Statistical Methods Reference Documents
Trend-cycle estimation: Concepts, interpretation, and calculation, 2026

Release date: June 8, 2026

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Statistics Canada releases graphical information on trend-cycle movements for several monthly economic indicators. Estimates of the trend-cycle are presented along with the seasonally adjusted data in selected charts in The Daily. The inclusion of trend-cycle information is intended to support the analysis and interpretation of the seasonally adjusted data.

This reference document provides information on trend-cycle data. It outlines basic concepts and definitions and discusses selected issues related to the use and interpretation of trend-cycle estimates. The document includes a specific example using data on monthly retail sales. Detailed information on the computation of the trend-cycle is also provided.

1 Defining trend-cycle

Trend-cycle data represent a smoothed version of a seasonally adjusted time series, providing information on longer-term movements, including changes in direction underlying the series.

The trend-cycle is the combination of two distinct components:

  • The trend provides information on longer-term movements in the seasonally adjusted data series over several years.
  • The cycle is a sequence of smoother fluctuations around the longer-term trend in part characterized by alternating periods of expansion and contraction.

Changes in trend-cycle data reflect the influence of factors that condition long-run movements in the economic indicator over time, along with fluctuations in economic activity associated with the business cycle. These two components, the trend and the cycle, are often paired together because of the difficulty involved in estimating them individually.

2 Trend-cycle versus seasonally adjusted data

seasonally adjusted data series is a series that has been modified to eliminate the effect of seasonal and calendar influences in order to facilitate comparisons of underlying conditions from period to period. Seasonally adjusted data series can also be defined as the combination of the trend-cycle and the irregular component of a time series.

In much the same way as a seasonally adjusted series represents the raw series with seasonal and calendar effects removed, the trend-cycle estimates represent the seasonally adjusted series with the irregular component removed. As its name suggests, the irregular component is the part of the time series that is not in line with the usual or expected pattern of the series. This irregular component is not part of the trend-cycle, nor is it related to current seasonal factors or calendar effects.

The irregular component of a time series can represent unanticipated economic events or shocks (for example, strikes, disruptions, natural disasters, unseasonable weather, etc.) or can simply arise from noise in the measurement of the unadjusted data. In some cases, this irregular component can make large contributions to the period-to-period movements in a seasonally adjusted time series.

By removing this irregular component from seasonally adjusted data, the trend-cycle data can yield a better picture of longer-term movements in the time series. In this sense, the trend-cycle can be interpreted as a smoothed version of the seasonally adjusted series.

3 Analytical value of trend-cycles

Trend-cycle data provide information on longer-term movements in a seasonally adjusted time series, including changes in the direction of the dataThese smoothed data make it easier to identify periods of positive change (growth) or negative change (decline) in the time series, as the noise of the irregular component has been removed. This allows for a more accurate identification of turning points in the data.

For example, the accompanying graph presents data on monthly retail sales in Canada from January 2021 to January 2026. Two data lines are shown: the seasonally adjusted time series and the trend-cycle estimates. The trend-cycle estimates for the most recent reference months are more subject to revision than the estimates for previous periods, and are presented as a dotted line.

While the seasonally adjusted data can be used to examine basic changes in the direction of the time series, it is easier to see the longer-term movement in these data from the trend-cycle line. The trend-cycle estimates show that retail sales trended upward at a relatively constant rate from early 2021 to mid-2022 and then expanded at a slower pace until mid-2024. Spending accelerated during the second half of 2024 before moderating in 2025. Estimates for the most recent months are based on a preliminary estimation of the trend-cycle and should be interpreted with caution as they are subject to revision as noted above.

Chart 1: Retail sales

Data table for chart 1
Data table for Chart 1
Table summary
This table displays the results of Data table for Chart 1 Seasonally adjusted and Trend-cycle , calculated using billions of dollars units of measure (appearing as column headers).
  Seasonally adjusted Trend-cycle
billions of dollars
Note: The higher variability associated with the trend-cycle estimates is indicated with a dotted line on the chart for the current reference month and the previous three months.
Sources: Statistics Canada tables 20-10-0056-01 and 20-10-0067-01 extracted on April 16, 2026; and trend-cycle computations.
2021  
January 55.154 57.834
February 58.779 58.180
March 61.769 58.524
April 58.398 58.792
May 56.947 59.061
June 59.653 59.576
July 60.146 60.061
August 61.110 60.470
September 60.843 60.947
October 61.645 61.539
November 62.429 61.943
December 61.334 62.260
2022  
January 62.883 62.825
February 63.403 63.421
March 64.105 64.087
April 64.090 64.658
May 65.844 65.139
June 66.821 65.458
July 64.895 65.431
August 65.164 65.360
September 64.851 65.297
October 65.401 65.272
November 65.413 65.265
December 64.679 65.348
2023  
January 66.269 65.509
February 65.669 65.576
March 65.348 65.622
April 65.631 65.655
May 65.660 65.756
June 65.996 65.877
July 65.887 65.991
August 65.934 66.162
September 66.582 66.302
October 66.510 66.360
November 66.558 66.391
December 66.325 66.372
2024  
January 66.085 66.307
February 66.244 66.260
March 66.158 66.226
April 66.779 66.242
May 65.963 66.306
June 65.893 66.440
July 66.888 66.721
August 67.100 67.142
September 67.513 67.603
October 68.041 68.115
November 68.299 68.679
December 70.027 69.109
2025  
January 69.652 69.398
February 69.189 69.585
March 69.797 69.674
April 70.015 69.752
May 69.158 69.736
June 70.139 69.751
July 69.532 69.781
August 70.279 69.845
September 69.698 69.864
October 69.468 69.924
November 70.241 70.024
December 69.930 70.098
2026  
January 70.709 70.235

Trend-cycle data are particularly useful when the irregular component makes large contributions to the month-to-month movements in a seasonally adjusted time series. In these cases, graphical information on the trend-cycle helps to interpret the movements in the seasonally adjusted series.

4 Data revisions and use

4.1 Necessity of data revisions

Existing estimates of the trend-cycle are revised with each release of new seasonally adjusted data. As new seasonally adjusted data becomes available, the trend-cycle data for previous months can be better estimated. If the trend-cycle data were not revised along with the seasonally adjusted series, the resulting trend-cycle data could contain series breaks, and would likely be inconsistent with the seasonally adjusted series in terms of levels, period-to-period movements, or both. It is necessary to revise the trend-cycle data to maintain their analytical value.

4.2 Interpreting preliminary estimates (dotted line)

The trend-cycle line that is published graphically is dotted in the most recent reference periods, as these periods are more likely to be subject to revisions. This is done to signal that the trend-cycle data in this period is a preliminary estimate, and subject to change as new data becomes available. New data make it possible to more accurately estimate the various components that make up the time series. These revisions can change the location of economic turning points, as well as reverse movements between individual months. These types of revisions are more likely to occur in the most recent reference periods.

4.3 Trend-cycle is not a forecast

The trend-cycle should not be viewed as a way to forecast the underlying seasonally adjusted data. These estimates are based solely on the historical values of the seasonally adjusted series and do not take into account any other information that could be used to project data for future reference periods. Furthermore, since the trend-cycle is subject to revision when additional reference periods are added to the series, the shape of the trend-cycle in the most recent reference periods should be viewed as a preliminary estimate.

5 Estimation methodology

5.1 Available estimation methods

There is no unique method that is recommended to estimate the trend-cycle that underlies a time series. A variety of methods have been developed in the literature, ranging from very simple to highly complex. Some methods introduce restrictions on the shape of the trend (for example a linear trend of several years), others are based on explicit models that estimate a trend-cycle component, and others, still, are based on variations of moving averages, where the mean of the data is calculated from successive sub spans or intervals of the data.

Since the trend-cycle can also be interpreted as a smoothed version of the seasonally adjusted series, a straightforward way of estimating the trend-cycle is by averaging the last three or six months of the data. While this may yield additional insight into the long-term movement in the series, some measure of caution is warranted as this approach does not take the place of more formal trend-cycle estimation techniques. It can be shown that indicators of the economic cycle derived from this simplified method tend to shift in time and may be artificially dampened.

5.2 Statistics Canada’s approach

Statistics Canada uses a weighted moving average of the data to compute the trend-cycle. This method is based on the Cascade Linear Filter of Dagum and Luati (2008). This weighted average is computed using the previous six months, the current month and (for older estimates) up to six of the subsequent months in the series. In real time, for the most recent reference month in the series, only data for the six previous months and current month are used, as data for subsequent months are not yet known. As these data become available, the trend-cycle estimates will be revised.

This specific weighted moving average method was selected after an empirical analysis of different alternatives. The estimate of the trend-cycle obtained with the selected method exhibits good statistical properties, as it provides smooth results with limited revisions, and has a low incidence of falsely identifying turning points. As well, it is a linear process and will preserve additive relationships in the data. This implies, for example, that the trend-cycle plotted on employment for men and women separately will sum up to the plotted trend-cycle line for both sexes. The method is easy to replicate as the weights used in the calculation of the weighted average are available.

5.3 Technical calculation details

The trend-cycle is estimated by applying moving averages weighted according to the cascade linear filter to the seasonally adjusted series. In general, the moving average used to calculate the trend-cycle for a specific reference month is a weighted average of up to 13 consecutive months, which are centered on the reference month, where possible.

For more information on the calculation of trend-cycle estimates, please consult this document’s appendix.

Appendix A: Details on the calculation of trend-cycle estimates at Statistics Canada

This appendix details the way Statistics Canada calculates trend-cycle estimates. It is intended as a technical description to support users who wish to apply trend-cycle estimation to monthly series available on the Statistics Canada website. General formulas outlining the mathematical calculations are presented below, and the derivation and application of the moving average weights are provided. For more information on the use of trend-cycle estimates in analysis, please refer to the previous part of this document.

The trend-cycle estimation method used at Statistics Canada applies moving averages and does not remove seasonal patterns. This procedure is intended for monthly series with at least 13 data points that do not exhibit seasonal patterns (either because no seasonality exists, or because it has been removed by seasonal adjustment).

A.1 The general formula

For each month  t MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWG0baaaa@3712@ , the following formula is applied to estimate the trend-cycle, denoted as  T C t MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVCI8FfYJH8YrFfeuY=Hhbbf9v8qqaqFr0xc9pk0xbb a9q8WqFfeaY=biLkVcLq=JHqpepeea0=as0Fb9pgeaYRXxe9vr0=vr 0=vqpWqaaeaabiGaciaacaqabeaadaqaaqaaaOqaaabaaaaaaaaape GaamivaiaadoeapaWaaSbaaSqaa8qacaWG0baapaqabaaaaa@3903@ :

Formula 1

TCt=j=t6t+6IjWj(t)Yjk=t6t+6IkWk(t),      (1)MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGubGaam4qa8aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGH 9aqpdaWcaaWdaeaapeWaaubmaeqal8aabaWdbiaadQgacqGH9aqpca WG0bGaeyOeI0IaaGOnaaWdaeaapeGaamiDaiabgUcaRiaaiAdaa0Wd aeaapeGaeyyeIuoaaOGaamysa8aadaWgaaWcbaWdbiaadQgaa8aabe aak8qacaWGxbWdamaaDaaaleaapeGaamOAaaWdaeaapeWaaeWaa8aa baWdbiaadshaaiaawIcacaGLPaaaaaGccaWGzbWdamaaBaaaleaape GaamOAaaWdaeqaaaGcbaWdbmaavadabeWcpaqaa8qacaWGQbGaeyyp a0JaamiDaiabgkHiTiaaiAdaa8aabaWdbiaadshacqGHRaWkcaaI2a aan8aabaWdbiabggHiLdaakiaadMeapaWaaSbaaSqaa8qacaWGQbaa paqabaGcpeGaam4va8aadaqhaaWcbaWdbiaadQgaa8aabaWdbmaabm aapaqaa8qacaWG0baacaGLOaGaayzkaaaaaaaakiaacYcacaWLjaGa aCzcaiaacIcacaaIXaGaaiykaaaa@6212@

where Y j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@ is the value of the input series for month j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbaaaa@3706@ , available for j = 1 , , T MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbGaeyypa0JaaGymaiaacYcacqGHMacVcaGGSaGaamivaaaa @3C8E@ . If the value of the input series for month j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbaaaa@3706@ is available, I j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGjbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@382E@ is an indicator equal to 1. Otherwise, it is equal to 0. Applying this formula near the beginning or end of a series leads to undefined terms (e.g. Y 0 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaaGimaaWdaeqaaaaa@3809@ ), discussed in Section A.2. The quantities shown as W j ( t ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGxbWdamaaDaaaleaapeGaamOAaaWdaeaapeWaaeWaa8aabaWd biaadshaaiaawIcacaGLPaaaaaaaaa@3AEE@ represent the moving average weights applied to month j   MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbGaaiiOaaaa@382A@ for the calculation of the trend-cycle for month t MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWG0baaaa@3712@ . This is referred to as the cascade linear filter, as derived by Dagum and Luati (2008) and presented in Table 1.

Table 1  Full-precision moving average weights for calculating the trend-cycle for month t
Months Weights
t-6 and t+6 -0.027
t-5 and t+5 -0.007
t-4 and t+4 0.031
t-3 and t+3 0.067
t-2 and t+2 0.136
t-1 and t+1 0.188
t 0.224

Applying formula (1) for each month t=1,,TMathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWG0bGaeyypa0JaaGymaiaacYcacqGHMacVcaGGSaGaamivaaaa @3C98@  yields the trend-cycle series.

A.2 Applying the general formula

The weights presented in Table 1 were developed by combining several filters that are each optimal for specific purposes. The combined results provide robust trend-cycle estimates with good statistical properties. For more information, see Dagum and Luati (2008).

By design, aggregating the weights in Table 1 for all months from  (t6) MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaaiikaiaads hacqGHsislcaaI2aGaaiykaaaa@39F9@ to (t+6) MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaaiikaiaads hacqGHRaWkcaaI2aGaaiykaaaa@39EE@ gives an exact total of 1. This is necessary so that the level of the trend-cycle series is the same on average as the level of the input series. Note that when we derive the trend-cycle estimates for the first six and the last six months of the input series, formula (1) includes terms that are not defined, such as  Y 0 MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamywamaaBa aaleaacaaIWaaabeaaaaa@37BE@  However, these terms can be assumed to be 0 since they disappear when multiplied by the corresponding indicator coefficient,  I 0 MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamysamaaBa aaleaacaaIWaaabeaaaaa@37AE@  which equals 0 by definition. In these cases, the denominator in formula (1) represents an adjustment to the moving average weights. Referred to as the cut-and-normalize approach, this ensures that the moving average weights used to estimate the trend-cycle for each month add up to 1. In the cut-and-normalize approach, the weights of the months for which data are unavailable are redistributed proportionally to the months for which data are available. For all other months, the denominator in formula (1) is equal to 1, and the formula is reduced to a simple symmetric moving average with the weights specified in Table 1.

A.3 Alternate expression

In formula (1), a cut-and-normalize approach is used to derive the moving average weights for the first and last six months of the input series. In effect, the cut-and-normalize approach to estimating the trend-cycle employs modified moving average weights to calculate the trend-cycle of the first six months of the series and the final six months. For example, when the trend-cycle estimate for the final month of a series is calculated, the values of the six subsequent months are not yet known. The cut-and-normalize approach proportionally rescales the weights for the months that are available so that their sum is 1. An equivalent expression to formula (1) is given in formula (2), which is based on the rescaled moving average weights, W˜j(t)MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaWGQbaapaqaa8qadaqadaWd aeaapeGaamiDaaGaayjkaiaawMcaaaaaaaa@3AFD@ , given in formula (3).

Formula 2

TCt=j=t6t+6IjW˜j(t)Yj,      (2)MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGubGaam4qa8aadaWgaaWcbaWdbiaadshaa8aabeaak8qacqGH 9aqpdaqfWaqabSqaaiaadQgacqGH9aqpcaWG0bGaeyOeI0IaaGOnaa qaaiaadshacqGHRaWkcaaI2aaaneaacqGHris5aaGccaWGjbWdamaa BaaaleaapeGaamOAaaWdaeqaaOWdbiqadEfapaGbaGaadaqhaaWcba WdbiaadQgaa8aabaWdbmaabmaapaqaa8qacaWG0baacaGLOaGaayzk aaaaaOGaamywa8aadaWgaaWcbaWdbiaadQgaa8aabeaak8qacaGGSa GaaCzcaiaaxMaacaGGOaGaaGOmaiaacMcaaaa@50DE@

Formula 3

whereW˜j(t)= Wj(t)k=t6t+6IkWk(t).      (3)MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaqG3bGaaeiAaiaabwgacaqGYbGaaeyzaiaaysW7caaMe8UaaGjb VlqadEfapaGbaGaadaqhaaWcbaWdbiaadQgaa8aabaWdbmaabmaapa qaa8qacaWG0baacaGLOaGaayzkaaaaaOGaeyypa0JaaeiOamaalaaa paqaa8qacaWGxbWdamaaDaaaleaapeGaamOAaaWdaeaapeWaaeWaa8 aabaWdbiaadshaaiaawIcacaGLPaaaaaaak8aabaWdbmaavadabeWc paqaa8qacaWGQbGaeyypa0JaamiDaiabgkHiTiaaiAdaa8aabaWdbi aadshacqGHRaWkcaaI2aaan8aabaWdbiabggHiLdaakiaadMeapaWa aSbaaSqaa8qacaWGQbaapaqabaGcpeGaam4va8aadaqhaaWcbaWdbi aadQgaa8aabaWdbmaabmaapaqaa8qacaWG0baacaGLOaGaayzkaaaa aaaakiaac6cacaWLjaGaaCzcaiaacIcacaaIZaGaaiykaaaa@6073@

A.4 Illustration

To illustrate how to compute and apply the moving average weights, we consider a monthly series, YtMathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamiDaaWdaeqaaaaa@3848@ , that spans from January 2010 to July 2015—a total of 67 months. The rescaled moving average weights in the formulas below have been rounded to six decimal places. This rounding will sometimes lead to an overestimation or an underestimation at the beginning and end of the series. Because of rounding errors, the trend-cycle obtained using these rounded weights will not be precise within these sections. The full-precision weights must be used to reproduce published trend-cycle estimates exactly.

Three examples below illustrate trend-cycle estimates near the beginning, middle and end of the series. These demonstrate the application of the moving averages when not all months of the 13-term moving average are available (example 1 and example 3), as well as when they are (example 2).

Example 1

For the March 2010 trend-cycle estimate ( t=3 MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamiDaiabg2 da9iaaiodaaaa@38B6@ of the series), the YjMathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@  values are available only for j=1,,9 MathType@MTEF@5@5@+= feaahOart1ev3aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGaamOAaiabg2 da9iaaigdacaGGSaGaeSOjGSKaaiilaiaaiMdaaaa@3BEF@ , which correspond to January 2010 to September 2010. Therefore, a nine-term moving average is used.

According to formula (3), the rescaled weight applied to January 2010 for this moving average is

W˜1(3)=0.136(0.136+0.188+0.224+0.188+0.136+0.067+0.0310.0070.027) 0.145299.MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIXaaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaakiabg2da9maalaaapaqaa8 qacaaIWaGaaiOlaiaaigdacaaIZaGaaGOnaaWdaeaapeWaaeWaa8aa baWdbiaaicdacaGGUaGaaGymaiaaiodacaaI2aGaey4kaSIaaGimai aac6cacaaIXaGaaGioaiaaiIdacqGHRaWkcaaIWaGaaiOlaiaaikda caaIYaGaaGinaiabgUcaRiaaicdacaGGUaGaaGymaiaaiIdacaaI4a Gaey4kaSIaaGimaiaac6cacaaIXaGaaG4maiaaiAdacqGHRaWkcaaI WaGaaiOlaiaaicdacaaI2aGaaG4naiabgUcaRiaaicdacaGGUaGaaG imaiaaiodacaaIXaGaeyOeI0IaaGimaiaac6cacaaIWaGaaGimaiaa iEdacqGHsislcaaIWaGaaiOlaiaaicdacaaIYaGaaG4naaGaayjkai aawMcaaaaacqGHijYUcaqGGcGaaGimaiaac6cacaaIXaGaaGinaiaa iwdacaaIYaGaaGyoaiaaiMdacaGGUaaaaa@7292@

Approximate values of the rescaled moving average weights, W˜j(3)MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaWGQbaapaqaa8qadaqadaWd aeaapeGaamiDaaGaayjkaiaawMcaaaaaaaa@3AFD@ , calculated for the months included in the moving average to estimate the trend-cycle for month 3, are shown in Table 2.

Table 2  Rescaled moving average weights (approximate values) for March 2010
Reference month Weight Approximate value
j=1 (Jan. 2010) W ˜ 1 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIXaaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A8D@ 0.145299
j=2 (Feb. 2010) W ˜ 2 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIYaaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A8E@ 0.200855
j=3 (Mar. 2010) W ˜ 3 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIZaaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A8F@ 0.239316
j=4 (Apr. 2010) W ˜ 4 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI0aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A90@ 0.200855
j=5 (May 2010) W ˜ 5 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI1aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A91@ 0.145299
j=6 (June 2010) W ˜ 6 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A92@ 0.071581
j=7 (July 2010) W ˜ 7 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI3aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A93@ 0.033120
j=8 (Aug. 2010) W ˜ 8 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI4aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A94@ -0.007479
j=9 (Sept. 2010) W ˜ 9 ( 3 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI5aaapaqaa8qadaqadaWd aeaapeGaaG4maaGaayjkaiaawMcaaaaaaaa@3A95@ -0.028846

Finally, applying formula (2) to the input series Y j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@ gives the following expression for T C 3 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGubGaam4qa8aadaWgaaWcbaWdbiaaiodaa8aabeaaaaa@38CF@ , the trend-cycle estimate for March 2010:

TC3=Y1*(0.145299)+ Y2*(0.200855)+ Y3*(0.239316)+ Y4*(0.200855)+ Y5*(0.145299)+Y6*(0.071581)+ Y7*(0.033120)+ Y8*(0.007479)+ Y9*(0.028846).MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcqaaaaaaaaaWdbe aafaqabeWabaaabaGaamivaiaadoeapaWaaSbaaSqaa8qacaaIZaaa paqabaGcpeGaeyypa0Jaamywa8aadaWgaaWcbaWdbiaaigdaa8aabe aak8qacaqGQaWaaeWaa8aabaWdbiaaicdacaGGUaGaaGymaiaaisda caaI1aGaaGOmaiaaiMdacaaI5aaacaGLOaGaayzkaaGaey4kaSIaae iOaiaadMfapaWaaSbaaSqaa8qacaaIYaaapaqabaGcpeGaaeOkamaa bmaapaqaa8qacaaIWaGaaiOlaiaaikdacaaIWaGaaGimaiaaiIdaca aI1aGaaGynaaGaayjkaiaawMcaaiabgUcaRiaabckacaWGzbWdamaa BaaaleaapeGaaG4maaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGaaG imaiaac6cacaaIYaGaaG4maiaaiMdacaaIZaGaaGymaiaaiAdaaiaa wIcacaGLPaaacqGHRaWkcaqGGcGaamywa8aadaWgaaWcbaWdbiaais daa8aabeaak8qacaqGQaWaaeWaa8aabaWdbiaaicdacaGGUaGaaGOm aiaaicdacaaIWaGaaGioaiaaiwdacaaI1aaacaGLOaGaayzkaaGaey 4kaSIaaeiOaiaadMfapaWaaSbaaSqaa8qacaaI1aaapaqabaaak8qa baGaaeOkamaabmaapaqaa8qacaaIWaGaaiOlaiaaigdacaaI0aGaaG ynaiaaikdacaaI5aGaaGyoaaGaayjkaiaawMcaaiabgUcaRiaadMfa paWaaSbaaSqaa8qacaaI2aaapaqabaGcpeGaaeOkamaabmaapaqaa8 qacaaIWaGaaiOlaiaaicdacaaI3aGaaGymaiaaiwdacaaI4aGaaGym aaGaayjkaiaawMcaaiabgUcaRiaabckacaWGzbWdamaaBaaaleaape GaaG4naaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGaaGimaiaac6ca caaIWaGaaG4maiaaiodacaaIXaGaaGOmaiaaicdaaiaawIcacaGLPa aacqGHRaWkcaqGGcGaamywa8aadaWgaaWcbaWdbiaaiIdaa8aabeaa k8qacaqGQaWaaeWaa8aabaWdbiabgkHiTiaaicdacaGGUaGaaGimai aaicdacaaI3aGaaGinaiaaiEdacaaI5aaacaGLOaGaayzkaaaabaGa ey4kaSIaaeiOaiaadMfapaWaaSbaaSqaa8qacaaI5aaapaqabaGcpe GaaeOkamaabmaapaqaa8qacqGHsislcaaIWaGaaiOlaiaaicdacaaI YaGaaGioaiaaiIdacaaI0aGaaGOnaaGaayjkaiaawMcaaaaaaaa@A74C@

Example 2

For the August 2012 trend-cycle estimate ( t=32 MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWG0bGaeyypa0JaaG4maiaaikdaaaa@3991@ of the series), the values of Y j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@ are available for each month from j=26,...,38 MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbGaeyypa0JaaGOmaiaaiAdacaGGSaGaaiOlaiaac6cacaGG UaGaaiilaiaaiodacaaI4aaaaa@3E7F@ , which correspond to February 2012 to February 2013. Therefore, a complete 13-term moving average is used. Because the denominator of formula (3) is exactly equal to 1 in this case, the rescaling has no effect and the weights used in the moving average are identical to the weights in Table 1.

The rescaled weight applied to August 2012 in this moving average is given by

W˜32(32)=0.224 (0.0270.007+0.031+0.067+0.136+0.188+0.224+0.188+0.136+0.067+0.0310.0070.027)=0.224.MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIZaGaaGOmaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaeyypa0 ZaaSaaa8aabaWdbiaaicdacaGGUaGaaGOmaiaaikdacaaI0aGaaeiO aaWdaeaapeWaaeWaa8aabaWdbiabgkHiTiaaicdacaGGUaGaaGimai aaikdacaaI3aGaeyOeI0IaaGimaiaac6cacaaIWaGaaGimaiaaiEda cqGHRaWkcaaIWaGaaiOlaiaaicdacaaIZaGaaGymaiabgUcaRiaaic dacaGGUaGaaGimaiaaiAdacaaI3aGaey4kaSIaaGimaiaac6cacaaI XaGaaG4maiaaiAdacqGHRaWkcaaIWaGaaiOlaiaaigdacaaI4aGaaG ioaiabgUcaRiaaicdacaGGUaGaaGOmaiaaikdacaaI0aGaey4kaSIa aGimaiaac6cacaaIXaGaaGioaiaaiIdacqGHRaWkcaaIWaGaaiOlai aaigdacaaIZaGaaGOnaiabgUcaRiaaicdacaGGUaGaaGimaiaaiAda caaI3aGaey4kaSIaaGimaiaac6cacaaIWaGaaG4maiaaigdacqGHsi slcaaIWaGaaiOlaiaaicdacaaIWaGaaG4naiabgkHiTiaaicdacaGG UaGaaGimaiaaikdacaaI3aaacaGLOaGaayzkaaaaaiabg2da9iaaic dacaGGUaGaaGOmaiaaikdacaaI0aaaaa@8372@

The rescaled moving average weights, W ˜ j ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaWGQbaapaqaa8qadaqadaWd aeaapeGaamiDaaGaayjkaiaawMcaaaaaaaa@3AFD@ , calculated for the months included in the moving average used to calculate the trend-cycle estimate for month 32, are presented in Table 3.

Table 3  Rescaled moving average weights to calculate trend-cycle for August 2012
Reference month(s) Weight Value
j=26 (Feb. 2012) and j=38 (Feb. 2013) W ˜ 26 ( 32 ) , W ˜ 38 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIYaGaaGOnaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaI4aaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42BA@ -0.027
j=27 (Mar. 2012) and j=37 (Jan. 2013) W ˜ 27 ( 32 ) , W ˜ 37 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIYaGaaG4naaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaI3aaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42BA@ -0.007
j=28 (Apr. 2012) and j=36 (Dec. 2012) W ˜ 28 ( 32 ) , W ˜ 36 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIYaGaaGioaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaI2aaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42BA@ 0.031
j=29 (May 2012) and j=35 (Nov. 2012) W ˜ 29 ( 32 ) , W ˜ 35 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIYaGaaGyoaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaI1aaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42BA@ 0.067
j=30 (June 2012) and j=34 (Oct. 2012) W ˜ 30 ( 32 ) , W ˜ 34 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIZaGaaGimaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaI0aaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42B1@ 0.136
j=31 (July 2012) and j=33 (Sept. 2012) W ˜ 31 ( 32 ) , W ˜ 33 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIZaGaaGymaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaOGaaiilai qadEfapaGbaGaadaqhaaWcbaWdbiaaiodacaaIZaaapaqaa8qadaqa daWdaeaapeGaaG4maiaaikdaaiaawIcacaGLPaaaaaaaaa@42B1@ 0.188
j=32 (Aug. 2012) W ˜ 32 ( 32 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaIZaGaaGOmaaWdaeaapeWa aeWaa8aabaWdbiaaiodacaaIYaaacaGLOaGaayzkaaaaaaaa@3C07@ 0.224

Applying formula (2) to the input series Y j MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383D@ produces the following expression for the August 2012 trend-cycle estimate, T C 32 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGubGaam4qa8aadaWgaaWcbaWdbiaaiodaa8aabeaaaaa@38CF@ :

TC32=Y26*(0.027)+Y27*(0.007)+Y28*(0.031)+Y29*(0.067)+Y30*(0.136)+Y31*(0.188)+Y32*(0.224)+Y33*(0.188)+ Y34*(0.136)+Y35*(0.067)+ Y36*(0.031)+Y37*(0.007)+Y38*(0.027).MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcqaaaaaaaaaWdbe aafaqabeWabaaabaGaamivaiaadoeapaWaaSbaaSqaa8qacaaIZaGa aGOmaaWdaeqaaOWdbiabg2da9iaadMfapaWaaSbaaSqaa8qacaaIYa GaaGOnaaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGaeyOeI0IaaGim aiaac6cacaaIWaGaaGOmaiaaiEdaaiaawIcacaGLPaaacqGHRaWkca WGzbWdamaaBaaaleaapeGaaGOmaiaaiEdaa8aabeaak8qacaqGQaWa aeWaa8aabaWdbiabgkHiTiaaicdacaGGUaGaaGimaiaaicdacaaI3a aacaGLOaGaayzkaaGaey4kaSIaamywa8aadaWgaaWcbaWdbiaaikda caaI4aaapaqabaGcpeGaaeOkamaabmaapaqaa8qacaaIWaGaaiOlai aaicdacaaIZaGaaGymaaGaayjkaiaawMcaaiabgUcaRiaadMfapaWa aSbaaSqaa8qacaaIYaGaaGyoaaWdaeqaaOWdbiaabQcadaqadaWdae aapeGaaGimaiaac6cacaaIWaGaaGOnaiaaiEdaaiaawIcacaGLPaaa cqGHRaWkcaWGzbWdamaaBaaaleaapeGaaG4maiaaicdaa8aabeaak8 qacaqGQaWaaeWaa8aabaWdbiaaicdacaGGUaGaaGymaiaaiodacaaI 2aaacaGLOaGaayzkaaGaey4kaSIaamywa8aadaWgaaWcbaWdbiaaio dacaaIXaaapaqabaaak8qabaGaaeOkamaabmaapaqaa8qacaaIWaGa aiOlaiaaigdacaaI4aGaaGioaaGaayjkaiaawMcaaiabgUcaRiaadM fapaWaaSbaaSqaa8qacaaIZaGaaGOmaaWdaeqaaOWdbiaabQcadaqa daWdaeaapeGaaGimaiaac6cacaaIYaGaaGOmaiaaisdaaiaawIcaca GLPaaacqGHRaWkcaWGzbWdamaaBaaaleaapeGaaG4maiaaiodaa8aa beaak8qacaqGQaWaaeWaa8aabaWdbiaaicdacaGGUaGaaGymaiaaiI dacaaI4aaacaGLOaGaayzkaaGaey4kaSIaaeiOaiaadMfapaWaaSba aSqaa8qacaaIZaGaaGinaaWdaeqaaOWdbiaabQcadaqadaWdaeaape GaaGimaiaac6cacaaIXaGaaG4maiaaiAdaaiaawIcacaGLPaaacqGH RaWkcaWGzbWdamaaBaaaleaapeGaaG4maiaaiwdaa8aabeaak8qaca qGQaWaaeWaa8aabaWdbiaaicdacaGGUaGaaGimaiaaiAdacaaI3aaa caGLOaGaayzkaaGaey4kaSIaaeiOaiaadMfapaWaaSbaaSqaa8qaca aIZaGaaGOnaaWdaeqaaaGcpeqaaiaabQcadaqadaWdaeaapeGaaGim aiaac6cacaaIWaGaaG4maiaaigdaaiaawIcacaGLPaaacqGHRaWkca WGzbWdamaaBaaaleaapeGaaG4maiaaiEdaa8aabeaak8qacaqGQaWa aeWaa8aabaWdbiabgkHiTiaaicdacaGGUaGaaGimaiaaicdacaaI3a aacaGLOaGaayzkaaGaey4kaSIaamywa8aadaWgaaWcbaWdbiaaioda caaI4aaapaqabaGcpeGaaeOkamaabmaapaqaa8qacqGHsislcaaIWa GaaiOlaiaaicdacaaIYaGaaG4naaGaayjkaiaawMcaaiaac6caaaaa aa@BE13@

Example 3

For the July 2015 trend-cycle estimate ( t=67 MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWG0bGaeyypa0JaaGOnaiaaiEdaaaa@3999@ of the series), the values of Y j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@ are known only for each month from j=61,...,67 MathType@MTEF@5@5@+= feaahOart1ev3aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGQbGaeyypa0JaaGOnaiaaigdacaGGSaGaaiOlaiaac6cacaGG UaGaaiilaiaaiAdacaaI3aaaaa@3E80@ , which correspond to January 2015 to July 2015. Therefore, a seven-term moving average is used.

The rescaled weight applied to July 2015 in this moving average is

W ˜ 67 ( 67 ) = 0.224   ( 0.224 + 0.188 + 0.136 + 0.067 + 0.031 0.007 0.027 ) 0.366013 . MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaG4naaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaOGaeyypa0 ZaaSaaa8aabaWdbiaaicdacaGGUaGaaGOmaiaaikdacaaI0aGaaeiO aaWdaeaapeWaaeWaa8aabaWdbiaaicdacaGGUaGaaGOmaiaaikdaca aI0aGaey4kaSIaaGimaiaac6cacaaIXaGaaGioaiaaiIdacqGHRaWk caaIWaGaaiOlaiaaigdacaaIZaGaaGOnaiabgUcaRiaaicdacaGGUa GaaGimaiaaiAdacaaI3aGaey4kaSIaaGimaiaac6cacaaIWaGaaG4m aiaaigdacqGHsislcaaIWaGaaiOlaiaaicdacaaIWaGaaG4naiabgk HiTiaaicdacaGGUaGaaGimaiaaikdacaaI3aaacaGLOaGaayzkaaaa aiabgIKi7kaaicdacaGGUaGaaG4maiaaiAdacaaI2aGaaGimaiaaig dacaaIZaGaaiiOaaaa@6B6E@

The rescaled moving average weights, W j ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGxbWdamaaDaaaleaapeGaamOAaaWdaeaapeWaaeWaa8aabaWd biaadshaaiaawIcacaGLPaaaaaaaaa@3AEE@ , calculated for the other months included in the moving average used to calculate the trend-cycle estimate for month 67, are presented in Table 4.

Table 4  Rescaled moving average weights (approximate values) for July 2015
Reference month Weight Approximate value
j=61 (Jan. 2015) W ˜ 61 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaGymaaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C11@ -0.044118
j=62 (Feb. 2015) W ˜ 62 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaGOmaaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C12@ -0.011438
j=63 (Mar. 2015) W ˜ 63 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaG4maaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C13@ 0.050654
j=64 (Apr. 2015) W ˜ 64 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaGinaaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C14@ 0.109477
j=65 (May 2015) W ˜ 65 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaGynaaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C15@ 0.222222
j=66 (June 2015) W ˜ 66 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaGOnaaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C16@ 0.307190
j=67 (July 2015) W ˜ 67 ( 67 ) MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaaI2aGaaG4naaWdaeaapeWa aeWaa8aabaWdbiaaiAdacaaI3aaacaGLOaGaayzkaaaaaaaa@3C17@ 0.366013

Applying formula (2) to the input series Y j MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGzbWdamaaBaaaleaapeGaamOAaaWdaeqaaaaa@383E@ gives the following expression for the July 2015 trend-cycle estimate, T C 67 MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qacaWGubGaam4qa8aadaWgaaWcbaWdbiaaiAdacaaI3aaapaqabaaa aa@3993@ :

T C 67 =   Y 61 * ( 0.044118 )   +   Y 62 * ( 0.011438 )   +   Y 63 * ( 0.050654 )   +   Y 64 * ( 0.109477 ) +   Y 65 * ( 0.222222 )   +   Y 66 * ( 0.307190 )   +   Y 67 * ( 0.366013 ) . MathType@MTEF@5@5@+= feaagKart1ev2aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcqaaaaaaaaaWdbe aafaqabeGabaaabaGaamivaiaadoeapaWaaSbaaSqaa8qacaaI2aGa aG4naaWdaeqaaOWdbiabg2da9iaacckacaWGzbWdamaaBaaaleaape GaaGOnaiaaigdaa8aabeaak8qacaqGQaWaaeWaa8aabaWdbiabgkHi TiaaicdacaGGUaGaaGimaiaaisdacaaI0aGaaGymaiaaigdacaaI4a aacaGLOaGaayzkaaGaaeiOaiabgUcaRiaabckacaWGzbWdamaaBaaa leaapeGaaGOnaiaaikdaa8aabeaak8qacaqGQaWaaeWaa8aabaWdbi abgkHiTiaaicdacaGGUaGaaGimaiaaigdacaaIXaGaaGinaiaaioda caaI4aaacaGLOaGaayzkaaGaaeiOaiabgUcaRiaabckacaWGzbWdam aaBaaaleaapeGaaGOnaiaaiodaa8aabeaak8qacaqGQaWaaeWaa8aa baWdbiaaicdacaGGUaGaaGimaiaaiwdacaaIWaGaaGOnaiaaiwdaca aI0aaacaGLOaGaayzkaaGaaeiOaiabgUcaRiaabckacaWGzbWdamaa BaaaleaapeGaaGOnaiaaisdaa8aabeaak8qacaqGQaWaaeWaa8aaba WdbiaaicdacaGGUaGaaGymaiaaicdacaaI5aGaaGinaiaaiEdacaaI 3aaacaGLOaGaayzkaaaabaGaey4kaSIaaeiOaiaadMfapaWaaSbaaS qaa8qacaaI2aGaaGynaaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGa aGimaiaac6cacaaIYaGaaGOmaiaaikdacaaIYaGaaGOmaiaaikdaai aawIcacaGLPaaacaqGGcGaey4kaSIaaeiOaiaadMfapaWaaSbaaSqa a8qacaaI2aGaaGOnaaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGaaG imaiaac6cacaaIZaGaaGimaiaaiEdacaaIXaGaaGyoaiaaicdaaiaa wIcacaGLPaaacaqGGcGaey4kaSIaaeiOaiaadMfapaWaaSbaaSqaa8 qacaaI2aGaaG4naaWdaeqaaOWdbiaabQcadaqadaWdaeaapeGaaGim aiaac6cacaaIZaGaaGOnaiaaiAdacaaIWaGaaGymaiaaiodaaiaawI cacaGLPaaacaGGUaaaaaaa@9D3D@

A.5 Exact weights

A summary of the rescaled moving average weights, W˜j(t)MathType@MTEF@5@5@+= feaagKart1ev2aqatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq=Jc9 vqaqpepm0xbba9pwe9Q8fs0=yqaqpepae9pg0FirpepeKkFr0xfr=x fr=xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaaeaaaaaaaaa8 qaceWGxbWdayaaiaWaa0baaSqaa8qacaWGQbaapaqaa8qadaqadaWd aeaapeGaamiDaaGaayjkaiaawMcaaaaaaaa@3AFD@ , that are used in calculating the trend-cycle estimates over the entire series are given in Table 5.

Table 5  Rescaled weights for each month, derived under the cut-and-normalize approach
  j=t-6 j=t-5 j=t-4 j=t-3 j=t-2 j=t-1 j=t j=t+1 j=t+2 j=t+3 j=t+4 j=t+5 j=t+6
t=1 0 0 0 0 0 0 =(0.224) / (0.612) =(0.188) / (0.612) =(0.136) / (0.612) =(0.067) / (0.612) =(0.031) / (0.612) =(-0.007) / (0.612) =(-0.027) / (0.612)
t=2 0 0 0 0 0 =(0.188) / (0.8) =(0.224) / (0.8) =(0.188) / (0.8) =(0.136) / (0.8) =(0.067) / (0.8) =(0.031) / (0.8) =(-0.007) / (0.8) =(-0.027) / (0.8)
t=3 0 0 0 0 =(0.136) / (0.936) =(0.188) / (0.936) =(0.224) / (0.936) =(0.188) / (0.936) =(0.136) / (0.936) =(0.067) / (0.936) =(0.031) / (0.936) =(-0.007) / (0.936) =(-0.027) / (0.936)
t=4 0 0 0 =(0.067) / (1.003) =(0.136) / (1.003) =(0.188) / (1.003) =(0.224) / (1.003) =(0.188) / (1.003) =(0.136) / (1.003) =(0.067) / (1.003) =(0.031) / (1.003) =(-0.007) / (1.003) =(-0.027) / (1.003)
t=5 0 0 =(0.031) / (1.034) =(0.067) / (1.034) =(0.136) / (1.034) =(0.188) / (1.034) =(0.224) / (1.034) =(0.188) / (1.034) =(0.136) / (1.034) =(0.067) / (1.034) =(0.031) / (1.034) =(-0.007) / (1.034) =(-0.027) / (1.034)
t=6 0 =(-0.007) / (1.027) =(0.031) / (1.027) =(0.067) / (1.027) =(0.136) / (1.027) =(0.188) / (1.027) =(0.224) / (1.027) =(0.188) / (1.027) =(0.136) / (1.027) =(0.067) / (1.027) =(0.031) / (1.027) =(-0.007) / (1.027) =(-0.027) / (1.027)
t=7,…,T-6 -0.027 -0.007 0.031 0.067 0.136 0.188 0.224 0.188 0.136 0.067 0.031 -0.007 -0.027
t=T-5 =(-0.027) / (1.027) =(-0.007) / (1.027) =(0.031) / (1.027) =(0.067) / (1.027) =(0.136) / (1.027) =(0.188) / (1.027) =(0.224) / (1.027) =(0.188) / (1.027) =(0.136) / (1.027) =(0.067) / (1.027) =(0.031) / (1.027) =(-0.007) / (1.027) 0
t=T-4 =(-0.027) / (1.034) =(-0.007) / (1.034) =(0.031) / (1.034) =(0.067) / (1.034) =(0.136) / (1.034) =(0.188) / (1.034) =(0.224) / (1.034) =(0.188) / (1.034) =(0.136) / (1.034) =(0.067) / (1.034) =(0.031) / (1.034) 0 0
t=T-3 =(-0.027) / (1.003) =(-0.007) / (1.003) =(0.031) / (1.003) =(0.067) / (1.003) =(0.136) / (1.003) =(0.188) / (1.003) =(0.224) / (1.003) =(0.188) / (1.003) =(0.136) / (1.003) =(0.067) / (1.003) 0 0 0
t=T-2 =(-0.027) / (0.936) =(-0.007) / (0.936) =(0.031) / (0.936) =(0.067) / (0.936) =(0.136) / (0.936) =(0.188) / (0.936) =(0.224) / (0.936) =(0.188) / (0.936) =(0.136) / (0.936) 0 0 0 0
t=T-1 =(-0.027) / (0.8) =(-0.007) / (0.8) =(0.031) / (0.8) =(0.067) / (0.8) =(0.136) / (0.8) =(0.188) / (0.8) =(0.224) / (0.8) =(0.188) / (0.8) 0 0 0 0 0
t=T =(-0.027) / (0.612) =(-0.007) / (0.612) =(0.031) / (0.612) =(0.067) / (0.612) =(0.136) / (0.612) =(0.188) / (0.612) =(0.224) / (0.612) 0 0 0 0 0 0

References

The following references provide more information on the topic of seasonal adjustment, including trend-cycle estimation.

Dagum, E. B. & Luati, A. (2008). A cascade linear filter to reduce revisions and false turning points for real time trend-cycle estimation. Econometric Reviews, 28(1-3), 40-59.

Statistics Canada (2009). Seasonal adjustment and trend-cycle estimation, in Statistics Canada Quality Guideline, 5th edition, Catalogue no. 12-539-X. https://www150.statcan.gc.ca/n1/pub/12-539-x/2009001/seasonal-saisonnal-eng.htm

Statistics Canada (2026). Seasonal adjustment: Concepts and interpretation, 2026. Catalogue no. 19-20-0001. https://www150.statcan.gc.ca/n1/pub/19-20-0001/192000012026001-eng.htm

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