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FEDERAL RESERVE BANK OF SAN FRANCISCO WORKING PAPER SERIES Unemployment Dynamics in the OECD Michael Elsby University of Edinburgh and NBER Bart Hobijn FRB San Francisco Aysegül Sahin FRB New York February 2011 Working Paper 2009-04 http://www.frbsf.org/publications/economics/papers/2009/wp09-04bk.pdf The views in this paper are solely the responsibility of the authors and should not be interpreted as reflecting the views of the Federal Reserve Bank of San Francisco or the Board of Governors of the Federal Reserve System. Unemployment Dynamics in the OECD Michael W. L. Elsby Bart Hobijn Ayşegül Şahin University of Edinburgh and NBER FRB San Francisco FRB New York February 2011 Abstract We provide a set of comparable estimates for the rates of in‡ow to and out‡ow from unemployment using publicly available data for fourteen OECD economies. We then devise a method to decompose changes in unemployment into contributions accounted for by changes in in‡ow and out‡ow rates for cases where unemployment deviates from its ‡ow steady state, as it does in many countries. Our decomposition reveals that ‡uctuations in both in‡ow and out‡ow rates contribute substantially to unemployment variation within countries. For Anglo-Saxon economies we …nd approximately a 15:85 in‡ow/out‡ow split to unemployment variation, while for Continental European and Nordic countries, we observe much closer to a 45:55 split. Using the estimated ‡ow rates we compute gross worker ‡ows into and out of unemployment. In all economies we observe that increases in in‡ows lead increases in unemployment, whereas out‡ows lag a ramp up in unemployment. Keywords: Unemployment, Worker ‡ows, Job Finding Rate, Separation Rate. JEL-codes: E24, J6. We would like to thank anonymous referees, Regis Barnichon, Shigeru Fujita, Wilbert van der Klaauw, Emi Nakamura, Simon Potter, Gary Solon, participants at the New York/Philadelphia Workshop on Quantitative Macroeconomics 2008, Midwest Macroeconomics Conference 2009, Recent Developments in Macroeconomics Conference 2009, EEA Conference 2009, CREI/Kiel Conference on Macroeconomic Fluctuations and the Labor Market 2009 for helpful comments, and Joseph Song for outstanding research assistance. The views expressed in this paper are those of the authors and do not necessarily re‡ect those of the Federal Reserve Bank of New York, the Federal Reserve Bank of San Francisco or the Federal Reserve System. An Excel spreadsheet with all the data, calculations, and results presented in this paper is available for download at http://www.frbsf.org/economics/economists/bhobijn/UnemploymentDynamicsInTheOECD.xlsm. Thanks to Jonas Staghøj for pointing out a coding error in a previous version of the spreadsheet. E-mail addresses for correspondence: mike.elsby@ed.ac.uk; bart.hobijn@sf.frb.org; aysegul.sahin@ny.frb.org. 1 1 Introduction Unemployment rates among developed economies have varied substantially both across time and across countries over the last 40 years. This variation in unemployment may occur as a result of variation in the rate at which workers ‡ow into the unemployment pool, variation in the rate at which unemployed workers exit the unemployment pool, or a combination of the two. The relative contributions of changes in in‡ow and out‡ow rates to changes in unemployment have been abundantly documented for the U.S.1 Less is known, however, about the driving forces of unemployment variation in other countries. Such a question is of interest because of the considerable variation in unemployment that has been observed in developed economies in recent decades, notably in Continental Europe. In this paper, we provide a detailed analysis of unemployment ‡ows for fourteen developed economies using publicly available data. In the …rst part of our analysis we describe how it is possible to derive measures of the rates of in‡ow2 to and out‡ow from the unemployment pool using annual data from the OECD. To do this, we generalize the method developed by Shimer (2007), which makes use of time series for the number employed, the number unemployed, and the number unemployed less than …ve weeks to infer ‡ow hazard rates for the U.S. A limitation that arises when applying this methodology outside the U.S. is that series on short duration unemployment can be noisy for countries in which short durations account for a small proportion of overall unemployment, such as in Continental Europe. To address this, we develop a method that exploits additional data on unemployment at higher durations to construct a set of comparable time series for the unemployment in‡ow and out‡ow rates across countries. Our measures allow us to document a set of stylized facts on unemployment ‡ows among developed economies. First, the average level of unemployment in‡ow and out‡ow rates varies substantially across countries. Interestingly, the results suggest a natural partitioning of economies into Anglo-Saxon, Nordic and Continental European. Anglo-Saxon and Nordic economies display high exit rates from unemployment, with monthly hazards that exceed 20 percent. In stark contrast, out‡ow rates among Continental European economies 1 See Elsby, Michaels, and Solon [2009], Fujita and Ramey [2008], Hall [2005a,b], Shimer [2007], and Yashiv [2007]. 2 Some recent literature on unemployment ‡ows has referred to the rate of in‡ow into unemployment as the “separation rate” (Shimer, 2005a, b; Fujita and Ramey, 2008). We refer to it as the in‡ow rate for two reasons. First, a separation is typically taken to mean a quit or a layo¤ from an employer. In the presence of job-to-job transitions, such separations need not lead to an unemployment spell. Second, some unemployment spells originate from non-participation rather than a separation from employment. 2 are much lower— typically less than 10 percent at a monthly frequency. Symmetrically, unemployment in‡ow rates also vary considerably across countries. Anglo-Saxon and Nordic countries exhibit in‡ow hazards that exceed 1.5 percent at a monthly frequency. However, as with the observed levels of out‡ow rates, monthly in‡ow rates among Continental European economies are again much lower at around 0.5 to 1 percent. These observations con…rm the diagnosis that European labor markets are sclerotic in the sense that they display much lower rates of reallocation of labor, as documented in Blanchard and Summers (1986), Bertola and Rogerson (1997), Blanchard and Wolfers (2000), and Blanchard and Portugal (2001). In the second part of our analysis, we pose the question of how much of the observed variation in unemployment within each country can be accounted for by variation in the in‡ow rate into unemployment and variation in the out‡ow rate from unemployment respectively. To answer this, we provide a method for decomposing changes in the unemployment rate into contributions due to changes in the ‡ow hazards that can be applied in countries with very di¤erent unemployment dynamics. Recent literature (Elsby, Michaels, and Solon [2009], Fujita and Ramey [2009], Petrongolo and Pissarides [2008]) has evaluated these contributions under the assumption that the unemployment rate is closely approximated by its ‡ow steady state value. Under this assumption, contemporaneous unemployment variation may be decomposed into contributions related to contemporaneous logarithmic variation in in‡ow and out‡ow hazards. While this steady state assumption holds as a reasonable approximation in the U.S., we show that it can be very inaccurate in other developed economies, notably those of Continental Europe. Reacting to this we show that, in cases where unemployment deviates from steady state, current variation in unemployment can be decomposed recursively into contributions due to current and past logarithmic changes in the in‡ow and out‡ow hazards. Intuitively, when unemployment is out of steady state, it can vary as a result of contemporaneous changes in the in‡ow and out‡ow rates, or as a result of dynamics driven by past changes in these ‡ow hazards. Using our alternative decomposition, we obtain a much more accurate characterization of changes in unemployment rates across countries. Application of our decomposition to our estimated time series for the ‡ow hazard rates provides us with a second stylized fact on unemployment ‡ows. Among all countries that we consider, ‡uctuations in both in‡ow and out‡ow rates contribute substantially to unemployment variations within countries. The relative contribution of each di¤ers across countries, however. Among Anglo-Saxon economies we …nd approximately a 15:85 in‡ow/out‡ow split of unemployment variation, a result that echoes recent …ndings for the U.S. over the same 3 sample period. For Continental European and Nordic countries, however, we observe much closer to a 45:55 in‡ow/out‡ow split. Thus, a complete understanding of unemployment variation among our large sample of developed economies requires an understanding of the determinants of both the in‡ow rate as well as the out‡ow rate. The …nal part of our empirical analysis uses the estimated ‡ow hazard rates to compute measures of the number of workers ‡owing in and out of the unemployment pool (as opposed to the hazard rates for these ‡ows).3 A third stylized fact that emerges from these results is that a geographical partitioning also applies to average worker ‡ows across countries. AngloSaxon and Nordic countries exhibit annual worker ‡ows in and out of unemployment that comprise more than 15 percent of the labor force. Among Continental European economies, on the other hand, worker ‡ows typically involve less than 10 percent of the labor force, echoing the …ndings of Blanchard and Portugal (2001) and Bertola and Rogerson (1997). We then analyze the dynamic relationship between these worker ‡ows and unemployment within each country. Using a simple correlation analysis, we document a fourth stylized fact on unemployment ‡ows among developed economies: The timing of the contributions of in‡ows and out‡ows to unemployment variation displays a remarkable uniformity across countries. In all economies we observe that increases in in‡ows lead increases in unemployment, whereas out‡ows lag a ramp up in unemployment, an observation that has been highlighted for the U.S. in earlier studies.4 Our …ndings that variation in unemployment in‡ows accounts for a substantial fraction of unemployment variation and is an important leading indicator for changes in unemployment dovetails with a recent literature on U.S. unemployment ‡ows. A growing trend in modern macroeconomic models of the aggregate labor market has been to assume that the in‡ow rate into unemployment is acyclical (Hall [2005a,b], Shimer [2005] among others). Reacting to this, a number of recent studies has cautioned against this trend by documenting evidence for systematic countercyclical movements in unemployment in‡ows in U.S. data.5 Our …ndings 3 Our analysis is not the …rst to estimate worker ‡ows across countries. Other studies that examine worker ‡ows for a subset of European countries include Albaek and Sørensen (1998) for Denmark; Bauer and Bender (2004) and Bachmann (2005) for Germany; Bertola and Rogerson (1997) for Canada, Germany, Italy, the U.K., and the U.S.; Burda and Wyplosz (1994) for France, Germany, Spain, and the U.K.; Petrongolo and Pissarides (2008) for France, Spain and the U.K.; and Pissarides (1986), Bell and Smith (2002), and Gomes (2008) for the U.K. Reichling (2005) reports estimates of the separation rate for a set of countries (see his Table 5) and also emphasizes that the separation rate is lower in European countries than in the U.S. 4 See Darby, Haltiwanger, and Plant [1985, 1986], Blanchard and Diamond [1990], Davis [2006], Fujita and Ramey [2008]. 5 Recent studies that have emphasized this fact include Braun, De Bock, and DiCecio (2006); Davis (2006); Elsby, Michaels, and Solon (2009); Fujita and Ramey (2008); Kennan (2006); and Yashiv (2008). Older 4 show that this caution resonates all the more if we wish to understand the considerable variation in unemployment rates observed outside the U.S. The remainder of the paper is organized as follows. In section 2 we summarize the OECD data that we use throughout our analysis. In section 3, we describe our methodology for inferring the rates of in‡ow to and out‡ow from the unemployment pool using the OECD data. Application of this methodology provides individual time series for the unemployment ‡ow hazards for each of the fourteen countries in our sample. In section 4, we pose the question of how much of the variation in unemployment within countries can be accounted for by changes in the in‡ow and out‡ow rates respectively. To answer this question, we derive a decomposition of unemployment variation that allows for unemployment to deviate from steady state. We show that allowing for such deviations is critical for understanding unemployment ‡uctuations outside the U.S. Section 5 presents evidence on the number of workers ‡owing in and out of unemployment, and documents stylized facts on the timing of the impact of worker ‡ows on unemployment changes. Section 6 summarizes and o¤ers conclusions. 2 Data Since a large part of our analysis is informed by the available data, we start by discussing the OECD samples that we use. These are taken from two di¤erent sources. First, we use annual measures of the unemployment stock by duration, taken from OECD (2010a).6 We then supplement these data with quarterly measures of the aggregate unemployment rate, taken from OECD (2010b). Both slices of data are based on the labor force surveys conducted in each of the countries in our sample. The fourteen economies that we focus on are: Australia, Canada, France, Germany, Ireland, Italy, Japan, New Zealand, Norway, Portugal, Spain, Sweden, United Kingdom, and the United States. For all countries relatively long historical quarterly time series are available for the unemployment rate. Our focus on these economies is primarily driven by the length of the available requisite series for unemployment by duration. Throughout, we denote the fraction of the labor force in an unemployment spell of less than d months in <1 <3 <6 <12 7 month t by u<d . t . For our analysis we use annual time series for ut , ut , ut , and ut studies that have documented this include Perry (1972); Marston (1976); Blanchard and Diamond (1990); and Baker (1992). 6 The data are also publicly available on the web from http://stats.oecd.org. 7 For many countries, data on unemployment duration initially were collected only once a year. More 5 Note that we de…ne these categories inclusively, in the sense that u<3 includes u<1 t t , and so on. The starting year for the available series varies between 1968 (for the U.S.) and 1986 (for New Zealand and Portugal).8 For all countries, the data end in 2009. An important advantage of using data from the OECD is that, even though the labor force surveys of these countries have di¤erent structures, the OECD data have been standardized to adhere to the same structure. This aids cross-country comparisons of our results.9 3 The Ins and Outs of Unemployment in the OECD At the heart of our analysis is a set of estimated annual time series of ‡ow hazard rates into and out of unemployment for fourteen OECD countries. These time series are estimated using an extension of the method that Shimer (2007) developed for the United States. Shimer’s method cannot be applied directly to other OECD countries because the required data are not available. The extension that we introduce allows us to overcome this limitation and to produce annual time series for the rates of in‡ow to and out‡ow from the unemployment pool for a large subset of OECD countries. 3.1 Analytical Framework The evolution over time of the unemployment rate, which we denote by ut , can be written as:10 dut = st (1 ut ) ft ut ; (1) dt where st is the monthly rate of in‡ow into unemployment, ft is the monthly out‡ow rate from unemployment, and t indexes months.11 As mentioned above, the data that we use in recently, mainly due to the standardization of Labor Force Surveys in the European Union, countries are collecting these data at a quarterly frequency. Because our aim is to construct historical time series that are as long as possible, we focus on annual time series. 8 The initial year in the sample for each country is listed in Table 2. 9 While the OECD goes to some lengths to standardize their unemployment measures, their procedures may not be perfect. For example, it is possible that workers who de…ne themselves as out of the labor force in e.g. the U.S. might de…ne themselves as unemployed in Europe. Addressing these important issues of standardization is beyond the scope of this paper. 10 It is important to note that equation (1) implicitly assumes that all of the in‡ow into unemployment originates from employment. We have calculated a set of results taking into account non-participation. Except for the level of the average in‡ow rate, these results were very similar to those we present here. Details of these results, as well as an explanation of why this is the case are provided in the Appendix. 11 We de…ne the ‡ow hazards st and ft in monthly terms to aid comparison with estimates reported in U.S. studies of unemployment ‡ows. 6 the remainder of the paper allow us to infer unemployment ‡ows at an annual frequency. Thus, we would like to relate the continuous time evolution of unemployment in equation (1) to the unemployment rates that we observe at discrete annual intervals. Assuming that the ‡ow hazards are constant within years,12 and solving equation (1) forward one year allows us to do this: (2) ut = t ut + (1 t )ut 12 , where ut = st st + ft (3) denotes the ‡ow steady-state unemployment rate, and t =1 e 12(st +ft ) (4) is the annual rate of convergence to steady state. In this way we can relate variation in the unemployment stock ut in a given country over the course of a year to variation in the underlying ‡ow hazards, st and ft .13 To implement this, however, we need to obtain estimates of these ‡ow hazards, to which we now turn. Our method for estimating the out‡ow rate ft is an extension of the method popularized by Shimer (2007). In his study of U.S. unemployment ‡ows, he infers the monthly out‡ow probability Ft using the identity that the monthly change in the unemployment stock is given by ut+1 ut = u<1 Ft ut . (5) t+1 Here u<1 t+1 denotes the stock of unemployed workers with duration less than one month, and hence re‡ects the ‡ows into unemployment; Ft ut re‡ects the ‡ows out of unemployment. 12 This assumption does lead to some smoothing out of high frequency variation in the ‡ow hazards that we estimate. As many U.S. studies of unemployment ‡ows have shown, and as we will con…rm in our cross– country estimates, it is predominantly the in‡ow rate st that displays such high frequency variation. It follows that annual smoothing is likely to lead to an overstatement of the contribution of changes in the out‡ow rate ft to unemployment variation. This works against a key …nding of this paper that variation in the in‡ow rate st accounts for a substantial fraction of unemployment variation. 13 For simplicity, we abstract from labor force growth in equations (1) through (4). It is straightforward to show, however, that if the labor force grows at monthly rate gt , then ut = st =(st + ft + gt ) and t = 1 e 12(st +ft +gt ) . In our sample, gt averages around 0.001 on a monthly basis. In contrast, the average value of (st + ft ) in our sample is on the order of 0.2. This point also extends to speci…c countries and periods in which labor force growth accelerates. For example, gt rose in the 2000s in Spain up to 0.003 on a monthly basis. However, over the same period, we observe that (st + ft ) averages around 0.1 in Spain. Consequently, allowing for labor force growth does not a¤ect our results in a quantitatively important way. 7 Solving for the monthly out‡ow probability, one obtains14 Ft = 1 u<1 t+1 ut+1 ut . (6) The monthly out‡ow probability is then related to the associated monthly out‡ow hazard rate, ft<1 , through ft<1 = ln(1 Ft ). (7) 3.2 Estimation of Flow Hazard Rates Duration Dependence and Estimation of the Out‡ow Rate In what follows we will see that the estimate of the out‡ow rate implied by equation (6) works well for countries in which the out‡ow rate from unemployment is relatively high, such as the U.S. However, in countries that exhibit low exit rates, such as those of Continental Europe, estimates based on equation (6) can be substantially noisy. The simple reason is that low out‡ow rates imply that very few unemployed workers at a point in time are in their …rst month of unemployment, which increases the sampling variance of the estimate of u<1 t+1 , and in turn 15 leads to noisy estimates of ft . Our approach to this problem is to use the additional unemployment duration data available from the OECD to increase the precision of our estimate of ft in countries where the out‡ow rate is low. To see how this may be done recall that the OECD data also report the unemployment stock at durations higher than one month. It follows that, analogous to the method detailed above, it is possible to write the probability that an unemployed worker 14 Since the OECD database reports only quarterly data on the aggregate unemployment rate, we compute ut by interpolating quarterly data. 15 For example, the OECD data for the U.S. are based on the Current Population Survey, which surveys around 130,000 individuals each month. In the U.S., the labor force participation rate averaged 47.9 percent, 6.1 percent of which were unemployed, 43.3 percent of which were unemployed for less than one month. This suggests around 130; 000 0:479 0:061 0:433 1; 645 respondents have been unemployed less than one month in each month’s survey. In contrast, each survey for Germany includes around 165,000 respondents, with an average participation rate of 48.5 percent, 8.3 percent of which were unemployed, but only 6.9 percent of which were unemployed for less than one month. This implies that only around 458 respondents have been unemployed for less than one month in each survey for Germany. This simple comparison would suggest that the sampling variance of the estimate of short-term unemployment in each survey in Germany will be 3.6 times its U.S. equivalent. In addition, this calculation becomes much more extreme when one accounts for the fact that the OECD data for the U.S. are annual averages of monthly data, while those for Germany correspond to just one month, April. Similar calculations for other European countries yield similar conclusions. 8 exits unemployment within d months as Ft<d =1 u<d t+d ut+d ut . (8) As before, this can be mapped into an out‡ow rate estimate given by ft<d = ln(1 Ft<d )=d: (9) Given the available data, we can estimate ft<d for d = 1; 3; 6; 12.16 It is important to clarify the interpretation of the out‡ow rate measures ft<d . It is tempting to interpret ft<d as the out‡ow rate for unemployed workers of duration d. However, that is not an accurate interpretation. Rather, it is the hazard rate associated with the probability that an unemployed worker at time t completes her spell within the subsequent d months. These four measures, ft<1 ; ft<3 ; ft<6 ; and ft<12 , are not necessarily estimates of the same out‡ow rate. Only in the case where the out‡ow hazard is unrelated to the duration of an unemployment spell, i.e. if there is no duration dependence in out‡ow rates, are all four measures consistent estimates of the aggregate out‡ow rate from unemployment, de…ned as the average out‡ow rate among the entire unemployed population. However, if there is duration dependence in unemployment out‡ow rates in a given country, then estimates based on durations of unemployment greater than one month, ft<3 ; ft<6 ; and ft<12 , will not yield consistent estimates of the average out‡ow rate among the unemployed. For example, imagine that there exists negative duration dependence whereby the out‡ow rate declines with duration.17 In such an environment, we would expect to observe ft<1 > ft<3 > ft<6 > ft<12 . To see why, consider the version of equation (8) which expresses the fraction of the unemployment stock in month t that exits within the next three months. The remaining unemployed workers that do not exit over these subsequent three months increasingly will be comprised of unemployed workers with low out‡ow rates, i.e. the high duration unemployed. This process of dynamic selection will imply that excessive weight will be placed on the low out‡ow rates of high duration unemployed workers in the estimate of ft<3 , generating a downward bias in its estimate of ft . This argument applies even more 16 The appendix contains a detailed description on how we estimate these rates combining the annual and quarterly data available. 17 In the U.S., for example, the …nding of substantial negative duration dependence in unemployment exit rates has been widely documented since Kaitz (1970). Most recently, Shimer (2008) has emphasized this stylized fact for the U.S. 9 strongly to the estimates of ft<6 and ft<12 .18 In light of this, we formally test for the presence of duration dependence in out‡ow rates by testing the hypothesis that ft<1 = ft<3 = ft<6 = ft<12 . The formal details are described in the Appendix, but our general approach is as follows. First, we derive the asymptotic distribution of the unemployment rates by duration as well as for the unemployment rates. We then apply the Delta method to compute the joint asymptotic distribution of the out‡ow rate estimates ft<d with d = 1; 3; 6; 12. This allows us to formulate a simple Chi-squared test of the null hypothesis of no duration dependence. It should be noted that we test for a very broad de…nition of duration dependence. As has been emphasized since Kaitz (1970), duration dependence can arise through two channels. “True”duration dependence refers to the case where unemployment duration has a causal e¤ect on the out‡ow rates of individual workers. In contrast, “spurious” duration dependence refers to the process of dynamic selection whereby workers with high exit rates leave unemployment faster than those with low exit rates, thereby generating a negative correlation between duration and out‡ow rates (Salant, 1977). Our hypothesis test is not intended to distinguish between these two sources of duration dependence, but rather to test for whether the alternative measures of the out‡ow rate derived above are signi…cantly di¤erent from one another. Thus, the duration dependence we test for can arise due to either dynamic selection or true duration dependence or both. For those countries for which we reject the hypothesis of no duration dependence, we follow the recent U.S. literature in using ft<1 as our estimate of the unemployment out‡ow rate, as this measure provides the most accurate estimate of the average out‡ow rate in the presence of duration dependence. For countries with weak evidence for duration dependence for which we do not reject the null, we make use of all the additional information on the out‡ow rate contained in ft<3 ; ft<6 ; and ft<12 in order to obtain a more precise estimate of ft . Speci…cally, we use our estimates of the asymptotic distribution of the out‡ow rate estimates, ft<1 ; ft<3 ; ft<6 ; and ft<12 to compute an optimally weighted estimate of the out‡ow rate that minimizes the mean squared error of the estimate.19 The results of the hypothesis test are reported in Table 2. While we …nd signi…cant evidence of duration dependence in Anglo-Saxon and Nordic countries and Japan, we do not observe signi…cant evidence among the Continental European countries in our sample.20 It is By the same token, the estimate of ft<1 that has been widely used in recent literature is also subject to this drawback, just to a lesser degree than the other three measures. 19 The construction of these optimal weights is detailed in the Appendix. 20 While our hypothesis test provides a natural rule of thumb, we implicitly rule in favor of the null when 18 10 natural to ask whether this conclusion is supported by the results of microeconometric studies that estimate duration dependence for speci…c European economies. A particularly useful summary of this literature is reported by Machin and Manning (1999, Table 6). They show that the evidence for duration dependence among European economies is quite inconclusive. Estimates of duration dependence in Germany and Spain, for example, di¤er across studies, with evidence found for negative, positive and negligible duration dependence reported. Our conclusion of limited evidence for duration dependence lies at the midpoint of this array. A clearer consensus emerges for France and the U.K. For France, the literature …nds very little evidence for duration dependence, at least within the …rst year of the unemployment spell. In contrast, for the U.K., the literature in general …nds evidence for negative duration dependence. Our estimates are in line with these conclusions. Our results are also consistent with other work that has estimated duration dependence across countries. In their own analysis, Machin and Manning (1999) …t a Weibull duration model to the duration structure of unemployment across countries. They report weak negative duration dependence in France and Spain in the 1990s, but strong negative duration dependence in Australia, the U.K. and the U.S. in the 1980s and 1990s. Using a similar approach on OECD data, Hobijn and Şahin (2009) also …nd little evidence of duration dependence among Continental European economies, but substantial evidence among economies with high unemployment out‡ow rates. The result of our hypothesis test is that we use ft<1 as our estimate of the out‡ow rate for the Anglo-Saxon countries in our sample and the optimally weighted average of ft<1 ; ft<3 ; ft<6 ; and ft<12 for the remaining countries. Temporal Aggregation Bias and Estimation of the In‡ow Rate Given our estimate of the out‡ow rate, we compute the in‡ow rate st using the method pioneered by Shimer (2007). In particular, note that the expression for the annual unemployment rate in equation (2) is simply a nonlinear equation in the unemployment rates, ut+12 and ut , and the ‡ow hazard rates, st and ft . We can thus solve equation (2) for the in‡ow rate. As emphasized by Shimer (2007) and subsequent work based on his method, this estimate of the in‡ow rate is robust to temporal aggregation bias in the measurement of unemployment in‡ows. In particular, since equation (2) is inferred from solving forward the continuous-time di¤erential equation for the evolution of the unemployment rate, it accounts for the fact that the hypothesis of no duration dependence cannot be rejected. This raises the question of the power of the test. In results that can be replicated in the spreadsheet that accompanies this paper, we observe that the test does indeed have high power among the Continental European economies for which we fail to reject the null, in the sense that the estimates of ft<d are similar for all durations d. 11 workers who ‡ow into unemployment after one period’s survey may exit prior to the next period’s survey, ‡ows that would be missed in discrete-time data. Correcting for temporal aggregation bias in the in‡ow rate is particularly important the context of the OECD data, since the data are available at an annual frequency, in contrast to the monthly data that are available for the U.S.21 A natural question is whether a symmetric bias a¤ects estimation of the out‡ow rate. Interestingly, time aggregation causes relatively little bias in the out‡ow rate, for two reasons. First, consider the measure of the out‡ow probability in equation (6). This is just the complement of the probability that those unemployed at time t remain unemployed by time t + 1. If there were a time aggregation problem, the concern would be that the data fail to pick up on workers who exit unemployment after one period’s survey, but who re-enter prior to the next period’s survey. However, the measure of the out‡ow probability in equation (6) does not miss such transitions: Any worker who followed this path would be identi…ed as short-term unemployed in the second survey, and therefore correctly counted as an out‡ow. Second, it still could be the case that the measure of the out‡ow probability in equation (6) misses multiple exits from unemployment within the period (e.g. out after …rst survey, in again, out again, in again prior to next survey). However, we will see that the in‡ow rate in practice is very small in comparison to the out‡ow rate for all countries in our sample, so that the probability of such multiple transitions is likely to be miniscule.22 3.3 Evidence from OECD Data The average unemployment in‡ow and out‡ow hazards over the sample periods for the whole sample of countries are reported in Table 2. A striking observation from these results is the substantial cross-country variation in both st and ft . A particularly useful illustration of this point is in Figure 1, which displays the average values of st and ft from Table 2 in graph form. Interestingly, one can discern a natural partition of developed economies between Anglo-Saxon, Nordic and Continental European economies. Figure 1 reveals very high out‡ow rates among the Anglo-Saxon and Nordic economies. 21 The magnitude of the correction for time aggregation bias in in‡ow rates also will vary across countries. In European economies with sclerotic unemployment ‡ows, we will see that the out‡ow rate from unemployment ft is low. As a result, the correction for time aggregation bias is smaller for these countries, as a lower proportion of in‡ows into unemployment after one survey will exit unemployment prior to the next survey. 22 Shimer (2007) makes a similar point. In his words: “Because the probability of losing a job during the month that it is found is comparatively small, time aggregation causes relatively little bias in the job …nding rate.” 12 Among these countries the average monthly unemployment out‡ow hazard exceeds 20 percent. The economies of Continental Europe stand in stark contrast. Unemployment out‡ow rates in these economies lie below 10 percent at a monthly frequency. A similar picture develops for the estimates of the in‡ow rates in Figure 1. We observe high unemployment in‡ow hazards among the Anglo-Saxon and Nordic economies, which typically lie above 1.5 percent on a monthly basis. Likewise, in‡ow rates among the European economies are again much lower at around 0.5 to 1 percent per month. Figure 1 also shows that there are both extremes and intermediate cases that are understated in this Anglo-Saxon/Nordic/Continental Europe taxonomy. For Japan, while the average unemployment out‡ow rate of 19 percent is similar to those in Anglo-Saxon and Nordic economies, its in‡ow rate is more comparable to those of Continental Europe. Another intermediate case is the U.K., which displays unemployment ‡ows that lie halfway between the Anglo-Saxon and the Continental European models. Perhaps the most striking observation, however, is the outlier status of the U.S. With an average monthly unemployment out‡ow rate of nearly 60 percent and an average in‡ow rate of 3.5 percent, it exhibits transition rates at least 50 percent larger than the remainder of our sample of countries. Figures 2 and 3 display the time series for the in‡ow and out‡ow hazards for each country in our sample. The transition rates are plotted on log scales since, as emphasized in the literature on unemployment ‡ows, and as we will con…rm in what follows, it is the logarithmic variation in st and ft that places them on an equal footing with respect to ‡uctuations in the unemployment rate. Figures 2 and 3 reveal that, in addition to signi…cant cross-country variation in unemployment ‡ows, there is also substantial variation in unemployment ‡ow hazards over time within countries. Although there is a great deal of information contained in these …gures, a number of observations come to light. First, there are important di¤erences in the frequency of ‡uctuations in unemployment ‡ows across economies. Among the Anglo-Saxon economies, a clear cyclical pattern is present, suggesting a substantial high frequency component to unemployment ‡uctuations in these countries. Among other economies, however, the variation in st and ft occurs at a much lower frequency, and it is hard to di¤erentiate cycle from trend. Figures 2 and 3 are also indicative of how the relative contributions of variation in the in‡ow and out‡ow rates di¤er across countries. Speci…cally, the Anglo-Saxon economies appear to display relatively more variation in the out‡ow rate from unemployment, a point that has been emphasized in recent literature for the U.S. However, inspection of the time 13 series for the Nordic and European economies reveals greater variation in the in‡ow rate, suggesting about an equal contribution of the ins and the outs to unemployment variation in these countries. Figures 2 and 3 also provide a sense of the degree to which these stylized facts have held true in the most recent recession. In many respects, historical di¤erences in unemployment dynamics between Anglo-Saxon and Continental European economies have been echoed in recent data. Inspection of the time series for the ‡ow hazards after 2007 reveals that, as in the past, the recent rise in unemployment has been associated more with rises in unemployment in‡ows in Continental European economies, and with declines in rates of out‡ow in AngloSaxon countries. Figures 2 and 3 do point to one stark feature of the recession, however: The out‡ow rate from unemployment in the U.S. fell precipitously to reach a historic low, a point noted by many observers of the Great Recession in the U.S. (see Elsby, Hobijn and Şahin [2010], for example). An advantage of the cross-country estimates in Figures 2 and 3 is that they provide a useful perspective on this phenomenon. Despite the record decline in rates of exit from unemployment in the U.S., the level of the out‡ow rate witnessed recently in the U.S. still dwarfs those observed in Continental Europe. Of course, this visual impression is only suggestive of the relative contributions of the in‡ow and out‡ow hazards to unemployment variation; we address this issue more formally in section 4. Before we do so, we …rst compare our estimates of unemployment transition rates with those reported in related literature. 3.4 Relation to Existing Evidence Unemployment ‡ows for the U.S. have been extensively studied in the literature. Almost all of these studies, including Elsby, Michaels, and Solon (2009), Fujita and Ramey (2009) and Shimer (2007), are based on data from the Current Population Survey. Since the OECD data that we use are also based on the same survey data, the levels of our estimated ‡ow hazards are in line with these previous estimates.23 The cross-country analysis of ‡ow rates that is most closely related to the results in this paper is Hobijn and Şahin (2009). They use GMM to estimate average job-…nding and separation rates for a broader sample of countries. Since they focus on average ‡ow hazards, their analysis does not address the dynamic properties of the evolution of unemployment in 23 One exception is Hall [2005], who employs a broader de…nition of unemployment than the usual Current Population Survey de…nition. Consequently he estimates a lower out‡ow rate. 14 these countries. The average ‡ow transition rates that they obtain using their estimation method are almost identical to those documented in Table 2. The time series plotted in Figures 2 and 3 for countries other than the U.S. also are qualitatively similar to previous results based on microdata for individual countries. Our estimates for the U.K. are consistent with the declining employment to unemployment (E– U) and rising unemployment to employment (U–E) transition rates estimated using U.K. Labour Force Survey data from the early 1990s on (Bell and Smith [2002], Gomes [2008], and Petrongolo and Pissarides [2008]). The trends we …nd for Germany are consistent with Bachmann (2005) who uses German social security data to estimate a sharp rise in the E–U transition rate and a decline in the U–E hazard in the early 1990s. In addition, the estimated time series for Spain correspond very closely to those reported in Petrongolo and Pissarides (2008) using Spanish Labor Force Survey data. Reichling (2005) reports estimates of the separation rate for a set of countries (see his Table 5) and also emphasizes that the separation rate is lower in European countries than in the U.S. There are also several cross-country studies that provide structural estimates of search models that include estimated ‡ow hazards. Two examples of these are Ridder and van den Berg (2003) and Jolivet, Postel-Vinay and Robin (2006). Because they are based on structural models, the estimated transition rates in these papers do not correspond exactly to the ‡ow rate concept we use here. However, the qualitative ranking of countries in terms of the levels of in‡ow and out‡ow rates are very similar to ours. For example, Italy is estimated to have the smallest out‡ow rate, the U.S. the highest, with the U.K lying between the U.S. and the Continental European countries. 4 Decomposing Unemployment Fluctuations In this section, we formulate and apply a formal decomposition of changes in unemployment into parts due to changes in the in‡ow and out‡ow rates for each country. Our decomposition allows for deviations of the actual unemployment rate from its ‡ow steady-state value. We show that allowing for such deviations is important for understanding unemployment ‡uctuations in many, especially European, countries. We use the annual time series on in‡ow and out‡ow rates, presented above, to conduct this decomposition. Because we use annual data in what follows, time, t, is denoted in years rather than months in the remainder of this paper. 15 4.1 Analytical Framework As mentioned above, an important aim of this paper is to understand the proximate driving forces behind variation in unemployment rates across countries. As previous literature has shown, such a task is relatively straightforward for the U.S.24 The reason is that unemployment dynamics are uncommonly rapid in the U.S.— that is, st + ft is a relatively large number in the U.S. The formal implication of this is that the rate of convergence of the unemployment rate to its ‡ow steady state value in equation (2), t = 1 e 12(st +ft ) , is very close to one in the U.S. In this case, the unemployment rate can be approximated very closely by its ‡ow steady state value, ut ut = st , and st + ft t 1: (10) As emphasized in Elsby, Michaels and Solon (2009), log di¤erentiation of the latter implies d ln ut (1 ut )[d ln st d ln ft ]: (11) Thus, in countries with labor markets characterized by fast unemployment dynamics, a simple decomposition of unemployment variation presents itself: The relative contributions of the in‡ow and out‡ow rates to unemployment variation can be gleaned from comparing the contemporaneous logarithmic variation in the two ‡ow hazard rates. Based on the evidence we found above, one might anticipate that the approximations that underlie the decomposition of unemployment variation based on (11) work well among the Anglo-Saxon and Nordic economies, which display relatively high rates of in‡ow and out‡ow. However, the evidence also suggests that there is good reason to hesitate in applying equation (11) as a decomposition of unemployment variation in Continental Europe. The reason is that the unemployment ‡ow hazards in these economies are very low, especially relative to the U.S. Inspection of equation (2) reveals that, for Continental Europe, the ‡ow steady-state unemployment rate is therefore likely to be a poor approximation to the actual unemployment rate. Reacting to this, we devise a decomposition of unemployment changes that holds even when unemployment is out of steady state. Our approach uses equation (2) as its starting point. We show in the Appendix that a log-linear approximation to (2) allows us to express 24 See Elsby, Michaels and Solon (2009), Fujita and Ramey (2009) and Pissarides (2009), among others. 16 the log change in the unemployment rate recursively as ln ut t 1 1 ut 1 [ ln st ln ft ] + 1 t 2 ln ut 1 . (12) t 2 This decomposition distinguishes between changes in the steady state due to current changes in the in‡ow and out‡ow rates, and changes in the unemployment rate due to deviations from the steady state caused by past changes in the ‡ow rates. A number of aspects are worth noting about equation (12). First, if unemployment dynamics are very fast, so that st + ft is high and t is close to one for all t, then equation equation (12) reduces to the steady-state decomposition implied by (11). In addition, a particularly intuitive way of understanding (12) is to consider the case where t = for all t. In that case, the log change in the unemployment rate in (12) is a distributed lag of contemporaneous and past log changes in the in‡ow rate st and the ft . This highlights a potential pitfall of applying the steady-state decomposition in (11) to unemployment ‡ows in economies, such as those of Continental Europe, with slow unemployment dynamics: Out of steady state, contemporaneous variation in the unemployment rate is driven both by contemporaneous as well as lagged variation in the ‡ow hazards. We will see that, by ignoring these lag e¤ects, the steady-state decomposition can lead to misleading conclusions on the relative contributions of the in‡ow and out‡ow rate to changes in unemployment. In principle, the non-steady-state decomposition in equation (12) can be used to assess the relative contributions of in‡ow and out‡ow rates for any given change in the unemployment rate at any time for any given country. Clearly, however, given the wealth of information in our dataset, performing such a decomposition for every unemployment episode in every country would be excessive. Thus, we need a method of summarizing the relative contributions of the ins and outs of unemployment. Fujita and Ramey (2009) formulate such a summary method for the U.S. using the steady-state decomposition. Speci…cally, they compute the following values: f = cov( ln ut ; (1 ut 1 ) ln ft ) and var( ln ut ) s = cov( ln ut ; (1 ut 1 ) ln st ) ; var( ln ut ) (13) where a superscript indicates that these are based on the assumption that observed unemployment is closely approximated by its steady-state value. If this assumption holds, f and s should approximately sum to one. We extend Fujita and Ramey’s s to the decomposition of unemployment changes out 17 of steady state based on equation (12). In particular, for each country in our sample we compute f = cov ( ln ut ; Cf t ) , var( ln ut ) s = cov ( ln ut ; Cst ) , and var( ln ut ) 0 = cov ( ln ut ; C0t ) , var( ln ut ) (14) where Cf t , Cst , and C0t denote the respective cumulative contributions of contemporaneous and past variation in the in‡ow rate, the out‡ow rate, as well as the initial deviation from steady state at time t = 0. Consistent with (12), they are de…ned recursively by Cf t = Cst = t 1 ut 1 ) ln ft + (1 t 1 (1 ut 1 ) ln st + and C0t = t 1 (1 t 2) 1 Cf t 1 with Cf 0 = 0, (15) t 2 1 C0t t 2 t 2 Cst 1 with Cs0 = 0, (16) t 2 1 with C00 = ln u0 . (17) t 2 If the decomposition fully captures ‡uctuations in the unemployment rate then 1. 4.2 s+ f + 0 = Accounting for Unemployment Fluctuations in the OECD In order to illustrate why it is important to take into account deviations from steady state for many countries, consider Figure 4. This plots the actual unemployment rate, ut , as well as the ‡ow-steady-state unemployment rate, ut , for the four countries that are studied by Petrongolo and Pissarides (2008), namely France, Spain, the U.K., and the U.S. As has been emphasized in the recent literature, for the U.S. the actual unemployment rate is virtually identical to the steady-state unemployment rate. However, we observe that this is not the case for the other three countries. Another way of seeing this is to look at the second column of Table 3. This lists the standard deviation of the logarithmic deviation of unemployment from steady state for each of the countries in our sample. Table 3 reveals that these deviations tend to be small among Anglo-Saxon economies which have high in‡ow and out‡ow rates, with the exception of the U.K. All other countries exhibit substantial deviations of unemployment from its ‡owsteady-state value. To see what happens when one applies the decomposition based on the steady-state 18 assumption to a country that substantially deviates from steady state, consider the top panel of Figure 5. It depicts the steady-state decomposition of ln ut into parts due to changes in the in‡ow rate, the out‡ow rate, and a residual part that is due to approximation error for France. As can be seen from this …gure, the residuals from the steady-state decomposition are very large. In fact, in this case we observe that f + s = 1:37 rather than 1. Thus, if one calculates s and imputes f = 1 s , then one would underestimate f by 0:37 because of the approximation error induced by deviations from steady state.25 The bottom panel of Figure 5 depicts the non-steady-state decomposition for France. As this …gure shows, the residuals are very small and the magnitudes of the parts due to the ‡ow rates decrease relative to the steady-state decomposition. In the …rst …ve years of the sample a non-trivial part of unemployment ‡uctuations in France was due to the labor market not being in steady state in 1976. This is re‡ected by the contribution of the initial value to the changes in the unemployment rate. The results of our non-steady-state decomposition based on equations (12), (14) and (15) for each country are presented in Table 3. For purposes of comparison, we also include the results from applying the steady-state decomposition. The results in Table 3 are notable from a number of perspectives. First, as anticipated above, we observe that the steady-state decomposition in equation (13) works quite well for economies with fast unemployment dynamics, such as the Anglo-Saxon and Nordic economies, in the sense that s and f approximately sum to one for these economies. In contrast, the steady-state decomposition performs very poorly among economies with slow unemployment dynamics: The sum of the estimated s and f consistently lies above one for these countries, rendering the steady-state decomposition uninformative in determining the driving forces of unemployment variation.26 As anticipated by the results for France in Figure 5, the results of our non-steady-state decomposition reveal that this problem is substantially reduced when we take into account the lag structure of the e¤ects of changes in in‡ow and out‡ow rates on unemployment: The residual variance of log changes in unemployment is closer zero for all countries, and especially so among economies with slow unemployment dynamics. Thus, taking account of the dynamic e¤ects of changes in the unemployment ‡ow hazards on the unemployment rate 25 In their analysis, Petrongolo and Pissarides (2008) implicitly acknowledge this drawback by eliminating the periods for which the deviation of the unemployment rate from its ‡ow steady state value is large. 26 The main reason that the steady-state decomposition consistently explains more than 100% of unemployment variation is that contemporaneous changes in log ‡ow hazards in reality have only a partial contemporanous e¤ect on current unemployment, determined by t 1 < 1 (see equation (12)). The steady-state decomposition erroneously attributes their full e¤ect contemporaneously. 19 is important for inferring the proximate driving forces of unemployment ‡uctuations. In this way, the non-steady-state decomposition summarized in equations (12), (14) and (15) is a useful contribution to the analysis of unemployment ‡ows across countries. The formal results of the non-steady-state decomposition in Table 3 in many ways con…rm the suggestive picture that one can discern from the time series in Figure 2 and 3. Among the Anglo-Saxon economies of Australia, Canada, New Zealand, the U.K. and the U.S., we observe that variation in the out‡ow rate accounts for the majority (though not all) of the variation in the unemployment rate over the respective sample periods. In particular, we …nd something like a 15:85 in‡ow/out‡ow accounting for unemployment variation for these economies. However, variation in the in‡ow rate plays a much larger role among other economies. In fact, we …nd much closer to a 45:55 in‡ow/out‡ow split for the Continental European, Nordic and Japanese economies. These observations are an interesting addition to the debate that has progressed for the U.S. Recent studies have cautioned against the neglect of variation in unemployment in‡ows as an important driving force for changes in unemployment in the U.S. context.27 The results summarized in Table 3 show that this caution resonates all the more if we wish to understand the considerable variation in unemployment rates outside of the U.S. The latter point is important for our understanding of the economics of unemployment. The relative abundance and ease of access to relevant data for the U.S. have led to a wealth of research that documents the proximate driving forces for variation in the U.S. unemployment rate. However, the variation in unemployment in the U.S., though substantially cyclical, is dwarfed by the unemployment experiences among many European economies. A prominent example is Spain, which faced unemployment rates that varied from below 5 percent in the 1970s to 25 percent in the 1990s (see Figure 4). Our results suggest that, in order to understand the substantial variation in unemployment rates among European economies, it is necessary to understand both the variation in the out‡ow rate from unemployment as well as the in‡ow rate. 4.3 Relation to Existing Evidence A number of studies have documented the contributions of changes in in‡ow and out‡ow rates to unemployment variation in the U.S. (see Elsby, Michaels and Solon, 2009; Shimer, 2007; 27 See Braun, De Bock and DiCecio (2006), Elsby, Michaels and Solon (2009), Fujita and Ramey (2009), and Yashiv (2008). 20 and Fujita and Ramey, 2009). A natural question is whether the results of our decomposition are similar to these related …ndings. Recall from Table 3 that we …nd approximately a 15:85 in‡ow/out‡ow contribution to unemployment variation in the U.S. over the period 1968 to 2009 covered by our data. At …rst blush, this …nding can seem di¤erent from those reported in prior research.28 Fujita and Ramey (2009), for example, report a greater role for in‡ows, accounting for as much as 56 percent of unemployment ‡uctuations. The most comparable previous estimates of in‡ow and out‡ow rates to the ones we present here are those derived by Elsby, Michaels and Solon (2009). Using their quarterly analogs of our annual estimates yields an estimated in‡ow contribution of 27 percent over the period 1968 to 2004, a little larger than our estimates based on annual data. This con…rms the intuition foreshadowed in footnote 12 that the use of annual data leads to some smoothing of high frequency ‡uctuations in the in‡ow rate, leading to an understatement of the in‡ow contribution to unemployment variation. However, the understatement is not nearly as severe as one might imagine from a simple comparison with Fujita and Ramey (2009).29 Comparatively little research has studied the contributions of the changes in the in‡ow and out‡ow rates to the ‡uctuations in unemployment across countries. A notable exception is Petrongolo and Pissarides (2008), who study the dynamics of unemployment in three European countries: the U.K., France and Spain. They implement a di¤erent method for treating deviations of actual unemployment from its ‡ow steady state, by dropping observations for which that deviation is large. Despite this, our results line up well with their …ndings for the U.K. and Spain. Using U.K. Labor Force Survey microdata for the period 1993 to 2005, they report an in‡ow contribution of 0.48. Over the same period, we estimate a steady state in‡ow contribution of 0.43 for the U.K. Similarly, using Spanish Labor Force survey data for the period 1987 to 2006, Petrongolo and Pissarides report an average in‡ow 28 An exception is Shimer (2007) who reports an in‡ow contribution of 18 percent for the period 1967 to 2007 using a slightly di¤erent decomposition method (see his Table 1, column 2). Shimer’s method is analogous to ours, except that he uses the sample average ‡ow hazards as the expansion point for his approximation. Speci…cally, he computes two counterfactual unemployment rates. The …rst …xes the in‡ow rate at its sample average and allows the out‡ow rate vary as it did in the data; the second does the opposite. He then decomposes the variance of unemployment into components related to these two counterfactuals. 29 The relatively large in‡ow contributions reported by Fujita and Ramey can be traced to a number of factors. First, their larger estimated in‡ow contributions are based on di¤erent data sources that use longitudinally linked monthly microdata from the Current Population Survey (the so-called gross ‡ows data). Second, Fujita and Ramey decompose changes in steady-state unemployment rather than the realized unemployment series, which in practice accentuates the estimated in‡ow contribution. Third, the sample periods reported by Fujita and Ramey do not coincide with ours. Relaxing all these di¤erences yields an in‡ow contribution of 27 percent. 21 contribution of 0.43. The corresponding value in our calculations is 0.40. It is reassuring that these two perspectives on the data yield similar answers: The OECD data for the U.K. and Spain are annual measures based on the respective quarterly labor force surveys that Petrongolo and Pissarides use. This suggests that there is little slippage in using annual data to measure the ‡ow contributions to unemployment ‡uctuations for these European countries.30 5 Worker Flows So far, we have focused on the ‡ow hazard rates for worker transitions in and out of unemployment. These ‡ow rates, in turn, generate actual worker ‡ows into and out of unemployment. In this …nal part of our analysis, we construct annual time series of worker ‡ows for the fourteen OECD countries in our sample. We use these time series to uncover a very robust stylized fact across countries: In‡ows lead changes in unemployment, while out‡ows lag. 5.1 Analytical Framework The annual ‡ow hazard rates that we presented before can be used to compute the total out‡ows out of unemployment and in‡ows into unemployment. Let Ft be the total number of workers that ‡ows out of the unemployment pool in year t as a fraction of the labor force, and let St be the total in‡ows into unemployment. Given (1), these ‡ows can be written as31 Ft = 12ft ut + t (1 ut ) (ut ut ) , and St = 12st (1 ut ) t ut (ut ut ) . (18) By construction, the ‡ows are such that the increase in the unemployment rate is the di¤er30 Petrongolo and Pissarides’results for France based on unemployment claims data do not line up as well with our estimates. They report an in‡ow contribution of 0.2 for the years 1991 to 2007, smaller than our analogous estimate of 0.5. We suspect that this discrepancy arises because the OECD data that underlie our estimates are based on French Labor Force Survey data, rather than the claimant data used by Petrongolo and Pissarides. This is consistent with results reported by Petrongolo and Pissarides’ for the U.K. Their measured in‡ow contribution based on U.K. unemployment claims data for the period 1993Q2 to 2005Q3 is 0.25, much less than their estimate of 0.48 based on the U.K. Labor Force Survey. R t+12 31 The total in‡ow into unemployment can be derived as St = st t [1 u ( )] d = R t+12 st t 1 ut e (st +ft ) (ut ut ) d = 12st (1 ut ) u (u u ), where the second equality follows t t t t from solving the di¤erential equation for the unemployment rate (1) forward. Analogously, the total outR t+12 R t+12 ‡ow from unemployment can be derived as Ft = ft t u ( ) d = st t ut + e (st +ft ) (ut ut ) d = 12ft ut + t (1 ut ) (ut ut ). 22 ence between the in‡ows and the out‡ows, i.e. ut = St Ft . (19) A large number of studies (Darby, Haltiwanger, and Plant [1986], Davis [1987, 2006], Blanchard and Diamond [1990], Merz [1999], and Fujita and Ramey [2009]) has noted two key stylized facts about worker ‡ows in the U.S. The …rst is that gross ‡ows increase when unemployment increases. The second is that changes in in‡ows, St , tend to lead the changes in out‡ows, Ft , as well as changes in the unemployment rate, ut . In what follows, we con…rm that these stylized facts for the U.S. also hold for many other developed economies. 5.2 Evidence on Worker Flows in the OECD Figures 6 and 7 depict the time series for our estimates of the number of workers ‡owing into unemployment, St , and the number ‡owing out, Ft , together with the unemployment rate for each country in our sample. In line with the di¤erences in the ‡ow hazard rates st and ft between Anglo-Saxon Countries and Continental Europe, we …nd very large di¤erences in average worker ‡ows between these groups of countries as well. The second column of Table 4 contains the average worker ‡ows for all countries in our sample. These echo the stark geographical partitioning of labor market ‡ows that we detailed above for the ‡ow hazard rates across countries. Anglo-Saxon countries exhibit annual worker ‡ows in and out of unemployment that comprise more than 15 percent of the labor force. The U.S. is once more a conspicuous outlier with average annual worker ‡ows of 40 percent of the labor force. At the opposite end of the spectrum again lie the economies of Continental Europe with worker ‡ows that typically account for less than 10 percent of the labor force. In addition, a prominent visual pattern to the timing of changes in these ‡ows emerges from Figures 6 and 7. It can be seen that increases in the unemployment rate are often preceded by rises in the number of workers ‡owing into the unemployment pool, followed by a commensurate rise in the out‡ow. Thus, in most countries we observe that gross ‡ows increase when unemployment rises, and that in‡ows tend to lead out‡ows, just as observed in U.S. data. This observation can be seen more formally using a simple correlation analysis. The last six columns of Table 4 report the contemporaneous, lead, and lag correlations between the changes in the ‡ows and changes in the unemployment rate. These correlations tell the following story. In the year prior to a rise in unemployment, in‡ows into the unemployment 23 pool rise— the one year lead correlation between changes in in‡ows and contemporaneous changes in unemployment is positive in almost all economies. Moreover, in‡ows remain high in the year that unemployment rises— the contemporaneous correlation between changes in in‡ows and changes in unemployment are positive for all countries. In the year following an unemployment ramp up, out‡ows begin to rise— the one year lag correlation between changes in out‡ows and contemporaneous changes in unemployment is positive in almost all economies. Thus, just like studies that use monthly data for the U.S., we …nd that changes in in‡ows tend to lead changes in the unemployment rate in the annual data we use. What emerges from our results on worker ‡ows is that, even though the OECD economies have very di¤erent levels of ‡ows, the cyclical behavior of worker ‡ows across countries is very similar. Economic downturns, in which the unemployment rate increases, …rst see an increase in workers ‡owing into unemployment, rather than a decline in the number of workers ‡owing out of it. Subsequently, the out‡ows increase as the economy recovers. These results have stark implications for popular models of the aggregate labor market. An important recent trend in these models has been to assume that in‡ow rate st into unemployment is constant over the business cycle (Hall [2005a,b], Blanchard and Gali [2006], Gertler and Trigari [2006], Krusell, Mukoyama, and Şahin [2010], for example). In the context of these models, increases in unemployment during recessions are driven entirely by declines in the job …nding hazard, ft . This assumption has important implications for the dynamic properties of worker ‡ows over the cycle. A rich literature on unemployment ‡ows in the U.S. has emphasized that such models imply that increases in the unemployment rate are preceded by reductions in the number of workers ‡owing out of the unemployment pool, Ft (Darby, Haltiwanger, and Plant, 1985, 1986; Blanchard and Diamond, 1990; Davis, 2006). Consequently, reductions in out‡ows are predicted to lead increases in the unemployment rate in this class of models. In addition, because the in‡ow rate st is assumed constant, these models also imply that the number of workers ‡owing into the unemployment pool St will decline modestly in the wake of a recession as the employment rate 1 ut falls, so that changes in St lag changes in the unemployment rate. Thus, models that assume a constant in‡ow rate have two important predictions with regard to worker ‡ows: (i) when unemployment goes up gross worker ‡ows decline, and (ii) out‡ows lead changes in unemployment, while in‡ows lag. The studies of worker ‡ows in the U.S. cited above have established that neither of these theoretical implications is borne out by the data for the U.S. This has led researchers to 24 challenge the empirical relevance of such models in the U.S. context (Davis [2006]; Fujita and Ramey [2009]; Ramey [2008]). Our results reveal that the observation of increased in‡ows as a leading indicator of increased unemployment, far from being unique to U.S. data, is something close to a stylized fact for all modern developed labor markets. These results con…rm and reinforce earlier …ndings based on earlier periods for subsets of the European countries that we study. Using Portuguese microdata from the early 1990s, Blanchard and Portugal (2001) emphasize that the levels of worker ‡ows are much lower in Portugal relative to the U.S. Similar …ndings are reported by Bertola and Rogerson (1997, Table 3) who document reduced worker ‡ows in Italy and Germany relative to Anglo-Saxon counterparts using OECD data for 1988. Using data from France, Germany, Spain, and the U.K. up to the early 1990s, Balakrishnan and Michelacci (2001) and Burda and Wyplosz (1994) have highlighted that both in‡ows and out‡ows increased as European unemployment soared in the 1970s and 1980s, with increased in‡ows leading increased unemployment. 6 Conclusion Our analysis of publicly available data from the OECD provides four contributions to our understanding of unemployment ‡ows. First, we present a method of estimating the ‡ow hazard rates for entering and exiting unemployment across fourteen developed economies, building on the method pioneered by Shimer (2007) for the U.S. An important bene…t of this methodology is that it can be extended to estimate unemployment ‡ows for additional economies over longer time periods as more data becomes available. Application of this method to fourteen OECD countries uncovers a stark contrast in average ‡ow hazard rates between Anglo-Saxon, Nordic, and Continental European countries. Anglo-Saxon and Nordic labor markets are characterized by high unemployment in‡ow and out‡ow rates, while these ‡ow hazard rates in Continental European economies are generally less than half of those in their Anglo-Saxon counterparts. Notably, results for the U.S. which have received much attention in recent literature are a conspicuous outlier among developed economies, with in‡ow and out‡ow rates that are at least …fty percent larger than the remaining economies in our sample. These results strengthen and extend earlier work that has diagnosed European labor markets as sclerotic based on similar …ndings for subsets of the economies we study. Our second contribution is to devise a decomposition of unemployment ‡uctuations into parts due to changes in in‡ow and out‡ow rates that can be applied to countries with very 25 di¤erent unemployment dynamics. Conventional decompositions applied to U.S. data have exploited the fact that unemployment is closely approximated by its steady-state value in the U.S. (Elsby, Michaels, and Solon [2009]; Fujita and Ramey [2009]). For many OECD countries outside the U.S., however, we demonstrate that unemployment deviates considerably from its steady-state level. Consequently we show that conventional decompositions lead to misleading results on the relative importance of ‡uctuations in in‡ow and out‡ow rates for the dynamics of the unemployment rate. The results from applying our alternative decomposition reveal approximately a 15:85 in‡ow/out‡ow contribution to unemployment variation among Anglo-Saxon countries, whereas in most European countries the split is much closer to 45:55. Our third contribution is based on a simple correlation analysis of changes in worker ‡ows and changes in the unemployment rate over time. For all countries in our sample, worker ‡ows tend to increase when unemployment increases. Moreover, we …nd that, in almost all countries in our sample, changes in in‡ows into unemployment lead changes in the unemployment rate, while changes in out‡ows tend to lag unemployment variation. This con…rms and reinforces the conclusions of previous literature based on a smaller set of countries, suggesting that these …ndings for worker ‡ows are a stylized fact of modern labor markets. Stepping back, our empirical …ndings provide an important perspective on the theoretical literature on unemployment ‡ows that has evolved in recent years. Much of this recent literature has assumed the in‡ow rate into unemployment to be an exogenous constant. As a reaction to this, a number of studies of U.S. unemployment ‡ows has cautioned against this trend (Elsby, Michaels, and Solon [2009], Fujita and Ramey [2009], and Yashiv [2007]). A fourth contribution of the results of this paper is that the same conclusion extends to the analysis of labor markets in a wide range of developed economies, and especially so if one is interested in understanding the substantial changes in unemployment rates in Europe. 26 References [1] Albaek, Karsten and Bent E. 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De…ne the fraction of the labor force that has been unemployed in month t for less than a month as u1;t , more than one but less than three months as u3;t , more than three but less than six months as u6;t , more than six but less than twelve months u12;t , and <3 more than 12 months as u1;t . Then u<1 t = u1;t , ut = u1;t +u3;t , etc. Given this data and quarterly data for the unemployment rate, the four estimates of the out‡ow rate are ft<1 = ln (u3;t + u6;t + u12;t + u1;t ) + ft<3 = (ln (u6;t + u12;t + u1;t ) ft<6 ft<12 = = (ln (u12;t + u1;t ) (ln (u1;t ) ln ut ln ut ln ut 2 1 ln (u1;t + u3;t + u6;t + u12;t + u1;t ) + ln ut 3 3 3 , 3 ) =3, 6 ) =6, and 12 ) =12. (20) In practice, we have annualized data for the duration distribution of unemployment for which we do not know in which month of the year they are measures. Therefore, for our estimates of the out‡ow rates average the lagged unemployment rates, ut 3 , ut 6 , and ut 12 over the four quarters in the year for which the out‡ow rate is estimated. Asymptotic Distribution of Out‡ow Rate Estimates. We do not observe the u1;t , u3;t , u6;t , u12;t , and u1;t . Instead we observe their sample approximations based on the labor force surveys of the di¤erent countries. Let the sample size of the labor force survey be nt and let u bd;t d = 1; 3; 6; 12; 1 be the estimated fractions from the labor market survey. Moreover, we also observe the estimated unemployment rate u bt , not only at t but also at u bt 3 , u bt 6 , and u bt 12 . We assume that the sample of individuals in the labor force survey is independent across these realizations of the unemployment rate and is of the same size nt = nt s where s = 3; 6; 12 and the sample sizes are as given in Table 1. These sample approximations have a joint multinomial distribution, such that E (b ud;t ) = ud;t and E (b ut and var (b ud;t ) = as well as var (b ut s) = 1 ut n 1 ud;t (1 n s (1 ut s) ut = = ut s for s = 0; 3; 6; 12. ud ) and cov (b ud ; u bd0 ) = and De…ne the vector s) cov (b ut ; u bt and cov (b ud;t ; u bt s) Vt = " (d) Vt 03 1 u bd u bd0 n (22) = 0 for s = 3; 6; 12, = 0 for s 6= 0. u1;t u3;t u6;t u12;t u1;t ut and the covariance matrix s) (21) 5 31 05 3 (u) Vt # 3 , (23) (24) ut 6 ut 12 0 (25) (26) where (d) Vt and 2 6 6 =6 6 4 u1;t (1 u1;t ) u1;t u3;t u1;t u6;t u1;t u12;t u1;t u1;t u1;t u3;t u3;t (1 u3;t ) u3;t u6;t u3;t u12;t u3;t u1;t u1;t u6;t u3;t u6;t u6;t (1 u6;t ) u6;t u12;t u6;t u1;t u1;t u12;t u3;t u12;t u6;t u12;t u12;t (1 u12;t ) u12;t u1;t u1;t u1;t u3;t u1;t u6;t u1;t u12;t u1;t u1;t (1 u1;t ) (u) Vt 2 =4 ut 3 (1 ut 3) 0 0 0 ut 6 (1 ut 0 0 6) 0 ut 12 (1 ut 12 ) 3 5 3 7 7 7 , (27) 7 5 (28) and the o¤-diagonal zero matrices re‡ect that we assume independence of di¤erent samples in the labor force surveys. Assuming a relatively large sample of the labor force survey, nt , we can approximate p nt (b ut D ut ) ! N (0; Vt ) (29) 1 Vt nt (30) such that bt u N ut ; We are not interested in this distribution. Instead, we are interested in three estimates of the out‡ow rate, each of which is a consistent estimate if there is no duration dependence in the out‡ow rate during the …rst year of unemployment. De…ne the vector ft = ft<1 ft<3 ft<6 ft<12 0 (31) then we will use the Delta-method to derive the asymptotic distribution of b f for n ! 1.32 In order to do so, we consider the following gradient. 2 30 2 0 0 0 3ut 1 6 2 7 0 0 0 6 3ut ut u<1 7 t 6 2 7 1 1 6 3u 7 0 0 3(ut u<3 6 t ut u<1 7 t t ) 6 2 7 1 1 1 0 6 7 <1 <3 <6 @ft 3u t u u 3 u u 6 u u t ( t t ) ( t t ) 7 t = 6 (32) Df;t = 0 6 7 2 1 1 1 1 @ut 6 3ut ut u<1 7 <3 <6 <12 3(ut ut ) 6(ut ut ) 12(ut ut ) 7 t 6 1 1 6 7 0 0 6 7 3ut 3 3ut 3 6 7 1 0 0 0 4 5 6ut 6 1 0 0 0 12ut 12 This allows us to write the approximate distribution of b ft as 32 b ft N 1 ft ; Df;t Vt D0f;t n (33) Note that we assume that the level of unemployment, ut , is measured without any measurement error. 32 It is this distribution that we are going to use for the derivation of our hypothesis test as well as for the calculation of the "optimal" weighting of the di¤erent out‡ow rate estimates for our estimated out‡ow rate. Hypothesis Test for No Duration Dependence. If there is no duration dependence, then it is the case that H0 : ft = f , where f is scalar and is a vector with ones (34) which is the null-hypothesis of interest. For our 2 1 Mf = 4 0 0 test, we de…ne the matrix 3 0 0 1 1 0 1 5 0 1 1 Under the null-hypothesis, it is the case that Mf b ft N 1 0; Mf Df;t Vt D0f;t M0f n (35) (36) De…ne the Choleski-decomposition matrix C as Mf Df;t Vt D0f;t M0f = Ct C0t Then p nCt 1 Mf b ft (37) N (0; I3 ) (38) Remember that the sum of squares of 3 independent standard normally distributed random variables is chi-squared distributed with 3 degrees of freedom. Hence, when we de…ne gt = nb ft0 M0f C0t 1 Ct 1 Mf b f = nb ft0 M0f Mf Df;t Vt D0f;t M0f then, under the null it is the case that gt 2 (3) . (39) 1 Mf b ft (40) Optimal Weighting of Estimated Out‡ow Rates. For those countries for which we do not reject the null-hypothesis for reasonably large sample sizes and for the majority of the years, we then have to decide on the optimal weighting of the estimated …nding rates. That is, we want to …nd vector with weights, w, and estimate such that fbt = wt0 b ft wt0 = 1 33 (41) (42) and that, given this constraint, w minimizes Vf;t = wt0 Df;t Vt D0f;t wt (43) Let us …rst take care of the restriction. For this purpose, de…ne such that 2 3 2 0 6 0 7 6 7 6 = 6 4 0 5+4 1 et = e1 + Mw w wt 0 wt<1 wt<3 wt<6 et = w 1 0 0 1 (44) 3 0 0 7 7w e 1 5 t 1 0 1 0 1 (45) (46) Then the objective function can be written as et + w e t0 M0w Df;t Vt D0f;t Mw w et Vf;t = e01 Df;t Vt D0f;t e1 + 2e01 Df;t Vt D0f;t Mw w (47) which yields that the set of optimal weights is et = w and thus wt = e1 1 M0w Df;t Vt D0f;t Mw M0w Df;t Vt D0f;t e1 1 Mw M0w Df;t Vt D0f;t Mw (48) M0w Df;t VD0f;t e1 (49) Note, this only imposes that the weights add up to one but not that they are positive. Dynamic Decomposition of Changes in Unemployment. Note that the unemployment rate at the end of year t evolves according to ut = t ut + (1 t ) ut 1 ; (50) where t 1 e 12(st +ft ) is the annual rate of convergence to steady state, ut st = (st + ft ) is the steady state unemployment rate, and st and ft are respectively the monthly unemployment in‡ow and out‡ow hazard rates in year t. A log–linear approximation to (50) around st = st 1 , ft = ft 1 , and ut 1 = ut 1 is given by ln ut ln ut 1 + t 1 ln ut ln ut ln ut 1 + t 1 1 1 ut [ 1 + (1 ln st t 1) ln ut ln ft ] + (1 1 ln ut t 1) (51) 1 ln ut 1 ln ut 1 : (52) If unemployment is always in steady state, then ln ut = ln ut 1 ut 1 [ ln st ln ft ] (53) However, if unemployment deviates from steady state, then this approximation is not appropriate. 34 In that case, it is worthwhile to realize that ln ut ln ut 1 = t 1 ln ut ln ut 1 t 1 ln ut = t 1 ln ut ln ut 1 t 1 ln ut = t 1 (ln ut ln ut ) + t 1 (ln ut ln ut 1 ln ut ln ut 1 (54) 1 + t 1 (ln ut ln ut 1) 1) such that t 1 ln ut 1 and thus (ln ut (ln ut t 1 ln ut ) = 1 ln ut ) (55) ln ut (56) t 1 t 1 Substituting this into (51) we can write ln ut t 1 1 ut 1 [ ln st ln ft ] + 1 t 2 ln ut 1 . (57) t 2 Which allows us to do the decomposition out of steady state. E¤ect of Inclusion of Non-Participants. Equation (1) does not take into account ‡ows that stem from people that are not-in-the-labor-force (NILF) that start looking for a job and become unemployed. It also does not include persons that ‡ow out of unemployment as well as out of the labor force. In addition, it normalizes the size of the labor force to one, thus not taking into account labor force growth. We have actually calculated a set of results that allow for these things, but for the sake of clarity have abstracted from them in the analytical framework applied here. It turns out that including these things does not a¤ect the results much. Below we explain why. The …rst thing to note is that our estimates of the out‡ow rate out of unemployment solely use unemployment data and are not a¤ected by the simplifying assumptions described above. The out‡ow rate basically determines the total out‡ows out of unemployment. Since the change in the number of unemployed persons is the di¤erence between the in‡ows and the out‡ows, this implies that the total in‡ows into unemployment are also not sensitive to these simplifying assumptions. The only thing that is a¤ected is the in‡ow rate. In our framework, the in‡ow rate re‡ects the fraction of employed persons that ‡ows into unemployment. Without the simplifying assumption the in‡ow rate would re‡ect the fraction of persons that are either employed or NILF that ‡ow into unemployment. In e¤ect, if one would drop our simplifying assumption one would …nd a lower in‡ow rate that is scaled down by the labor force participation rate. For all countries in the sample, labor force growth is so small that it is swamped by the magnitude of worker ‡ows. Hence, the results presented here turn out to be almost identical to the ones that take into account labor force growth. 35 36 http://stats.oecd.org/mei/default.asp?lang=e&subject=10. Note: Sample sizes include non-labor force members. Information based on metadata for OECD (2008b), available at United States: Data comes from the monthly CPS. Each month about 60,000 households are interviewed for the survey. (We use n = 130; 000.) use n = 120; 000.) United Kingdom: Survey is conducted continuously throughout the year. In any three-month period, 57,000 households are interviewed (120,000 persons). (We Sweden: Participation is voluntary. Every month about 20,000 persons are included in the sample. (We use n = 20; 000.) n = 185; 000.) Spain: Sample includes 74,000 households; however in practice only about 65,000 households (i.e. approximately 185,000 persons) are interviewed. (We use Portugal: Sample size approximately 21,000 households. (We use n = 52; 500.) Norway: Sample size is 12,000 households (24,000 persons). Includes all armed forces.(We use n = 24; 000.) are excluded from the sample. (We use n = 40; 000.) New Zealand: Obtained from 16,000 private dwellings (approximately 32,000 persons) each quarter. From 2nd quarter of 1995, residents in non-private households Japan: The survey covers a sample of 40,000 households. (We use n = 100; 000.) Italy: The sample was doubled in April 1990 from 12,000 to 24,000 households. (We use n = 60; 000.) Ireland: Sample of 39,000 households is surveyed each quarter. Includes career military living in private households. (We use n = 97; 500.) Germany: The average quarterly sample in 2005 comprises about 165,000 respondents. (We use n = 165; 000.) n = 150; 000.) Previously, the Survey was annual. In March 2001, 75,000 households responded to the survey covering 150,000 persons which includes armed forces. (We use France: Data are compiled from various sources including the Labor Force Survey (“Employment Survey”). Since 2003, the Survey is quarterly and continuous. Canada: Approximately 56,000 households since 1976. (We use n = 135; 000.) Australia: Survey covers about 0.5% of Australia’s population. (We use n = 57; 000.) Table 1: Approximate sample sizes of Labor Force Surveys 37 1986 1977 1976 1983 1968 Portugal Spain Sweden United Kingdom United States 0% 0% 0% 0% 0% 0% 1% 1% 5% 2% 3% 0% 0% 0% included P-value f <1 0% 1% 1% 5% 10% 1% 0% 0% 9% 11% 2% 7% 0% 0% excluded P-value f <1 Rejected? H0 6.1% 7.7% 4.3% 15.4% 6.2% 4.1% 6.4% 3.3% 9.8% 10.8% 8.3% 8.1% 8.5% 7.1% rate (u) Unemployment 56.5% 13.9% 29.2% 6.3% 6.3% 38.5% 28.5% 18.9% 4.3% 5.9% 6.0% 7.7% 26.1% 22.8% rate (f ) Out‡ow Sample averages 3.6% 1.0% 1.2% 1.1% 0.4% 1.6% 1.7% 0.6% 0.4% 0.6% 0.5% 0.7% 2.4% 1.7% rate (s) In‡ow to H0 : ft<3 = ft<6 = ft<12 : H0 : ft<1 = ft<3 = ft<6 = ft<12 : The hypothesis ‘f <1 excluded’refers signi…cance level. The rejection of the null of no duration dependence is based on the second hypothesis and determined at a 1% the sample size reported in Table 1. The hypothesis ‘f <1 included’refers to Note: Reported P-values are sample averages for the test for no duration dependence over the sample period, based on the application of 1983 1983 Italy Norway 1983 Ireland 1986 1983 Germany New Zealand 1975 France 1977 1976 Japan 1978 Australia sample Start of Canada Country Test for no duration dependence Table 2: Test for no duration dependence and summary statistics on unemployment and ‡ow rates 38 9.0% 1.3% 1.1% 0.4% 13.0% 9.9% 1.5% 3.0% 0.2% Japan New Zealand Norway Portugal Spain Sweden United Kingdom United States 8.5% Germany Italy 5.1% France 14.2% 0.6% Canada Ireland 1.3% % dev. from ss Australia Country std. dev. of 0.85 0.91 0.50 0.76 0.94 0.55 0.90 0.61 1.08 0.80 0.92 0.75 0.80 0.96 f 0.16 0.22 0.53 0.50 0.42 0.46 0.13 0.48 0.43 0.77 0.56 0.62 0.24 0.11 s -0.01 -0.12 -0.03 -0.25 -0.36 0.00 -0.03 -0.09 -0.51 -0.57 -0.48 -0.37 -0.05 -0.07 residual Steady-state decomposition 0.85 0.85 0.50 0.57 0.68 0.54 0.88 0.56 0.83 0.47 0.56 0.54 0.79 0.93 f 0.16 0.17 0.51 0.43 0.32 0.45 0.13 0.45 0.15 0.55 0.47 0.45 0.23 0.10 s 0.00 0.00 0.00 0.01 0.00 0.01 0.00 0.00 0.05 0.00 0.00 0.02 0.00 0.00 0 -0.01 -0.02 -0.01 -0.01 0.00 0.00 -0.01 -0.01 -0.03 -0.02 -0.03 -0.01 -0.02 -0.03 residual Non-steady-state decomposition Table 3: Decompositions of unemployment ‡uctuations 39 Note: The column 1 2 (F + S) .2 -.4 .0 .1 -.1 .1 .0 .1 -.4 .0 -.1 -.1 -.2 -.6 k= 1 -.1 -.1 .4 -.1 -.2 .3 -.2 .1 -.2 -.2 -.2 -.1 .0 -.4 .3 .4 .8 .5 .6 -.2 .2 .0 .5 .7 .5 .6 .6 .5 k=1 Ft+k ) k=0 corr ( ut ; .5 -.1 .3 .7 .3 .2 .3 .2 -.1 .3 .6 .2 .0 -.3 k= 1 .4 .2 .7 .6 .5 .4 .2 .3 .2 .6 .5 .7 .3 .2 -.2 .2 .6 .2 .2 -.3 -.1 -.1 .1 .4 -.2 -.1 .3 .1 k=1 St+k ) k=0 corr ( ut ; list the average of the average in and out‡ow rates over the sample period. 40.0% United States 17.9% Norway 11.7% 19.5% New Zealand United Kingdom 7.0% Japan 13.3% 4.8% Italy Sweden 6.4% Ireland 4.6% 5.9% Germany 10.5% 7.3% France Spain 25.9% Canada Portugal 18.4% (F + S) Australia Country 1 2 Table 4: Average worker ‡ows and correlations with changes in the unemployment rate Figure 1: Average in- and out‡ow rates across countries. 40 Figure 2: In- and out‡ow rates (log-scale in percentages) for Anglo-Saxon and Nordic countries, and Japan 41 Figure 3: In- and outlfow rates (log-scale in percentages) for Continental European countries. 42 Figure 4: Actual versus steady state unemployment in four illustrative countries. 43 Figure 5: Steady-state versus non-steady-state decomposition of unemployment ‡uctuations for France. 44 Figure 6: Unemployment rate and worker ‡ows, Anglo-Saxon and Nordic countries, and Japan. 45 Figure 7: Unemployment rate and workers ‡ows, Continental European countries. 46