Board of Governors of the Federal Reserve System
International Finance Discussion Papers
Number 863, June 2006Screen Reader Version*
NOTE: International Finance Discussion Papers are preliminary materials circulated to stimulate discussion and critical comment. References to International Finance Discussion Papers (other than an acknowledgment that the writer has had access to unpublished material) should be cleared with the author or authors. Recent IFDPs are available on the Web at http://www.federalreserve.gov/pubs/ifdp/. This paper can be downloaded without charge from the Social Science Research Network electronic library at http://www.ssrn.com/.
Abstract:
This paper studies the transmission of volatility and trading activity in the foreign exchange market across trading regions for the eurodollar and dollaryen currency pairs, using highfrequency intraday data from Electronic Broking Services (EBS). In contrast with previous studies that use indicative quote frequency to proxy for trading activity, we use actual regional trading volume to identify five distinct trading regions in the foreign exchange market: Asia Pacific, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America. Based on realized volatility computed from highfrequency data and a regional volatility model, we find statistically significant evidence for volatility spillovers at both the ownregion and the interregion levels, but the economic significance of ownregion spillovers is much more important than that of interregion spillovers. We also examine the transmission of trading activity (trading volume and number of transactions) across the five trading regions and find similar results to those for volatility, but the economic significance of ownregion spillovers is even more dominant.
Keywords: Exchange rate, volatility, trading volume, highfrequency data
JEL classification: F31, G15
The informational linkages across financial markets have received increasing attention in the international finance literature. Such linkages across markets are mostly manifested by the transmission of both volatility and trading activity. In this study, we examine volatility and trading activity transmission in the global interdealer foreign exchange market. This paper uses a dataset of trading volume and prices in spot eurodollar and dollaryen trading from Electronic Broking Services (EBS) covering the period from January 1999 to February 2004. This EBS dataset has several important advantages. First, the EBS dataset consists of transactable quotes, as opposed to indicative quotes from Reuters used in previous studies, as well as actual trading volume which was previously not available. Second, EBS has become the major trading platform for the two most traded currency pairs, the yen and the euro, making the results based on this dataset a true representation of the behavior of global interdealer foreign exchange markets.
We investigate volatility and trading activity (measured by both trading volume and number of transactions) spillovers across three major trading areas (centered in Tokyo, London, and New York) for two currency pairs (eurodollar and dollaryen). We are interested in the extent to which changes in foreign exchange volatility in one market influence that in the next market, and whether changes in trading activity in one market are positively related to changes in trading activity in the next market. Specifically, this paper explores several issues as follows.
First, this paper uses a new dataset from EBS on regional trading volume to classify different trading regions in the global foreign exchange market for the eurodollar and dollaryen currency pairs. Trading volume is a better measure of trading activity than quote frequency used in previous studies (e.g., Melvin and Yin (2000) and Melvin and Melvin (2003)). EBS records regional trading volume by transactions that occur between pairs of the three physical locations of the EBS computer centers: Tokyo, London, and New York. These computer centers are linked together in real time, and EBS classifies the origin of each trade from the physical location of the computer center that serves each region.^{1} Based on our assessment, we define five distinct trading regions: Asia Pacific, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America.
Second, we test two competing hypotheses on volatility clustering as first studied in Engle, Ito, and Lin (1990): the heat wave hypothesis refers to volatility clustering at a regional levela high (low) volatility in a region today tends to be followed by a high (low) volatility in the same region on the following day. The competing meteor shower hypothesis refers to volatility clustering at a global levela high (low) volatility in one region today tends to be followed by high (low) volatility in the next trading region. Engle, Ito, and Lin (1990) find support for the meteor shower effect, while Baillie and Bollerslev (1990), Hogan and Melvin (1994), and Melvin and Melvin (2003) report evidence for the heat wave effect. These conflicting results may reflect differences in their sample period, mostly very short, and sampling frequency. This paper contributes to this research area by using highfrequency intraday data with a longer and more recent sample period to test the heat wave and meteor shower hypotheses. In addition, our measure of volatility is based on highfrequency data, thus allowing us to treat volatility as observable as opposed to latent (Andersen, Bollerslev, Diebold and Labys (2001)), which make our results independent of statistical models for volatility (e.g., GARCH and stochastic volatility models).
Third, we explore the spillovers of trading activity across regions for the two currency pairs. To our knowledge, this paper is the first to study trading activity transmission in the foreign exchange market. We use both trading volume and number of transactions to measure trading activity. Previous studies have attempted to proxy for actual transaction volume data by using futures exchange volume data (e.g., Chaboud and LeBaron (2001)) or the frequency of indicative quotes on Reuters data screens (e.g., Melvin and Yin (2000)), but these measures have already been shown to be poor proxies. Since informational linkages are manifested by both volatility and trading activity, we use trading activity as a robustness check for the information transmission dynamics. We also repeat the test with number of transactions, as Jones, Kaul, and Lipson (1994) find that in the case of equity markets the key information in trading volume is captured by number of transactions.
We estimate a regional volatility model by allowing each region's volatility to depend on its own past volatility and other regions' past volatilities, similar to Melvin and Melvin (2003). We find statistically significant evidence for both the heat wave and meteor shower effects for both currency pairs, but the heat wave effect is much more important economically than the meteor shower effect. We also estimate a regional model for trading activity similar to that of volatility. Consistent with results on volatility, we find statistically significant evidence for both the heat wave and the meteor shower effects. Again, we find that the heat wave effect is much more important economically than the meteor shower effect. The similarity of our results based on a longer and more recent sample period for both volatility and trading activity confirms the robustness of our findings.
The remainder of the paper is organized as follows. Section 2 describes data sources. Empirical models and empirical results are in Section 3. Section 4 presents conclusions of this paper.
The EBS system operates 24 hours a day and is widely used by dealers in all major foreign exchange trading centers. The electronic limit order book allows speedy transactions between dealers, usually completed within one second. We study the eurodollar and dollaryen currency pairs. The sample period is from January 4, 1999 through February 19, 2004. Our dataset is proprietary and confidential. It consists of minutebyminute foreign exchange midquotes, minutebyminute trading volume (expressed in base currency), and minutebyminute number of transactions.^{2} The quotes are all firm, i.e., they are transactable prices, rather than indicative quotes which do not present a binding commitment to trade at these prices. The data used in this paper present an aggregate and purely numerical picture of the EBS system, and do not contain any information on the identity of any market participants. To preserve data confidentiality, we show trading volume and number of transactions data in index form rather than the actual values. For each currency pair, trading volume and number of transactions are normalized by their respective average values over the whole sample period such that the average values are set at 100.
Although the FX market is a 24hour market, previous studies have documented strong intraday pattern of volatility and proxies for trading activity, reflecting the distinct opening and closing times in the major trading centers (e.g., Baillie and Bollerslev (1990), Melvin and Melvin (2003), and Ito and Hashimoto (2004)). The two panels in Figure 1 show trading volume by region for eurodollar and dollaryen respectively (indexed to average total trading volume across all regions), as reported in the EBS data. EBS records regional trading volume by transactions that occur between pairs of the three physical locations of the EBS computer center: Tokyo (TY), London (LN), and New York (NY). These computer centers are linked together in real time, and EBS classifies the origin of each trade from the physical location of the computer center that serves each region. All dealers located in the Asia Pacific area are served by the computer center in Tokyo and all trades are recorded as originating from Tokyo. The computer center in London serves dealers that are located in Europe, the Middle East, and Africa, and the computer center in New York serves dealers that are located in both North and South America. Dealers that are served by one of these three computer centers observe the same information simultaneously and can trade with any dealers, independent of the region that is served by the computer center. If a transaction is executed between two counterparties with London origin, it is recorded as a LN_LN transaction. If the two counterparties are from London and New York origins, it is recorded as a LN_NY transaction, and so on. Since EBS defines 5 p.m. New York time as the end of a trading day, we use New York time zone (EST) as the base time zone throughout the paper.
In both currency pairs, the patterns of trading volume are characterized by sharp spikes. For eurodollar as shown in Panel A, the two spikes occur around 8:30 a.m. (New York time) when most U.S. macroeconomic data are released, and 10 a.m. (New York time) when most foreign exchange options expire. Another spike occurs at 11 a.m. (4 p.m. London time), the time of the Reuters fixing often used to express international bond and stock indices in dollars. For dollaryen in Panel B, the same three spikes in volume occur as in eurodollar. The tallest spike in dollaryen trading volume occurs around 7:55 p.m. New York time (9:55 a.m. Tokyo time), however, marks the daily fixing in Tokyo by Bank of Tokyo Mitsubishi.
To identify geographic opening and closing periods, we use 24hour regional mean trading volume as a threshold signaling the open and close. We identify five distinct time periods: three periods when only Asian or European or American traders are actively trading, plus two trading overlap periods, the AsiaEurope overlap trading as well as the EuropeAmerica overlap trading. Therefore, we classify daily trading hours into five different regions: Asia Pacific (Tokyo), the AsiaEurope overlap (Tokyo/London), Europe (London), the EuropeAmerica overlap (London/New York), and America (New York).^{3} Our method is similar to Melvin and Melvin (2003), but there are two important improvements. First, we use real trading volume in determining the opening and closing hours for each region while they use frequency of indicative quotes as a proxy for trading volume and liquidity supply.^{4} Another improvement we make over the method used in Melvin and Melvin (2003) is that we consider both regional time series and crosssectional mean trading volume in determining opening and closing hours. Specifically, we calculate the time series average trading volume for each 30minute interval for each region, and compare it with the 24hour mean trading volume (mean of the 30minute mean volume) for each region. In order to control for the regional differences in trading volume, we divide the difference between the time series average trading volume and 24hour mean trading volume by the 24hour mean trading volume. At any particular point in time, the region with the largest positive ratio is considered open. Figure 2 summarizes our assessment of reasonable opening and closing hours for each of the five geographic trading regions, taking into account the daylight saving time shifts in Europe and America.
The work by Andersen, Bollerslev, Diebold and Labys (2001) shows that a lowfrequency volatility measure can directly be computed from highfrequency data (realized volatility). Realized volatility has several advantages over the existing methods to estimate volatility. First, it can be treated as an observable variable as opposed to a latent variable estimated from the GARCHtype models, which makes it easier to model the dynamics of volatility, especially in a multivariate setting. Second, it does not rely on any volatility models (e.g., GARCH and stochastic volatility models), making the volatility measure more robust.
To compute realized volatility (variance) for each trading region, we sum the squared fiveminute exchange rate returns (logarithmic changes in exchange rates) over each trading region, as shown in Figure 2. Because the five regions have different trading time lengths, we normalize realized volatility by the number of fiveminute intervals within each region to make the volatility estimates comparable across regions. We use the logarithm of normalized realized volatility as our volatility measure as previous research has shown that log volatility is closer to normality and can reduce outlier observations (Andersen, Bollerslev, Diebold, Labys (2001, 2003)). Figures 3 through 5 show the average fiveminute intraday and regional mean absolute returns, trading volume and numbers of transactions, respectively. Not surprisingly, absolute returns, trading volume and numbers of transactions are almost always highest during the EuropeAmerica overlap region. The AsiaEurope overlap region also appears highly active, especially for dollaryen.
We model the dynamics of volatility measures by allowing each region's volatility to depend on its past volatility and other regions' past volatilities (Melvin and Melvin (2003)). Specifically, we estimate the following fiveequation (one for each region) system of equations:
= A
+
... + A
+
B

(1) 

where is a vector of regional volatility at day , is a vector of dummy variables to control for day of the week and holidays in Japan, the United Kingdom, and the United States and for large movements in exchange rate due to foreign exchange interventions^{5}, and is a vector of innovations. The vector of volatility contains volatility measures for five trading ``regions'': Asia Pacific, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America. Because of the timezone difference, the timing convention of the vector of volatility measures differs across the five trading regions. For example, the first lag for the Asian region regression is the previous day's volatility of the Asian region and other regions, whereas the first lag for the American region regression is the previous day's volatility for the American region but the same day volatility for other regions. The lag length of the system of equations is chosen by the Akaike information criterion.^{6} We estimate this system of equations by using seemingly unrelated regressions (SUR), as the dating convention used results in different (calendar time) lags on other region's volatility for each equation (different righthand side variables across equations), making the SUR more efficient than ordinary least squares.
To study the transmission of trading activity across different trading regions, the joint dynamics of trading activity across the five trading regions must be modeled. Following the same modeling strategy used for volatility, we model each regional trading activity to depend on its past trading activity and other region's past activities. The timing convention for other region's past activities follows that used for volatility. As noted earlier, we use two measures of daily regional trading activity. First, trading volume denominated in base currency within each region is used to measure trading activity. Second, we use the number of transactions that occurs within each region to measure trading activity. Figure 4 shows average fiveminute intraday and regional trading volume. All trading volumes are index to the average trading volume where the index equals to 100 for average fiveminute trading volume over the whole sample. Figure 5 shows the average fiveminute intraday and regional number of transactions, also indexed to the average number of transactions.
To conserve space, we do not report all coefficient estimates from the fiveequation system of equations. We only report Wald test statistics for blocks of coefficients representing heat wave and meteor shower hypotheses. The null hypothesis for heat wave effect is that each regional volatility (trading activity) depends on its past volatility (trading activity), while the null hypothesis for meteor shower effect is that each regional volatility (trading activity) depends on other region's past volatilities (trading activities). Tables 1 through 6 report Wald test statistics for eurodollar and dollaryen exchange rate volatilities and trading activities. All tables have similar format in that columns show dependent variables for each regression and rows show independent variables for each regression. The diagonals of each table show Wald test statistic for the heat wave hypothesis, and the offdiagonals show the test statistic for meteor shower hypothesis. The value for the Wald test statistic is shown in bracket. All test statistics that are significant at the 95 percent level are in bold, and those that are significant at the 90 percent level are underlined. Adjusted Rsquared statistic for each regression is shown at the bottom of the table. In addition, the values for the teststatistic of residual autocorrelation for 5 and 35 lags are reported in the last two rows.
Table 1 reports Wald test statistics for heat wave and meteor shower effects for eurodollar exchange rate volatility. Inspecting the diagonals, there is statistically significant evidence of heat wave effect. Examining the offdiagonals, there is also statistically significant evidence of meteor shower effect. These findings are similar to results documented in Melvin and Melvin (2003) based on indicative quotes and a shorter, earlier sample period. The system of equations captures the joint dynamics of volatilities rather well, indicating by the adjusted Rsquared between 0.3 and 0.4. In addition, the values for residual autocorrelation for 5 and 35 lags show that there is not much persistence left in the residuals. The results for dollaryen exchange rate volatility are shown in Table 2. Similar to the results on eurodollar volatility, there is statistically significant evidence of both heat wave and meteor shower effects.
To evaluate the economic importance of the heat wave effect (ownregion past volatility) and the meteor shower effect (other region's past volatility) in explaining each region volatility persistence, we simulate our system of equations to examine the impact of a onestandard deviation shock to the innovations of volatility in each region on current and future values of itself and other regions. The ordering of our endogenous variables follows the actual starting of trading time for each region, with Asia Pacific starting first and America starting last. Figures 6 and 7 show the impulse response functions for eurodollar and dollaryen volatilities for 15 days (3 weeks). Columns of each figure represent dependent variables, while rows represent shocks of a onestandard deviation to independent variables. For example, the impact of a onestandard deviation shock from the AsiaEurope overlap trading region to Europe trading region is shown in the third column of the second row. The impulse response functions are shown in solid lines, and the twostandard error band is shown in dashed line. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. Consistent with results on the Wald test statistics for heat wave and meteor shower hypotheses shown in Tables 1 and 2, Figures 6 and 7 provide evidence for both heat wave and meteor shower effects. The meteor shower effect is most pronounced between the originator of a shock region and the consecutive region, as shown in the boxes to the right of the diagonals. The heat wave effect, however, is economically much more important than the meteor shower effect, indicating by the size and the persistent of the responses on the diagonals as compared to the offdiagonals, similar to results in Melvin and Melvin (2003).
It is well established that information affects both volatility and trading volume. Thus, we use test results for trading volume as a robustness check of the results for volatility. In addition, studying trading volume sheds light on the role of information in resolving heterogeneity in agents' beliefs (e.g., Harris and Raviv (1993) and Shalen (1993)). Results on statistical tests of heat wave and meteor shower hypotheses for eurodollar and dollaryen trading volumes are shown in Tables 3 and 4 and the results based on the number of transactions are shown in Tables 5 and 6. The results on eurodollar trading volume and the number of transactions show that there is statistically significant evidence of both the heat wave and meteor shower effects, while the results based on the number of transactions showing stronger evidence. Similar to the results on eurodollar trading activity, the results on the dollaryen trading activity show statistically significant evidence of both heat wave and meteor shower effects. For the meteor shower effect, most of trading activity spillover originates from Asia Pacific and the AsiaEurope overlap regions. This finding may be attributable to the fact that most information that drive dollaryen exchange rate originates from Japan.
The economic importance of heat wave and meteor shower effects for trading activity is evaluated in Figures 8 and 10 for eurodollar. The results are similar to those based on volatility in that the heat wave effect is more important economically than the meteor shower effect. However, the relative magnitude of economic importance between heat wave and meteor shower effects based on trading activity is much larger than that based on volatility. Figures 9 and 11 show results for dollaryen trading activity. The results are similar to those of eurodollar trading activity.
Overall, we find statistically significant evidence of heat wave and meteor shower effects for both volatility and trading activity for both currency pairs. However, the heat wave effect is more important economically than the meteor shower effect for both volatility and trading volume, especially for trading volume. The fact that results from both volatility and trading activity are similar confirms the robustness of empirical results documented in this paper.^{7}
This study uses a modelfree volatility measure computed from high frequency data to explore the transmission of volatility in the foreign exchange market. Our results are based on a dataset from EBS, which represents most of the global interdealer trading activity in the eurodollar and the dollaryen exchange rates and contains a longer and more recent sample period than previous studies (e.g., Engle, Ito, and Lin (1990), Baillie and Bollerslev (1990), Hogan and Melvin (1994), and Melvin and Melvin (2003)). In addition, our realized volatility is based on transactable quotes as opposed to indicative quotes used in existing studies. These advantages of our data should give us a better understanding of the sources of volatility clustering. Based on our regional volatility model, we find statistically significant evidence for both the heat wave and the meteor shower effects. The heat wave effect, however, dominates the meteor shower effect in economic significance.
Unlike previous studies, which only investigate the transmission of volatility across trading regions, this paper is the first to study the transmission of trading activity across trading regions. Similar to results for volatility, we find statistically significant evidence supporting both the heat wave and the meteor shower effects, and the heat wave effect is much more important economically than the meteor effect. The similarity of our results for both volatility and trading activity confirms the robustness of our findings.
Andersen, T., T. Bollerslev, F.X. Diebold, P. Labys, 2001, ``The Distribution of Realized Exchange Rate Volatility,'' Journal of the American Statistical Association, 96, 4255.
Andersen, T., T. Bollerslev, F.X. Diebold, P. Labys, 2003, ``Modeling and Forecasting Realized Volatility,'' Econometrica, 71, 529626.
Baillie, R., and T. Bollerslev, 1990, ``Intraday and Intermarket Volatility in Foreign Exchange Rates,'' Review of Economics Studies, 58, 565585.
Chaboud, A., and B. LeBaron, 2001, ``Foreign Exchange Market Trading Volume and Federal Reserve Intervention'', Journal of Futures Markets, 21, 851860.
Chaboud, A., S. Chernenko, E. Howorka, R.S. Krishnasami Iyer, D. Liu, and J. Wright, 2004, ``The HighFrequency Effects of U.S. Macroeconomic Data Releases on Prices and Trading Activity in the Global Interdealer Foreign Exchange Market,'' Federal Reserve Board's International Finance Discussion Papers Number 823.
Daníelsson, J., and R. Payne, 2002, ``Real Trading Patterns and Prices in Spot Foreign Exchange Markets,'' Journal of International Money and Finance, 21, 203222.
Engle, R.F., T. Ito, and W. Lin, 1990, ``Meteor Showers or Heat Waves? Heteroscedastic Intra daily Volatility in the Foreign Exchange Market,'' Econometrica, 59, 525542.
Goodhart, C., T. Ito, and R. Payne, 1996, ``One Day in June 1993: A Study of the Working of the Reuters 20002 Electronic Foreign Exchange Trading System,'' The Microstructure of Foreign Exchange Markets, The University of Chicago Press.
Harris, M., and A. Raviv, 1993, ``Difference of Opinion Make a Horse Race,'' Review of Financial Studies, 6, 473506.
Hogan Jr., K.C., and M. T. Melvin, 1994, ``Sources of Meteor Showers and Heat Waves in the Foreign Exchange Market,'' Journal of International Economics, 37, 239 247.
Ito, T., and Y. Hashimoto, 2004, ``Microstructure of the Yen/Dollar Foreign Exchange Market: Patterns of IntraDay Activity Revealed in the Electronic Broking System,'' NBER Working Paper 10856.
Jones, C.M., G. Kaul, and M.L. Lipson, 1994, ``Transactions, Volume, and Volatility,'' Review of Financial Studies, 7, 631651.
Melvin, M., and B. Melvin, 2003, ``The Global Transmission of Volatility in the Foreign Exchange Market,'' Review of Economics and Statistics, 85, 670679.
Melvin, M., and X. Yin, 2000, ``Public Information, Exchange Rate Volatility, and Quote Frequency,'' Economic Journal, 110, 644661.
Omrane, W., and A. Heinen, 2004, ``The Foreign Exchange Quoting Activity as An Informative Signal,'' working paper, Catholic University of Louvain.
Shalen, C.T., 1993, ``Volume, Volatility, and the Dispersion of Beliefs,'' Review of Financial Studies, 6, 405434.
Table 1. Wald Tests for Heat Wave and Meteor Shower Effects for EuroDollar Volatility Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion volatility persistence) and meteor shower effect (interregional volatility spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  59.50, [0.00] 
96.02, [0.00] 
2.45, [0.48] 
12.42, [0.01] 
16.91, [0.00] 
AE  11.51, [0.01] 
30.19, [0.00] 
203.00, [0.00] 
3.79, [0.29] 
3.07, [0.38] 
EU  22.73, [0.00] 
34.50, [0.00] 
29.59, [0.00] 
36.70, [0.00] 
2.55, [0.47] 
EA  7.53, [0.06] 
25.56, [0.00] 
7.87, [0.05] 
39.68, [0.00] 
112.81, [0.00] 
AM  52.55, [0.00] 
8.36, [0.04] 
9.35, [0.03] 
18.02, [0.00] 
55.14, [0.00] 
Adj. Rsq  0.32 
0.37 
0.36 
0.39 
0.35 
pvalue, Q(5)  0.23 
0.09 
0.34 
0.35 
0.49 
pvalue, Q(35)  0.07 
0.08 
0.21 
0.10 
0.12 
Table 2. Wald Tests for Heat Wave and Meteor Shower Effects for DollarYen Volatility Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion volatility persistence) and meteor shower effect (interregional volatility spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  77.06, [0.00] 
217.20, [0.00] 
32.75, [0.00] 
8.79, [0.03] 
24.27, [0.00] 
AE  27.74, [0.00] 
6.43, [0.09] 
111.87, [0.00] 
16.93, [0.00] 
2.71, [0.44] 
EU  12.56, [0.01] 
21.38, [0.00] 
14.37, [0.00] 
77.84, [0.00] 
1.99, [0.57] 
EA  4.19, [0.24] 
10.09, [0.02] 
3.33, [0.34] 
26.19, [0.00] 
149.84, [0.00] 
AM  80.45, [0.00] 
3.45, [0.33] 
4.70, [0.20] 
21.94, [0.00] 
32.55, [0.00] 
Adj. Rsq  0.44 
0.35 
0.33 
0.36 
0.29 
pvalue, Q(5)  0.31 
0.12 
0.26 
0.65 
0.37 
pvalue, Q(35)  0.21 
0.09 
0.22 
0.26 
0.09 
Table 3. Wald Tests for Heat Wave and Meteor Shower Effects for EuroDollar Trading Volume Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion trading volume persistence) and meteor shower effect (interregional trading volume spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  18.68, [0.00] 
26.02, [0.00] 
6.24, [0.10] 
4.71, [0.19] 
4.98, [0.17] 
AE  6.87, [0.08] 
22.63, [0.00] 
5.89, [0.12] 
6.22, [0.10] 
7.81, [0.05] 
EU  2.48, [0.48] 
7.99, [0.05] 
5.55, [0.14] 
11.46, [0.01] 
3.03, [0.39] 
EA  2.11, [0.55] 
3.42, [0.33] 
9.37, [0.02] 
12.33, [0.01] 
7.18, [0.07] 
AM  3.84, [0.28] 
3.13, [0.37] 
7.47, [0.06] 
8.89, [0.03] 
6.53, [0.09] 
Adj. Rsq  0.25 
0.27 
0.24 
0.25 
0.23 
pvalue, Q(5)  0.88 
0.91 
0.77 
0.67 
0.67 
pvalue, Q(35)  0.26 
0.74 
0.16 
0.60 
0.21 
Table 4. Wald Tests for Heat Wave and Meteor Shower Effects for DollarYen Trading Volume Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion trading volume persistence) and meteor shower effect (interregional trading volume spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  19.81, [0.00] 
8.16, [0.04] 
4.50, [0.21] 
2.64, [0.45] 
0.66, [0.88] 
AE  25.51, [0.00] 
1.73, [0.63] 
24.30, [0.00] 
11.42, [0.01] 
2.76, [0.43] 
EU  1.12, [0.77] 
1.84, [0.61] 
1.97, [0.58] 
1.55, [0.67] 
5.77, [0.12] 
EA  1.47, [0.69] 
7.10, [0.07] 
2.65, [0.45] 
1.70, [0.64] 
16.32, [0.00] 
AM  4.81, [0.19] 
2.27, [0.52] 
3.95, [0.27] 
5.09, [0.17] 
50.76, [0.00] 
Adj. Rsq  0.24 
0.22 
0.23 
0.22 
0.28 
pvalue, Q(5)  0.77 
0.54 
0.52 
1.00 
0.49 
pvalue, Q(35)  0.18 
0.27 
0.26 
0.95 
0.15 
Table 5. Wald Tests for Heat Wave and Meteor Shower Effects for EuroDollar Number of Transactions Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion number of deals persistence) and meteor shower effect (interregional number of deals spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  27.24, [0.00] 
28.91, [0.00] 
12.29, [0.01] 
5.85, [0.12] 
6.66, [0.08] 
AE  11.02, [0.01] 
16.62, [0.00] 
9.66, [0.02] 
9.27, [0.03] 
10.80, [0.01] 
EU  2.98, [0.39] 
12.11, [0.01] 
9.98, [0.02] 
13.71, [0.00] 
4.40, [0.22] 
EA  4.04, [0.26] 
4.10, [0.25] 
10.97, [0.01] 
11.97, [0.01] 
13.08, [0.00] 
AM  3.87, [0.28] 
2.43, [0.49] 
6.86, [0.08] 
9.81, [0.02] 
10.28, [0.02] 
Adj. Rsq  0.26 
0.28 
0.25 
0.26 
0.24 
pvalue, Q(5)  0.51 
0.61 
0.55 
0.47 
0.31 
pvalue, Q(35)  0.21 
0.20 
0.14 
0.43 
0.12 
Table 6. Wald Tests for Heat Wave and Meteor Shower Effects for DollarYen Number of Transactions Persistence
This table shows Wald teststatistics for block of coefficients representing heat wave effect (ownregion number of deals persistence) and meteor shower effect (interregional number of deals spillover persistence). Chisquared statistics and associated pvalues (in brackets) are reported for each blocks of coefficients. Dependent variables are in columns and independent variables are in rows. The five regions are AS (Asia), AE (AsiaEurope overlap), EU (Europe), EA (EuropeAmerica overlap), and AM (America). For each equation, adjusted Rsquared and pvalues of Qstatistics for residual autocorrelation are reported for 5 lags and 35 lags.
Independent Regions  Dependent Regions  AS  Dependent Regions  AE  Dependent Regions  EU  Dependent Regions  EA  Dependent Regions  AM 

AS  30.83, [0.00] 
10.71, [0.01] 
5.81, [0.12] 
3.74, [0.29] 
1.86, [0.60] 
AE  23.87, [0.00] 
2.14, [0.54] 
23.42, [0.00] 
12.06, [0.01] 
0.59, [0.90] 
EU  2.60, [0.46] 
3.07, [0.38] 
3.34, [0.34] 
2.93, [0.40] 
9.07, [0.03] 
EA  1.98, [0.58] 
9.26, [0.03] 
3.21, [0.36] 
2.36, [0.50] 
5.75, [0.12] 
AM  3.11, [0.38] 
3.31, [0.35] 
2.92, [0.40] 
4.31, [0.23] 
28.34, [0.00] 
Adj. Rsq  0.37 
0.23 
0.27 
0.22 
0.24 
pvalue, Q(5)  0.42 
0.16 
0.69 
1.00 
0.12 
pvalue, Q(35)  0.12 
0.10 
0.80 
0.93 
0.10 
Figure 1. Regional Trading Volume
This figure shows regional trading volume among three financial centers. All trading volumes are indexed to the average overall trading volume where the index equals to 100 for average overall trading volume per oneminute period over the whole sample (separate index for each currency). Regional mnemonics are LN_LN (London and London), NY_NY (New York and New York), TY_TY (Tokyo and Tokyo), LN_NY (London and New York), LN_TY (London and Tokyo), and NY_TY (New York and Tokyo).
Figure 2. Regional Time Zones Based on Trading Volume
This figure defines time zones (in New York time) for each region based on regional trading volume, adjusted for Daylight Saving Time (DST) whenever it is applicable. Day(t) = 17:01 NY time (t1)  17:00 NY time (t) where t is a calendar date. Local times are shown for three major financial centers: New York (NY), London (LN) and Tokyo (TY), and regional open hours (in three cases with or without GST) are marked by color bars.
Figure 3. Average FiveMinute Intraday and Regional Mean Absolute Returns
This figure shows means of fiveminute intraday and regional mean absolute return. Regional means are Asia, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America. The regional mean for Asia appears both at the first and the last sections (from 17:01 through 2:30).
Figure 4. Average FiveMinute Intraday and Regional Mean Trading Volumes
This figure shows means of fiveminute intraday and regional mean trading volumes. All trading volumes are indexed to the average trading volume where the index equals 100 for the mean global fiveminute trading volume over the whole sample (seperate index for each currency). Regional means are Asia, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America. The regional mean for Asia appears both at the first and the last means (from 17:01 through 2:30).
Figure 5. Average FiveMinute Intraday and Regional Mean Number of Transactions
This figure shows means of fiveminute intraday and regional mean number of transactions. All number of transactions are indexed to the average number of transactions where the index equals 100 for the mean global fiveminute number of transactions over the whole sample (seperate index for each currency). Regional means are Asia, the AsiaEurope overlap, Europe, the EuropeAmerica overlap, and America. The regional mean for Asia appears both at the first and the last means (from 17:01 through 2:30).
Figure 6. Response of EuroDollar Volatilities to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in volatility of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
Figure 7. Response of DollarYen Volatilities to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in volatility of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
Figure 8. Response of EuroDollar Trading Volumes to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in trading volume of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
Figure 9. Response of DollarYen Trading Volumes to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in trading volume of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
Figure 10. Response of EuroDollar Number of Transactions to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in the number of transaction of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
Figure 11. Response of DollarYen Number of Transactions to OneStandard Deviation Shocks
This figure shows the effect of a onestandard deviation shock to the innovations in the number of transaction of one region on day t on itself and the other regions for days t+1 through t+15 (3 weeks). The impulse response functions are shown in solid lines, and the twostandard error bands are shown in dashed lines. The twostandard error band is computed from a bootstrap with replacement for 2,000 repetitions. The ordering of the system of equations is Asia (AS), the AsiaEurope overlap (AE), Europe (EU), the EuropeAmerica overlap (EA), and America (AM).
** Cai and Wongswan are at the Division of International Finance of the Federal Reserve Board, Washington, D.C., 20551. Cai can be reached at fang.cai@frb.gov or (202) 4523540. Wongswan can be reached at jon.wongswan@frb.gov or (202) 4522953. Howorka is at EBS, 535 Madison Avenue, New York, NY 10022. We thank David Berger for excellent research assistance. We are grateful to Mark Carey, Alain Chaboud, Mico Loretan, Jonathan Wright, and participants in the IF Tuesday Group for helpful discussions. The views in this paper are solely the responsibility of the authors and should not be interpreted as reflecting the views of the Board of Governors of the Federal Reserve System or any other person associated with the Federal Reserve System. Return to text
1. All dealers located in the Asia Pacific area are served by the computer center in Tokyo and all trades are recorded as originating from Tokyo. The computer center in London serves dealers that are located in Europe, the Middle East, and Africa, and the computer center in New York serves dealers that are located in both North and South America. Return to text
2. See Chaboud et al (2004) for a more detailed discussion of the EBS data. Return to text
3. We do not consider the New York/Tokyo overlap period since it is very short (half an hour or so) and trading is very light. Return to text
4. It is still debatable whether frequency of indicative quotes is a good proxy for trading activity. Goodhart, Ito, and Payne (1996) finds it dubious to infer transactions frequency from indicative quote data, Daníelsson and Payne (2002) and Omrane and Heinen (2004) suggest that quote frequency is a fair proxy for volumes and liquidity supply. Return to text
5. During our sample period, U.S. monetary authorities intervened in the foreign exchange market once on September 22, 2000. Japanese monetary authorities intervened for 142 days; all dates are available on the Ministry of Finance's webpage (http://www.mof.go.jp/english/e1c021.htm). Return to text
6. All empirical results are qualitatively similar when we allow either longer or shorter lags. Results are available on request. Return to text
7. We also estimated the regional model for exchange rate returns. Because the model could not capture the dynamic of exchange rate return well, judging from low adjusted Rsquared around 0.02, we did not test the heat wave and meteor shower effects. Return to text
This version is optimized for use by screen readers. A printable pdf version is available.