawf8qacaWLjaGaaeyAaiaabAgaa8aabaWdbiaa dshacqGHGjsUceWG0bGbauaaaaaacaGL7baacaGGSaaabiqacahcca WLjaGaae4qaiaab+gacaqG2bWaaeWaa8aabaWdbiabeE7aO9aadaqh aaWcbaWdbiaadshaa8aabaWdbiaadMeaaaGcpaGaaGzaV=qacaGGSa Gaeq4TdG2damaaDaaaleaapeGabmiDa8aagaqbaaqaa8qacaWGybaa aaGccaGLOaGaayzkaaaabaGaeyypa0Zaaiqaa8aabaqbaeaabiWaaa qaa8qacqaHdpWCdaWgaaWcbaGaeq4TdGMaamysaaqabaGccqaHdpWC daWgaaWcbaGaeq4TdGMaamiwaaqabaGccqaHbpGCdaWgaaWcbaGaeq 4TdGgabeaaaOWdaeGacaaQXla0b8qacaWLjaGaaeyAaiaabAgaa8aa baWdbiaadshacqGH9aqpceWG0bGbauaaa8aabaGaaGimaaqaciaaOg VaqhWdbiaaxMaacaqGPbGaaeOzaaWdaeaapeGaamiDaiabgcMi5kqa dshagaqbaaaaaiaawUhaaiaac6caaaaaaa@B948@

In the last expression ρ η MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHbpGCdaWgaaWcbaGaeq4TdGgabeaaaaa@39B3@ denotes the correlation between the slope disturbances of the CCI and SMI. Furthermore, S t I MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGtbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaamysaaaaaaa@3925@ is the seasonal effect defined by (3.7) and δ t 11 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH0oazpaWaa0baaSqaa8qacaWG0baapaqaa8qacaaIXaGaaGym aaaaaaa@3A9A@ the intervention for September 2011 with β 11 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHYoGypaWaaWbaaSqabeaapeGaaGymaiaaigdaaaaaaa@397E@ the corresponding regression coefficient. Finally, υ t I MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHfpqDpaWaa0baaSqaa8qacaWG0baapaqaa8qacaWGjbaaaaaa @3A14@ and υ t X MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHfpqDpaWaa0baaSqaa8qacaWG0baapaqaa8qacaWGybaaaaaa @3A23@ are the disturbance terms for the CCI and SMI series and are defined as:

E ( υ t I ) = E ( υ t X ) = 0 , Cov ( υ t I , υ t I ) = { σ υ I 2     if t = t 0           if t t , Cov ( υ t X , υ t X ) = { σ υ X 2 if t = t 0         if t t , Cov ( υ t I , υ t X ) = 0 for all t and t . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qafaqaaeabcaaaaeGabiaCiiaaxMaacaWGfbGaaiikaiabew8a19aa daqhaaWcbaWdbiaadshaa8aabaWdbiaadMeaaaGccaGGPaaabaGaey ypa0JaamyraiaacIcacqaHfpqDpaWaa0baaSqaa8qacaWG0baapaqa a8qacaWGybaaaOGaaiykaiabg2da9iaaicdacaGGSaaabiqacahcca WLjaGaae4qaiaab+gacaqG2bWaaeWaa8aabaWdbiabew8a19aadaqh aaWcbaWdbiaadshaa8aabaWdbiaadMeaaaGcpaGaaGzaV=qacaGGSa GaeqyXdu3damaaDaaaleaapeGabmiDa8aagaqbaaqaa8qacaWGjbaa aaGccaGLOaGaayzkaaaabaGaeyypa0Zaaiqaa8aabaqbaeqabiqaaa qaauaabeqabmaaaeaapeGaeq4Wdm3damaaDaaaleaapeGaeqyXduNa amysaaWdaeaapeGaaGOmaaaakiaacckacaGGGcaapaqaceaaicWdbi aaxMaacaqGPbGaaeOzaaWdaeaapeGaamiDaiabg2da9iqadshagaqb aaaaa8aabaqbaeqabeWaaaqaa8qacaaIWaGaaiiOaiaacckacaGGGc GaaiiOaiaacckaa8aabiqaaWkapeGaaCzcaiaabMgacaqGMbaapaqa a8qacaWG0bGaeyiyIKRabmiDayaafaaaaaaaaiaawUhaaiaacYcaae GabiaCiiaaxMaacaqGdbGaae4BaiaabAhadaqadaWdaeaapeGaeqyX du3damaaDaaaleaapeGaamiDaaWdaeaapeGaamiwaaaak8aacaaMb8 +dbiaacYcacqaHfpqDpaWaa0baaSqaa8qaceWG0bWdayaafaaabaWd biaadIfaaaaakiaawIcacaGLPaaaaeaacqGH9aqpdaGabaWdaeaafa qabeGabaaabaqbaeqabeWaaaqaa8qacqaHdpWCpaWaa0baaSqaa8qa cqaHfpqDcaWGybaapaqaa8qacaaIYaaaaaGcpaqaceaaudWdbiaaxM aacaqGPbGaaeOzaaWdaeaapeGaamiDaiabg2da9iqadshagaqbaaaa a8aabaqbaeqabeWaaaqaa8qacaaIWaGaaiiOaiaacckacaGGGcGaai iOaaWdaeGabaqcb8qacaWLjaGaaeyAaiaabAgaa8aabaWdbiaadsha cqGHGjsUceWG0bGbauaaaaaaaaGaay5EaaGaaiilaaqaceGaWHGaaC zcaiaaboeacaqGVbGaaeODamaabmaapaqaa8qacqaHfpqDpaWaa0ba aSqaa8qacaWG0baapaqaa8qacaWGjbaaaOWdaiaaygW7peGaaiilai abew8a19aadaqhaaWcbaWdbiqadshapaGbauaaaeaapeGaamiwaaaa aOGaayjkaiaawMcaaaqaaiabg2da9iaaicdacaaMe8UaaeOzaiaab+ gacaqGYbGaaGjbVlaabggacaqGSbGaaeiBaiaaysW7caWG0bGaaGjb VlaabggacaqGUbGaaeizaiaaysW7ceWG0bGbauaacaGGUaaaaaaa@C58B@

If the model detects a strong correlation between the trends of the CCI and the SMI, then the trends of both series will develop into the same direction more or less simultaneously. In this case, the additional information from the SMI series will result in an increased precision of the estimates of the CCI figures. In the case of strong correlation between the disturbances of the trends, i.e., if ρ η 1 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHbpGCdaWgaaWcbaGaeq4TdGgabeaakiabgkziUkaaigdacaGG Saaaaa@3D15@ the trends are said to be cointegrated. In that case, there is one underlying common trend that drives the evolution of the trends of the two observed series. To see this, it is noted that the covariance matrix of the slope disturbances is implemented as a singular value decomposition:

cov ( η t I η t X ) = ( σ η I 2 σ η I σ η X ρ η σ η I σ η X ρ η σ η X 2 ) = ( 1 0 a 1 ) ( d 1 0 0 d 2 ) ( 1 a 0 1 ) . ( 3.10 ) MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaqGJbGaae4BaiaabAhadaqadaWdaeaafaqabeGabaaabaWdbiab eE7aO9aadaqhaaWcbaWdbiaadshaa8aabaWdbiaadMeaaaaak8aaba WdbiabeE7aO9aadaqhaaWcbaWdbiaadshaa8aabaWdbiaadIfaaaaa aaGccaGLOaGaayzkaaGaeyypa0ZaaeWaa8aabaqbaeqabiGaaaqaa8 qacqaHdpWCpaWaa0baaSqaa8qacqaH3oaAcaWGjbaapaqaa8qacaaI YaaaaaGcpaqaa8qacqaHdpWCdaWgaaWcbaGaeq4TdGMaamysaaqaba GccqaHdpWCdaWgaaWcbaGaeq4TdGMaamiwaaqabaGccqaHbpGCdaWg aaWcbaGaeq4TdGgabeaaaOWdaeaapeGaeq4Wdm3aaSbaaSqaaiabeE 7aOjaadMeaaeqaaOGaeq4Wdm3aaSbaaSqaaiabeE7aOjaadIfaaeqa aOGaeqyWdi3aaSbaaSqaaiabeE7aObqabaaak8aabaWdbiabeo8aZ9 aadaqhaaWcbaWdbiabeE7aOjaadIfaa8aabaWdbiaaikdaaaaaaaGc caGLOaGaayzkaaGaeyypa0ZaaeWaa8aabaqbaeqabiGaaaqaa8qaca aIXaaapaqaa8qacaaIWaaapaqaa8qacaWGHbaapaqaa8qacaaIXaaa aaGaayjkaiaawMcaamaabmaapaqaauaabeqaciaaaeaapeGaamiza8 aadaWgaaWcbaWdbiaaigdaa8aabeaaaOqaa8qacaaIWaaapaqaa8qa caaIWaaapaqaa8qacaWGKbWdamaaBaaaleaapeGaaGOmaaWdaeqaaa aaaOWdbiaawIcacaGLPaaadaqadaWdaeaafaqabeGacaaabaWdbiaa igdaa8aabaWdbiaadggaa8aabaWdbiaaicdaa8aabaWdbiaaigdaaa aacaGLOaGaayzkaaGaaiOlaiaaywW7caaMf8UaaGzbVlaaywW7caGG OaGaaG4maiaac6cacaaIXaGaaGimaiaacMcaaaa@87F0@

Instead of estimating σ η I 2 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHdpWCpaWaa0baaSqaa8qacqaH3oaAcaWGjbaapaqaa8qacaaI YaaaaOWdaiaacYcaaaa@3C48@ σ η X 2 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHdpWCpaWaa0baaSqaa8qacqaH3oaAcaWGybaapaqaa8qacaaI YaaaaOWdaiaacYcaaaa@3C57@ and ρ η , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHbpGCdaWgaaWcbaGaeq4TdGgabeaak8aacaGGSaaaaa@3A7C@ parameters d 1 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGKbWdamaaBaaaleaapeGaaGymaaWdaeqaaOGaaiilaaaa@38D3@ d 2 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGKbWdamaaBaaaleaapeGaaGOmaaWdaeqaaOGaaiilaaaa@38D4@ and a MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGHbaaaa@3701@ are estimated. If d 2 0 , MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGKbWdamaaBaaaleaapeGaaGOmaaWdaeqaaOWdbiabgkziUkaa icdacaGGSaaaaa@3B8B@ it follows that ρ η 1. MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaHbpGCdaWgaaWcbaGaeq4TdGgabeaakiabgkziUkaaigdacaGG Uaaaaa@3D17@ In that case, the covariance matrix of the slope disturbances is of reduced rank and both trends are driven by one common trend. This implies that the slope disturbances of both series simultaneously move up or down and that the slope disturbances of the SMI can be perfectly predicted from slope disturbances of the CCI by η t X = a η t I . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacqaH3oaApaWaa0baaSqaa8qacaWG0baapaqaa8qacaWGybaaaOGa eyypa0JaamyyaiabeE7aO9aadaqhaaWcbaWdbiaadshaa8aabaWdbi aadMeaaaGcpaGaaiOlaaaa@40A7@ Furthermore, the slope for the SMI series can be expressed as a linear combination of the slope for the CCI series as R t X = a R t I + R ¯ . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGsbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaamiwaaaakiab g2da9iaadggacaWGsbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaam ysaaaakiabgUcaRiqadkfapaGbaebapeGaaiOlaaaa@40DE@ Similarly, the trend for the SMI series can be expressed as a linear combination of the trend for the CCI series as L t X = a L t I + L ¯ + R ¯ t . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGmbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaamiwaaaakiab g2da9iaadggacaWGmbWdamaaDaaaleaapeGaamiDaaWdaeaapeGaam ysaaaakiabgUcaRiqadYeapaGbaebapeGaey4kaSIabmOua8aagaqe a8qacaWG0bGaaiOlaaaa@43B5@ Note that R ¯ MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGsbWdayaaraaaaa@3719@ and L ¯ MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGmbWdayaaraaaaa@3713@ are constants that are derived from the estimated states at the last two time periods of the series.

Cointegration increases the precision of the estimated trend and signal of the CCI series, allows for formulating more parsimonious models, but could also be seen as an argument to replace the CCI series by the SMI series since both series are driven by and represent the same common trend. For a more detailed discussion about cointegration in the context of state space modelling, see Koopman, Harvey, Shephard and Doornik (2009, Sections 6.4 and 9.1).

3.3  Estimation of structural time series models

The general way to analyse a structural time series model is to express it in the so-called state space representation and apply the Kalman filter to obtain optimal estimates for the state variables, see e.g., Durbin and Koopman (2012). The software for the analysis and estimation of the time series models is developed in Ox in combination with the subroutines of SsfPack 3.0, see Doornik (2009) and Koopman, Shephard and Doornik (2008).

All state variables are non-stationary and initialised with a diffuse prior, i.e., the expectation of the initial states are equal to zero and the initial covariance matrix of the states is diagonal with large diagonal elements. In Ssfpack 3.0, an exact diffuse log-likelihood function is obtained with the procedure proposed by Koopman (1997). Maximum likelihood (ML) estimates for the hyperparameters, i.e., the variance components of the stochastic processes for the state variables are obtained using a numerical optimization procedure (Broyden-Fletcher-Goldfarb-Shanno (BFGS) algorithm, Doornik, 2009). To avoid negative variance estimates, the log-transformed variances are estimated. More technical details about the analysis of state space models can be found in Harvey (1989) or Durbin and Koopman (2012).

Under the assumption of normally distributed disturbance terms, the Kalman filter can be applied to obtain optimal estimates for the state variables, see e.g., Durbin and Koopman (2012). The Kalman filter assumes that the variance and covariance terms are known in advance and are often referred to as hyperparameters. In practise, these hyperparameters are not known and are therefore substituted with their ML estimates. Estimates for state variables for period t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamiDaaaa@36F4@ based on the information available up to and including period t MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiFu0Je9sqqrpepC0xbbL8F4rqqrpgpC0xe9LqFf0xc9 qqpeuf0xe9q8qiYRWFGCk9vi=dbvc9G8Wq0db9qqpm0dXdIqpu0=vr 0=vr0=fdbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamiDaaaa@36F4@ are referred to as the filtered estimates. They are obtained with the Kalman filter where the ML estimates for the hyperparameters are based on the complete time series. The filtered estimates of past state vectors can be updated, if new data become available. This procedure is referred to as smoothing and results in smoothed estimates that are based on the complete time series.

Standard errors of the Kalman filter estimates do not reflect the additional uncertainty of using the ML estimates for the unknown hyperparameters. Therefore, the estimates of the standard errors are too optimistic.


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