macroeconomic factors of exchange rate volatility
TRANSCRIPT
Macroeconomic factorsof exchange rate volatility
Evidence from four neighbouring ASEANeconomies
Chong Lee-LeeFaculty of Management, Centre for Multimedia Banking,
Investment and Accounting, Multimedia University, Selangor, Malaysia, and
Tan Hui-BoonThe University of Nottingham Malaysia Campus, Semenyih, Malaysia
Abstract
Purpose – The purpose of this study is to examine the factors of exchange rate volatility from themacroeconomic perspective for four neighbouring ASEAN economies.
Design/methodology/approach – This study has scrutinised the link between macroeconomicfactors and exchange rate volatility in both the short and the long run by applying econometricstechniques.
Findings – This study further suggests the link between macroeconomic factors and exchange ratevolatility in both the short and the long run for the selected economies. The empirical results, however,indicate that a set of common factors seems to influence the exchange rate volatility, whereby the stockmarket is a great influence commonly found across countries. The Indonesian rupiah seems to be themost sensitive to the innovations in macroeconomic factors, while the Singapore dollar is the least.
Research limitations/implications – The macroeconomic factors are believed to be the forcesbehind exchange rate volatility through the presumable rigidities of their exchange rates, resultingfrom the managed float exchange rate system adopted by those countries. Their capital markets arevital in maintaining exchange rate stability, hence suggesting the imperative role of respectiveauthorities and market players in managing a viable capital market.
Originality/value – Little attention has been given to developing countries’ experiment with theirexchange rate systems due to their presumed rigid volatility. This study adopts a more sophisticatedapproach in measuring the volatility of the exchange rate and examines the underlying factors ofexchange rate volatility instead of the level of exchange rate.
Keywords Exchange rate mechanisms, Macroeconomics, GARCH specification, Econometrics
Paper type Research paper
1. IntroductionThroughout the years, the global economy has been transformed from a simplifiedfinancial architecture to a complex intertwined set of financial systems. From theBretton Woods system to the advent of flexible exchange rate systems in 1973 until thepresent days, the environment of international markets had experienced substantialchanges in the form of excessive variability in exchange rates, greater capital mobilityand punctuated by a series of financial crises worldwide in recent years. For example,the Asian crisis-1997 had hampered growth of many Asian countries and differentresponses had been adopted by the crisis-hit countries in ameliorating their economies.Thailand, Indonesia and South Korea all agreed to receive the International Monetary
The current issue and full text archive of this journal is available at
www.emeraldinsight.com/1086-7376.htm
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Studies in Economics and FinanceVol. 24 No. 4, 2007pp. 266-285q Emerald Group Publishing Limited1086-7376DOI 10.1108/10867370710831828
Fund (IMF) rescue programme whereby Malaysia had shied away from the offer.Different remedial measures were taken by the affected economies in managing theireconomic contraction and erratic exchange rate movement.
Asian economies in general have transformed tremendously since the 1970s and theexchange rate arrangements implemented by the countries have come a long waycompared with the past since the eruption of the Asian financial crisis-1997.Developing countries are more exposed to both internal and external disturbances thanever. A better understanding of exchange rate volatility therefore might providegreater economic stability. Previously, most researches have scrutinised determinantsof the level of exchange rate. Meese (1990) who studied the currency fluctuations in thepost-Bretton Woods era found that the changes of macroeconomic variables alonecould not explain major currencies movements. By using a long-span data, MacDonaldand Taylor (1994) however noticed relationships between macroeconomic variablesand exchange rate. A recent study by Rapach and Wohar (2002) meanwhile producedmixed results for the monetary model of exchange rate determination.
Movements of exchange rate are always a concern for various parties. Ininternational currency markets, exchange rate plays a significant role and thevariability of exchange rate, whichever way it sways, tends to give a significant impacton the economy. Since, the adoption of flexible exchange rate system in 1973, exchangerate movements have been excessive and the bulk of the previous studies on thissubject matter are based on the experience of developed countries such as Organizationof Economical Co-operation members. Little attention has been given to developingcountries’ experiment with different exchange rate systems due to their presumed rigidvolatility. However, nominal currencies of the developing nations might not producefixed and predictable exchange rate and its parity level might deviate, paving way forcurrency speculation moves. This explains why a currency crisis frequently takesplace in developing countries.
The exchange rate volatility faced by developing nations most likely will also varydespite of its pegging system due to the implicit weight of the currency that onecountry pegs. Though Asian economies generally prefer managed float exchange ratesystem, the exchange rate volatility of each currency is said to vary even in thepresence of a pegging system (Warner and Kreinin, 1983; Alba and Papell, 1998). Inview of this, the forces to exchange rate volatility for the four Asian economies thathave been selected for this study – Malaysia, Indonesia, Thailand and Singapore –deserve vigorous examination. The four countries, adopting semi-fixity exchange ratesystem, are small and open economies that have substantially liberalised their tradeand investment sectors since the 1980s. According to the classical problem ofmacroeconomic trilemma, exchange rate stability, capital mobility and autonomousmonetary policies all cannot be achieved simultaneously and one of the three must besacrificed. Therefore, the importance of identifying the factors of exchange ratevolatility of the four currencies must not to be underestimated or overlooked in order tomaintain their macroeconomic success. This paper, thus, intends to examine the causescontributing to the volatility of the Malaysian ringgit, the Indonesian rupiah, the Thaibaht and the Singapore dollar.
Given that the four economies experienced several switches in their exchange ratearrangements since the 1980s, this study only analyses the macroeconomic factors ofexchange rate volatility during the flexible exchange rate period. At the same time, the
Factors ofexchange rate
volatility
267
underlying macroeconomic factors of exchange rate volatility instead of the level ofexchange rate are investigated. In computing the exchange rate volatility, this studyuses a more sophisticated approach in measuring the volatility of exchange rate wheregeneralised autoregressive conditional heteroscedastic (GARCH) approach is selectedin view of its superior performance in providing a parsimonious stochastic process ofexchange rate return. In order to capture the asymmetric effect, exponential GARCH(E-GARCH), an extension of GARCH approach, is chosen.
The outline of this paper is as follows: Section 2 describes the exchange ratevolatility for the pre- and post-Asian crisis 1997 periods. Section 3 explains themethodology used while Section 4 delineates the results and discussions. Section 5presents a summary and the relevant concluding remarks.
2. Exchange rate volatility during the pre- and post-Asian crisis in 1997Figure 1 shows the volatility of Malaysian ringgit, Indonesian rupiah, Thai baht andSingapore dollar from January 1980 to December 2003 which these currencies arevis-a-vis US dollar. The volatility rates are computed based on the E-GARCHspecification where the lag order is selected based on the Schwartz criteria[1].
For most of the past two decades, a majority of the South-East Asian economies arein favour of a managed float system. The four countries of Malaysia, Indonesia,Thailand and Singapore attach great importance to exchange rates stability in theirpolicy making. This section looks at the 20-year exchange rates volatility in the hope tocast some light on the degree of exchange rate risk for the four economies bycomparing the volatility of their currencies. Overall, Indonesia is the country whichsuffered the most in terms of volatile exchange rate even for the past several years,when the effect of the Asian crisis began to subside for the others. Thailand’s exchangerate is the most volatile after Indonesia. Singapore had kept its exchange rate volatilityin the lowest compared with the other three countries examined since the 1980s.
Figure 1.Exchange rate volatilityfor the pre- and post Asiancrisis in 1997 from January1980 to December 2003
0
5
10
15
20
25
30
35
40
45
Jan-
80
Jan-
81
Jan-
82
Jan-
83
Jan-
84
Jan-
85
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86
Jan-
87
Jan-
88
Jan-
89
Jan-
90
Jan-
91
Jan-
92
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93
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94
Jan-
95
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96
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97
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98
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99
Jan-
00
Jan-
01
Jan-
02
Jan-
03
Ringgit S$ Rupiah Baht
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268
Malaysia had preserved considerably low exchange rate risk and its exchange ratevolatility generally was lower than that of Indonesia and Thailand prior to the pegsystem.
Over the years, Malaysia, Indonesia and Thailand have experienced substantialchanges in their measures taken in the form of monetary and fiscal policies in responseto the ever-changing environment. The rapid changes are particularly visible since theliberalisation of their trade and investment sectors in the 1980s and after the 1997Asian financial crisis. The exchange rate of these economies had depreciated sharplyas a result of currency speculation attacks that raised the curtain on the 1997 Asianfinancial crisis. In mitigating the negative impact of the crisis, Malaysia had taken adifferent path from that chosen by Indonesia and Thailand. While Malaysia hadpegged its currency to the US dollar in the year 1998, the other two had floated theircurrencies to arrest the sharp depreciation of their currencies. Singapore had weatheredits economy relatively well from the crisis and maintained a consistent exchange ratepolicy.
All the four countries are open economies that have generally implemented someform of managed exchange rate system since 1980 except for Indonesia and Thailand,which adopted the floating system for a few years following the 1997 Asian financialcrisis. All four economies have a high degree of similarities in their economicstructures, geographical location and stages of development but the measures theyeach took in response to the economic meltdown were somewhat different. Apparently,Singapore withstood the crisis with the least fluctuation in its currency given its soundmacroeconomic fundamentals but Indonesia suffered the most volatility in its rupiahmovement, partly because of the country’s political problem at that time. Malaysia, upto the point when the peg system was adopted, seemed to have lower volatility thanthat of Indonesia and Thailand.
3. MethodologyThis study covers the sample period for the four economies within the flexibleexchange rate period. Malaysia covers from January 1980 to September 1998, whenMalaysia ended its pegged system subsequently[2]. The sample periods for Indonesiaand Thailand when both embraced a flexible exchange rate span from August 1997 toJune 2001 and July 1997 to June 2001, respectively. The sample period for Singaporecovers from May 1985 to September 2003 due to its consistent exchange ratearrangement. The category of this exchange rate system is in accordance with IMF’sclassification and the data used are in monthly frequency. The exchange rate is quotedas domestic currency per foreign currency, namely the US dollar.
The exchange rate volatility is computed based on the E-GARCH specificationdeveloped by Nelson (1991) as it is able to account for the asymmetric effect. Itscanonical specification is written as follows:
logðhtÞ ¼ w0 þXq
i¼1
aigðzt2iÞ þXP
J¼1
gjlogðht2jÞ given
Rt ¼ mþ 1; 1tjVt21 , N ð0; htÞ
Factors ofexchange rate
volatility
269
where w and m ¼ constant:
gðztÞ ¼ uzt þ g½jztj2 Ejztj� and zt ¼1tffiffiffiffiht
p
R ¼ logðet=et21Þ where e is an exchange rate of Malaysian ringgit, Indonesian rupiah,Thai baht and Singapore dollar vis-a-vis US dollar, p ¼ the order of the autoregressive(AR) process and q ¼ the order of the moving-average (MA) process. If Zt is positive,then gðztÞ is a linear function of the slope changes Zt with slope of ðuþ gÞ: If Zt isnegative, the slope will be ðu2 gÞ: The conditional variance ht reacts asymmetricallyto the magnitude of innovation, zt2i: The lag order is selected based on the Schwartzcriteria. The exponential GARCH estimation is used to compute the exchange ratevolatility in view of its superior to the standard GARCH model given its variance couldbe an asymmetric function of its past term. Several studies have also employed theexponential GARCH model in estimating exchange rate volatility. For instances, Kim(1998) and Bond and Najand (2002) had utilised the same method in computingexchange rate volatility.
In this study, the computed exchange rate volatility will be incorporated in vectorautoregressive (VAR) model in the context of an econometric modelling ofJohansen-Juselius cointegration and Granger causality tests. The procedure ofincorporating the conditional volatility into a VAR model is supported by Ramchanderand Sant (2002) who also did the same step. Both Johansen-Juselius cointegration testand autoregressive distributed lag (ARDL) model are used to measure the long-runrelations, with Granger causality test in the framework of vector-error correction model(VECM) is employed to gauge the short-run relations.
For the long-run relationship, a multivariate cointegration method developed byJohansen (1988) and Johansen and Juselius (1990) is employed. Johansen and Juselius(1990) employed a maximum likelihood procedure to examine cointegrated procedure.Defining a vector Yt of n potential endogenous variables, Yt is an unrestricted VARwith m lags as follows:
Yt ¼ A0 þ A1Yt21 þ Lþ AmYt2m þ 1t
where Yt is an ðn £ 1Þ vector of variables, A’s is an ðn £ nÞ matrices of parameters and1t is an ðn £ 1Þ vector of constant terms. The Johansen cointegration test can be doneby estimating the above equation in its first difference specification as follows:
DYt ¼ G1DYt21 þ Lþ Gm21DYt2mþ1 þPYt2m þ 1t
where Gi ¼ ðI 2 A1 2 · · · 2 AiÞ with i ¼ 1; 2; . . . ;m2 1 and P ¼ 2ðI 2 A1 2 · · · 2AmÞ: I ¼ the identity matrix and P ¼ an ðn £ nÞ matrix. This model can capture bothshort- and long-run adjustments to the changes in Yt by examining Gi and Prespectively. The Johansen method measures the rank of the matrix P and it can befurther specified as P ¼ ab0 with a indicates the speed of adjustment to disequilibriumand b is a matrix of long-run coefficients. b is an ðn £ rÞ matrix of cointegrating vectorswhile a is an ðn £ rÞ adjustment coefficients matrix which each cointegrating vectorenters the n equations of the VAR. r ¼ 0; 1; . . . ; n and it is the rank of matrix or thenumber of cointegrating independent cointegrating vectors. If the rank ofP is zero, thenthere is no linear combination of the variables in Yt and they are said no cointegrationamong the variables. If the rank of P is full, then they are also said to be stationary. If
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0 , r , n; there will be r cointegrating equations. The maximum likelihood estimate ofb is obtained as the eigenvectors corresponding to the r largest and significanteigenvalues. The significance of eigenvalues can be examined by two maximumlikelihood test statistics that are trace and maximum eigenvalues statistics. The nullhypothesis for trace statistics is that there are at most r cointegration vectors while thereare r cointegrating vectors against the r þ 1 cointegrating vectors for maximumeigenvalues statistics. Both test statistics are shown as below:
TraceðltraceÞ ¼ TXn
i¼rþ1
Lnð1 2 li Þ;
Maximum eigenvalue ðlmax Þ ¼ TLnð1 2 lrþ1Þ
where li are the eigenvalue values.Meanwhile, the ARDL model of Pesaran and Shin (1999) used the ordinary least
square estimation to explain long-run relationship. This method has the advantage ofgetting consistent estimation of long-run coefficients no matter the underlyingregressors are I(1) or I(0). In general, an ADRL model contains of lagged values ofdependent variable, current and lagged values of one or more independent variablesand our model is expressed as below:
Dervt ¼ a0 þXn
j¼1
bjDervt2j þXn
j¼1
cjDmt2j þXn
j¼1
djDyt2j þXn
j¼1
ejDit2j
þXn
j¼1
f jDpt2j þXn
j¼1
gjDtbt2j þXn
j
hjDcit2j þ d1ervt21 þ d2mt21
þ d3yt21 þ d4it21 þ d5pt21 þ d6tbt21 þ d7cit21 þ 1t
where erv ¼ exchange rate volatility; relative money supply, m ¼ (md 2 mf); relativeincome, y ¼ ( yd 2 yf); relative interest rate, i ¼ (id 2 if); relative inflation rate,p ¼ ðpd 2 pfÞ; relative trade balance, tb ¼ (tbd 2 tbf); relative stock index,ci ¼ (cid 2 cif); a ¼ constant; 1 ¼ error term; subscript d and f refer domestic andforeign countries, respectively. All variables are in natural logarithm except for interestrates. The F-statistics will be computed for the significance of the lagged levelvariables with the null hypothesis of no cointegration. The null hypothesis ofnon-existence of long-run relationship is defined by:
H 0 ¼ d1 ¼ d2 ¼ d3 ¼ d4 ¼ d5 ¼ d6 ¼ d7 ¼ 0
against its alternative hypothesis:
H 1 ¼ d1 – d2 – d3 – d4 – d5 – d6 – d7 – 0
The lag length, n, is selected by Akaike information criterion (AIC). Owing to theasymptotic distributions of the F-statistics are non-standard, Pesaran et al. (1996)provide two sets of asymptotic critical values which on one side, all variables are I(0)and on the other side, all variables are I(1). These two sets of critical values cover all the
Factors ofexchange rate
volatility
271
possible categories of regressors into purely I(0), purely I(1) or mutually cointegrated. Ifthe computed F-statistic is greater than the upper bound (FU), the null hypothesis of nocointegration can be rejected whereas if the computed F-statistic falls below the lowerbound (FL), then the null hypothesis cannot be rejected. However, if the computedF-statistic falls between the upper and lower bound, the result is inconclusive and thestandard analysis for unit roots should be applied. Among others, Bahmani-Oskooeeand Kara (2000), Pesaran et al. (2001), Bahmani-Oskooee and Ng (2002), Piesse andHearn (2002) and Chou and Lee (2003) also utilised the ARDL technique in measuringlong-run relations.
On the other hand, causality test as proposed by Granger (1969, 1988) is included inthis study whereby error correction term(s) (ECM) is embraced in the causality test toavoid misspecification problem (Granger, 1988). The ECM(s) carries short-runcorrection to form long-run equilibrium and also captures short-run adjustment ofcointegration variables. Masih and Masih (1997a, b) indicated some important findingsthat if series are stationary after first differencing and if they are cointegrated of orderr, then r number of ECM(s) should be included in the VECM analysis. The vector timeseries can be written as Yt ¼ ð y1; y2; . . . ; ynÞ
0 while the general VECM formula is asbelow:
DYt ¼ d0 þPYt21 þXm
i¼1
uiDYt2i þ 1t
where Yt is an ðn £ nÞ vector of variables, d0 is an ðn £ 1Þ vector of constants, P and uare ðn £ nÞ matrices reflecting both short-and long-run effects, 1 is an ðn £ 1Þ vector ofwhite noise disturbances. If series are not cointegrated, then the P ¼ 0 and the VECMis an unrestricted VAR. However, if there is a cointegration relationship, the P can bedecomposed into two ðn £ rÞ matrices of a and b, for example P ¼ ab0.
On the other hand, the variance decomposition is a technique which allows fordynamic shocks among variables and it captures the forecast error of each of thevariables into components from the innovations by each endogenous variableincluding its own shock. The relative strength of the variable can be captured by usingthe forecast error of variance decomposition. This forecast error of variancedecomposition based on the Choleski decomposition is too sensitive to the order of thevariables. Therefore, the generalised variance decomposition based on Pesaran andShin (1998) is integrated to gauge the relative importance of the influence of eachmacroeconomic factor on exchange rate volatility.
The procedures of carrying out the analysis of macroeconomic factors of exchangerate volatility involve computing the conditional standard deviation of the exchangerates and then incorporate it into the setting as below:
erv ¼ a0 þ a1ðmd 2mfÞ þ a2ð yd 2 yfÞ þ a3ðid 2 ifÞ þ a4ðpd 2 pfÞ þ a5ðtbd 2 tbfÞ
þ a6ðcid 2 cifÞ þ 1
where erv ¼ conditional standard deviation of exchange rate[3]; m ¼ money supply(M2); y ¼ income[4]; i ¼ interest rate[5]; p ¼ inflation index[6]; tb ¼ ratio ofnominal exports to nominal imports; ci ¼ composite index[7]. Subscript d and f refer
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272
domestic and foreign countries, respectively. The use of relative terms is to capture theimportance of foreign and domestic influences on exchange rate volatility.
4. Results and discussionsTables I-V present the long-run relations of the macroeconomic factors of exchange ratevolatility for the four economies of Malaysia, Indonesia, Thailand and Singapore. In thissetting, the relative terms of interest rates (RI), money supplies (RM), consumer priceindices (RCPI), trade balances (RTB) and composite indices (RCI) are examined againstthe significance of their effect on the exchange rate volatility of the four countries. BothARDL and Johansen-Juselius methods indicate the presence of the long-run movementamong the variables for all the countries. However, the similar result is not found in thecase of Thailand. This suggests that exchange rate volatility and relativemacroeconomic factors are moving together to achieve their long-run equilibrium forthe three economies – Malaysia, Indonesia and Singapore. As a standard procedure, theunit root tests of augmented Dickey and Fuller (1979, 1981) and Kwiatkowski et al.(1992) techniques had been carried out prior to the cointegration test[8].
Both results of ARDL and Johansen-Juselius techniques seem to be consistent andthe following short-run factors of exchange rate volatility are, then, examined byemploying the Granger causality in the vector error-correction model. Tables VI-IXreport the short-run macroeconomic factors of exchange rate volatility for the foureconomies. For Malaysia, relative money supplies, trade balances and stock indices arethe factors which influence the volatility of the ringgit while for Indonesia, two relativemacroeconomic factors – money supplies and stock indices – might exert pressure tothe volatility of rupiah. There are two relative factors of consumer price indices andcomposite indices that might influence the volatility of Thai baht. For Singapore, tworelative macroeconomic factors of money supplies and composite indices mightmanifest their effect on the volatility of Singapore dollar.
To explain the relative forecast error variance of each macroeconomic factor forexchange rate volatility, Tables X-XIII present the results up to 48 months. TheMalaysian ringgit volatility is explained about 55 per cent by its own shocks andthen followed by the shocks in relative trade balance, money supplies and stockindices. On the other hand, the relative terms of interest rates, consumer priceindices, money supplies and stock indices contribute, in large proportion, toinnovations in Indonesian rupiah volatility for about 37, 26, 16 and 14 per cent,
Country F-statistics (lag selection based on AIC) T-statistics Results
Malaysia 3.2703 (1) * ECt21 ¼ 23.8772 * * CointegratedIndonesia 7.1261 (1) * * ECt21 ¼ 24.5485 * * CointegratedThailand 2.1031 (1) – No cointegrationSingapore 2.8977 (1) ECt21 ¼ 23.2809 * * Inconclusive
Notes: At the 5 per cent significance level, the critical values of the bound of the F-statistics are2.476-3.646 whereas at the 10 per cent significance level, the bounds are 2.141-3.250. Asterisks ( * *) and( *) indicate significance at 5 and 10 per cent levels, respectively, and figures in parentheses indicate thelag order. Kremers et al. (1992) have indicated that a significant lagged ECM is a relatively moreefficient way to suggest cointegration relationship. Hence, the error correction tern (EC) of Singapore issignificant and suggests that they are cointegrated
Table I.ARDL cointegration test
results for the underlyingfactors of exchange rate
volatility originated fromrelative macroeconomic
variables
Factors ofexchange rate
volatility
273
Per
iod
:19
80:
M1-
1998
:M
8,E
RV
,R
I,R
M,
RC
PI,
RIP
,R
TB
and
RC
Isp
ecifi
cati
on(l
agor
der
¼1)
Max
imu
mei
gen
val
ues
test
Tra
cete
stN
ull
Hy
pot
hes
isA
lter
nat
ive
hy
pot
hes
isM
axim
um
eig
env
alu
esst
atis
tics
95p
erce
nt
crit
ical
val
ues
Alt
ern
ativ
eh
yp
oth
esis
Tra
cest
atis
tics
95p
erce
nt
crit
ical
val
ues
r¼
0r¼
135
.630
345
.28
r.
112
8.79
18*
124.
24r#
1r¼
234
.482
039
.37
r.
293
.161
594
.15
r#
2r¼
323
.759
533
.46
r.
358
.679
568
.52
r#
3r¼
420
.289
427
.07
r.
434
.920
147
.21
r#
4r¼
58.
4684
20.9
7r.
514
.630
629
.68
r#
5r¼
65.
2251
14.0
7r.
66.
1622
15.4
1r#
6r¼
70.
9371
3.76
r.
70.
9371
3.76
Notes:
Th
eV
AR
ord
eris
bas
edon
lik
elih
ood
rati
ote
st.
* in
dic
ate
sig
nifi
can
ceat
5p
erce
nt
lev
el.J
uk
s(2
003)
,Joh
anse
n(1
994)
and
Pan
tula
(198
9)su
gg
est
that
the
trac
ete
sth
asso
me
adv
anta
ges
over
the
max
imu
mei
gen
val
ue
test
Table II.Johansen-Juseliuscointegration test resultsfor the underlying factorsof exchange ratevolatility originated fromrelative macroeconomicvariables- Malaysia
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274
Per
iod
:19
97:M
8-20
01:M
6,E
RV
,R
I,R
M,
RC
PI,
RIP
,R
TB
and
RC
Isp
ecifi
cati
on(l
agor
der
¼1)
Max
imu
mei
gen
val
ues
test
Tra
cete
stN
ull
hy
pot
hes
isA
lter
nat
ive
hy
pot
hes
isM
axim
um
eig
env
alu
esst
atis
tics
a95
per
cen
tcr
itic
alv
alu
esA
lter
nat
ive
hy
pot
hes
isT
race
stat
isti
csa
95p
erce
nt
crit
ical
val
ues
r¼
0r¼
151
.048
0*
45.2
8r.
115
0.60
05*
124.
24r#
1r¼
235
.321
939
.37
r.
299
.552
6*
94.1
5r#
2r¼
327
.834
933
.46
r.
364
.230
668
.52
r#
3r¼
417
.164
927
.07
r.
436
.395
847
.21
r#
4r¼
511
.481
320
.97
r.
519
.230
929
.68
r#
5r¼
66.
0383
14.0
7r.
67.
7496
15.4
1r#
6r¼
71.
7113
3.76
r.
71.
7113
3.76
Notes:
Th
eV
AR
ord
eris
bas
edon
lik
elih
ood
rati
ote
st.
* in
dic
ate
sig
nifi
can
ceat
5p
erce
nt
lev
el.J
uk
s(2
003)
,Joh
anse
n(1
994)
and
Pan
tula
(198
9)su
gg
est
that
the
trac
ete
sth
asso
me
adv
anta
ges
over
the
max
imu
mei
gen
val
ues
test
.T
est
stat
isti
csis
adju
sted
acco
rdin
gto
Rei
nse
lan
dA
hn
(199
2)d
ue
toth
ep
rob
lem
ofsm
all
sam
ple
size
.Th
ete
stst
atis
tics
isad
just
edb
y(T
2nk)
/T.T
–to
tal
nu
mb
erof
obse
rvat
ion
s;n
–th
en
um
ber
ofse
ries
andk
–la
gle
ng
thor
der
ofth
eV
AR
syst
em.
aF
orM
alay
sia,
inco
me
(y)
refe
rsto
ind
ust
rial
pro
du
ctio
nin
dex
;fo
rIn
don
esia
,it
den
otes
gro
ssn
atio
nal
pro
du
ct(G
NI)
;fo
rT
hai
lan
d,
itre
pre
sen
tsm
anu
fact
uri
ng
pro
du
ctio
nin
dex
;fo
rS
ing
apor
e,it
ind
icat
esto
tal
man
ufa
ctu
rin
gin
dex
Table III.Johansen-Juselius
cointegration test resultsfor the underlying factors
of exchange ratevolatility originated from
relative macroeconomicvariables – Indonesia
Factors ofexchange rate
volatility
275
Per
iod
:19
97:M
7-20
01:M
6,E
RV
,R
I,R
M,
RC
PI,
RIP
,R
TB
and
RC
Isp
ecifi
cati
on(l
agor
der
¼1)
Max
imu
mei
gen
val
ues
test
Tra
cete
stN
ull
hy
pot
hes
isA
lter
nat
ive
hy
pot
hes
isM
axim
um
eig
env
alu
esst
atis
tics
a95
per
cen
tcr
itic
alv
alu
esA
lter
nat
ive
hy
pot
hes
isT
race
stat
isti
csa
95p
erce
nt
crit
ical
val
ues
r¼
0r¼
142
.795
745
.28
r.
112
3.83
0212
4.24
r#
1r¼
234
.189
139
.37
r.
281
.034
594
.15
r#
2r¼
318
.353
133
.46
r.
346
.845
568
.52
r#
3r¼
416
.565
827
.07
r.
428
.492
447
.21
r#
4r¼
58.
2297
20.9
7r.
511
.926
629
.68
r#
5r¼
63.
3263
14.0
7r.
63.
6971
15.4
1r#
6r¼
70.
3707
3.76
r.
70.
3707
3.76
Notes:
Th
eV
AR
ord
eris
bas
edon
lik
elih
ood
rati
ote
st.
* in
dic
ates
sig
nifi
can
ceat
5p
erce
nt
lev
el.a
Tes
tst
atis
tics
isad
just
edac
cord
ing
toR
ein
sel
and
Ah
n(1
992)
du
eto
the
pro
ble
mof
smal
lsam
ple
size
.Th
ete
stst
atis
tics
isad
just
edb
y(T
2nk)
/T.T
–to
taln
um
ber
ofob
serv
atio
ns;n
–th
en
um
ber
ofse
ries
andk
–la
gle
ng
thor
der
ofth
eV
AR
syst
em.T
he
con
dit
ion
alst
and
ard
dev
iati
onof
exch
ang
era
teis
com
pu
ted
via
E-G
AR
CH
met
hod
.Th
ep
andq
ord
ers
for
the
fou
rec
onom
ies-
Mal
aysi
a,In
don
esia
,Th
aila
nd
and
Sin
gap
ore
are
(1,2
),(1
,2),
(2,2
)an
d(2
,2),
resp
ecti
vel
y.
Th
ese
lect
ion
ofp
andq
isb
ased
onth
eS
chw
artz
crit
eria
Table IV.Johansen-Juseliuscointegration test resultsfor the underlying factorsof exchange ratevolatility originated fromrelative macroeconomicvariables – Thailand
SEF24,4
276
Per
iod
:19
85:M
1-20
03:M
9,E
RV
,R
I,R
M,
RC
PI,
RIP
,R
Tan
dR
CI
spec
ifica
tion
(lag
ord
er¼
1)M
axim
um
eig
env
alu
este
stT
race
test
Nu
llh
yp
oth
esis
Alt
ern
ativ
eh
yp
oth
esis
Max
imu
mei
gen
val
ues
stat
isti
cs95
per
cen
tcr
itic
alv
alu
esA
lter
nat
ive
hy
pot
hes
isT
race
stat
isti
cs95
per
cen
tcr
itic
alv
alu
es
r¼
0r¼
155
.632
5*
45.2
8r.
114
3.64
41*
124.
24r#
1r¼
232
.769
939
.37
r.
288
.011
794
.15
r#
2r¼
323
.876
433
.46
r.
355
.241
868
.52
r#
3r¼
418
.133
827
.07
r.
431
.365
347
.21
r#
4r¼
57.
9812
20.9
7r.
513
.231
529
.68
r#
5r¼
64.
9929
14.0
7r.
65.
2504
15.4
1r#
6r¼
70.
2575
3.76
r.
70.
2575
3.76
Notes:
Th
eV
AR
ord
eris
bas
edon
lik
elih
ood
rati
ote
st.
* in
dic
ate
sig
nifi
can
ceat
5p
erce
nt
lev
el
Table V.Johansen-Juselius
cointegration test resultsfor the underlying factors
of exchange ratevolatility originated from
relative macroeconomicvariables – Singapore
Factors ofexchange rate
volatility
277
Dep
end
ent
var
iab
les
Ind
epen
den
tv
aria
ble
s
DE
RV
DR
ID
RM
DR
CP
ID
RIP
DR
TB
DR
CI
EC
Tt2
1
Per
iod
:19
80:M
1-19
98:M
8F
-sta
tist
ics
T-s
tati
stic
s
DE
RV
–1.
5686
(0.2
118)
91.1
038
**
(0.0
000)
1.19
79(0
.275
0)0.
2359
(0.6
277)
6.84
73*
*
(0.0
095)
8.38
51*
*
(0.0
042)
24.
1460
**
DR
I5.
5872
**
(0.0
190)
–0.
0012
(0.9
722)
3.29
02*
(0.0
711)
0.08
10(0
.776
2)0.
8614
(0.3
544)
5.22
26*
*
(0.0
233)
21.
1547
DR
M2.
1858
(0.1
408)
1.14
25(0
.286
3)–
0.56
74(0
.452
1)0.
2457
(0.6
207)
0.13
15(0
.717
2)1.
4257
(0.2
338)
1.01
88D
RC
PI
4.78
55*
*
(0.0
298)
0.08
08(0
.776
6)0.
0276
(0.8
683)
–2.
0523
(0.1
534)
0.02
35(0
.878
3)0.
0050
(0.9
440)
20.
3782
DR
IP3.
5205
*
(0.0
620)
0.58
19(0
.446
4)0.
4335
(0.5
110)
4.49
26*
*
(0.0
352)
–1.
3185
(0.2
522)
0.02
07(0
.885
8)0.
7531
DR
TB
0.02
70(0
.869
7)0.
0132
(0.9
087)
3.09
43*
(0.0
800)
0.54
88(0
.459
6)0.
0212
(0.8
845)
–0.
7752
(0.3
796)
23.
4328
**
DR
CI
0.83
73(0
.361
2)0.
3019
(0.5
833)
0.24
39(0
.621
9)0.
0735
(0.7
866)
0.08
61(0
.769
5)4.
3792
**
(0.0
376)
–2
0.17
10
Notes:
Th
ev
alu
esin
par
enth
eses
are
thep-
val
ue.
** ,
*in
dic
ate
sig
nifi
can
ceat
5an
d10
per
cen
tle
vel
s,re
spec
tiv
ely
Table VI.Results of error correctionestimates for theunderlying factors ofexchange rate volatilityoriginated from therelative macroeconomicvariables – Malaysia
SEF24,4
278
Dep
end
ent
var
iab
les
Ind
epen
den
tv
aria
ble
s
DE
RV
DR
ID
RM
DR
CP
ID
RIP
DR
TB
DR
CI
EC
Tt2
1
Per
iod
:19
97:M
7-20
01:M
6F
-sta
tist
ics
T-s
tati
stic
s
DE
RV
–1.
1979
(0.2
812)
3.54
71*
(0.0
680)
0.37
69(0
.543
3)0.
2150
(0.6
458)
0.00
02(0
.988
6)7.
8313
**
(0.0
083)
26.
6747
**
3.60
96*
*
DR
I0.
9638
(0.3
330)
–0.
0108
(0.9
178)
0.05
50(0
.816
0)2.
8207
(0.1
020)
1.18
87(0
.283
0)0.
8344
(0.3
673)
20.
0843
22.
7460
**
DR
M2.
4887
(0.1
237)
0.02
84(0
.867
2)–
0.04
79(0
.828
1)0.
0669
(0.7
975)
0.06
25(0
.804
0)0.
6734
(0.4
174)
21.
2384
1.88
40*
*
DR
CP
I3.
5080
(0.0
694)
*1.
0703
(0.3
063)
25.8
235
**
(0.0
000)
–0.
4523
(0.5
056)
0.02
00(0
.888
4)3.
9335
*
(0.0
552)
1.13
140.
9821
DR
IP2.
6609
(0.1
118)
1.13
52(0
.294
0)8.
8702
**
(0.0
052)
7.61
83*
*
(0.0
091)
–5.
5206
**
(0.0
246)
2.19
52(0
.147
4)2
0.96
912.
4043
**
DR
TB
0.89
18(0
.351
5)5.
7833
**
(0.0
216)
0.14
56(0
.705
1)1.
6290
(0.2
102)
0.12
76(0
.723
1)–
2.32
46(0
.136
3)2
1.09
221.
1228
DR
CI
0.22
48(0
.638
4)0.
0191
(0.8
910)
0.00
94(0
.923
5)2.
6370
(0.1
134)
1.44
06(0
.238
1)0.
8865
(0.3
529)
–0.
3740
21.
2087
Notes:
Th
ev
alu
esin
par
enth
eses
are
thep-
val
ue.
** ,
* in
dic
ate
sig
nifi
can
ceat
5an
d10
per
cen
tle
vel
.Tw
oco
inte
gra
tin
gv
ecto
rsar
ein
corp
orat
edin
toth
eV
EC
Man
aly
sis
sin
ceth
etr
ace
test
has
som
ead
van
tag
esov
erth
em
axim
um
eig
env
alu
ete
st(J
uk
s,20
03;
Joh
anse
n,
1994
;P
antu
la,
1989
)
Table VII.Results of error correction
estimates for theunderlying factors of
exchange rate volatilityoriginated from relative
macroeconomic variables– Indonesia
Factors ofexchange rate
volatility
279
Dep
end
ent
var
iab
les
Ind
epen
den
tv
aria
ble
s
DE
RV
DR
ID
RM
DR
CP
I
DR
IPD
RT
BD
RC
IP
erio
d:
1997
:M7-
2001
:M6
F-s
tati
stic
s
DE
RV
–1.
5778
(0.2
165)
0.93
12(0
.340
5)4.
9961
**
(0.0
312)
0.04
86(0
.826
6)0.
0190
(0.8
912)
6.07
24*
*(0
.018
2)D
RI
1.16
61(0
.286
8)–
0.01
75(0
.895
5)0.
1542
(0.6
968)
0.44
85(0
.507
0)0.
8558
(0.3
606)
0.02
14(0
.884
4)D
RM
1.87
77(0
.178
4)0.
7729
(0.3
847)
–0.
7096
(0.4
047)
2.54
01(0
.119
1)1.
3583
(0.2
509)
0.37
07(0
.542
6)D
RC
PI
0.70
31(0
.406
8)2.
6339
(0.1
127)
0.19
23(0
.663
4)–
0.00
77(0
.930
4)0.
0746
(0.7
861)
3.92
57*
(0.0
546)
DR
IP0.
6021
(0.4
425)
1.02
80(0
.316
9)0.
3567
(0.5
538)
1.41
87(0
.240
8)–
0.09
04(0
.765
3)0.
0673
(0.7
967)
DR
TB
0.37
33(0
.544
7)22
.400
8*
*(0
.000
0)0.
4737
(0.4
954)
13.3
617
**
(0.0
008)
4.09
44*
*(0
.049
9)–
0.59
69(0
.444
4)D
RC
I0.
8279
(0.3
685)
0.07
51(0
.785
5)21
.509
0*
*(0
.000
0)8.
1849
**
(0.0
068)
3.14
98*
(0.0
837)
0.08
95(0
.766
5)–
Notes:
Th
ev
alu
esin
par
enth
eses
are
thep-
val
ue.
** ,
* in
dic
ate
sig
nifi
can
ceat
5an
d10
per
cen
tle
vel
s,re
spec
tiv
ely
Table VIII.Results of error correctionestimates for theunderlying factors ofexchange rate volatilityoriginated from relativemacroeconomic variables– Thailand
SEF24,4
280
Dep
end
ent
var
iab
les
Ind
epen
den
tv
aria
ble
s
DE
RV
DR
ID
RM
DR
CP
ID
RIP
DR
TB
DR
CI
EC
Tt2
1
Per
iod
:19
85:M
1-20
03:M
9F
-sta
tist
ics
T-s
tati
stic
s
DE
RV
–2.
2542
(0.1
347)
2.95
12*
(0.0
873)
2.55
42(0
.111
5)1.
4069
(0.2
369)
1.23
25(0
.268
2)9.
8905
**
(0.0
019)
1.41
81D
RI
0.74
99(0
.387
5)–
1.44
98(0
.229
9)1.
6404
(0.2
017)
7.02
70*
*
(0.0
086)
0.20
20(0
.653
6)0.
1956
(0.6
587)
3.16
51*
*
DR
M0.
5942
(0.4
417)
4.66
52*
*
(0.0
319)
–0.
2447
(0.6
213)
3.23
77*
*
(0.0
734)
0.40
53(0
.525
0)0.
7049
(0.4
021)
21.
1492
DR
CP
I1.
8736
(0.1
725)
0.61
54(0
.433
6)0.
0175
(0.8
948)
–0.
7700
(0.3
812)
0.47
52(0
.491
3)2.
0867
(0.1
501)
20.
6482
DR
IP0.
4607
(0.4
981)
0.44
63(0
.504
8)1.
7216
(0.1
909)
5.66
99*
*
(0.0
181)
–0.
1006
(0.7
514)
0.84
96(0
.357
7)6.
6212
**
DR
TB
0.11
26(0
.737
5)0.
0702
(0.7
913)
3.95
58*
*
(0.0
480)
0.21
31(0
.644
8)2.
6289
(0.1
064)
–0.
4107
(0.5
223)
1.28
50D
RC
I0.
2335
(0.6
294)
0.00
29(0
.956
8)0.
3356
(0.5
630)
0.06
28(0
.802
4)0.
0424
(0.8
370)
4.30
09*
*
(0.0
393)
–2
0.64
47
Notes:
Th
ev
alu
esin
par
enth
eses
are
thep-
val
ue.
** ,
* in
dic
ate
sig
nifi
can
ceat
5an
d10
per
cen
tle
vel
s
Table IX.Results of error correction
estimates for theunderlying factors of
exchange rate volatilityoriginated from relative
macroeconomic variables– Singapore
Factors ofexchange rate
volatility
281
respectively, wherein its own shock is only about 4 per cent. The innovations inThai baht volatility are explained mostly by its own shock for about 60 per cent.This is followed by the shocks of relative money supplies and consumer priceindices which are about 13 and 12 per cent, respectively. Meanwhile, theinnovations of the Singapore dollar volatility are explained best by its own shock,which is almost 97 per cent. It is only explained by the shock in relative tradebalances and money supplies for about 1.4 and 1.1 per cent. This implies that thevolatility of Singapore dollar has high-exogoneity compared with other variables.Overall, the innovations in the exchange rate volatility of the Malaysian ringgit,the Thai baht and the Singapore dollar are relatively exogenous, in which after
Relative forecast error variance for ERVOwing to innovation in (percentage of variation in)
Horizon (monthly) DERV DRI DRM DRCPI DRIP DRTB DRCI
1 87.6599 2.4460 4.1026 1.4266 0.3777 2.9078 1.079412 63.0010 2.1779 10.2907 3.0509 2.6492 15.6434 3.186824 57.9680 2.1343 11.4377 3.3990 3.0348 18.4781 3.548148 55.3590 2.1142 12.0466 3.5250 3.2333 19.9831 3.7389
Table X.Generalised variancedecompositions ofexchange rate volatilityfor Malaysia
Relative forecast error variance for ERV:Owing to innovation in (percentage of variation in)
Horizon (monthly) DERV DRI DRM DRCPI DRIP DRTB DRCI
1 47.8493 3.0859 5.1632 15.7791 10.4572 2.1192 15.546112 11.7248 25.7699 13.1205 24.7808 3.0599 1.8262 19.717924 6.8546 34.1483 15.2322 25.3422 1.7940 1.2771 15.351648 4.2647 37.5477 16.0735 25.9049 1.1281 0.9861 14.0951
Table XI.Generalised variancedecompositions ofexchange rate volatilityfor Indonesia
Relative forecast error variance for ERV:Owing to innovation in (percentage of variation in)
Horizon (monthly) DERV DRI DRM DRCPI DRIP DRTB DRCI
1 68.8558 2.3349 8.5605 11.1025 0.1999 0.9997 7.946612 62.5067 3.3825 12.7562 10.4582 0.3915 2.8698 7.635224 58.3759 6.1288 12.4696 10.5846 0.5328 4.2630 7.645448 60.3854 0.8919 12.5279 11.4639 0.6900 4.9899 9.0511
Table XII.Generalised variancedecompositions ofexchange rate volatilityfor Thailand
Relative forecast error variance for ERV:Owing to innovation in (percentage of variation in)
Horizon (monthly) DERV DRI DRM DRCPI DRIP DRTB DRCI
1 97.7934 0.2688 0.7074 0.2198 0.7143 0.2708 0.025612 97.0981 0.1310 1.0562 0.1153 0.3064 1.2089 0.084124 96.9881 0.1153 1.0979 0.1025 0.2730 1.3324 0.090948 96.9289 0.1065 1.1207 0.0956 0.2553 1.3987 0.0944
Table XIII.Generalised variancedecompositions ofexchange rate volatilityfor Singapore
SEF24,4
282
48 months, over 50 per cent of their forecast variances are explained by their ownshocks. As a comparison among the four economies, the exchange rate volatility ofIndonesia seems to be the most endogenous in which it is the most sensitive andits innovation is explained by most of other factors than its own shock.
5. Summary and concluding remarksThe empirical results are suggestive of the existence of long-run macroeconomicfactors of exchange rate volatility in all the economies except for Thailand. It impliesthat the exchange rate volatility and macroeconomic factors are moving together toachieve the long-run equilibrium for all the three countries of Malaysia, Indonesia andSingapore. The short-run results of the macroeconomic factors of exchange ratevolatility, however, show that a set of common macroeconomic factors seem toinfluence the exchange rate volatility for each of the four countries. The findingsindicate that the significant common set factor influences the exchange rate volatility isonly generated from stock market. Hence, capital market seems to play a significantinfluence to exchange rate volatility in all the economies examined.
As a comparison, the Singapore dollar volatility is mostly explained by its owninnovation whereas the volatility of Indonesian rupiah is greatly influenced bymacroeconomic variables rather than its own innovations. Since, both the long- andshort-run factors of exchange rate volatility from the macroeconomic perspective arefound, the exchange rate volatility is still a manifestation of the macroeconomicvariables. By understanding the impact of the imbalance of the macroeconomicfundamentals, one can, in a way, smooth the exchange rate variability and at the sametime, generate a greater flexibility in pursuing the economic policies given the greaterexchange rate stability. Particularly, the role of respective authorities and marketplayers in the four countries are imperative in managing a viable capital market so asto ensue exchange rate stability.
Notes
1. The orders of p and q are assigned as (2,2), (1,1), (1,1) and (2,2), respectively, for the currenciesexamined.
2. Malaysia had ended its peg system on 20 July 2005 and starting from 21 July 2005, itsexchange rate system was back to the managed float system.
3. The conditional standard deviation of exchange rate is computed via E-GARCH method. Thep and q orders for the four economies-Malaysia, Indonesia, Thailand and Singapore are (1,2),(1,2), (2,2) and (2,2), respectively. The selection of p and q is based on the Schwartz criteria.
4. For Malaysia, income ( y) refers to industrial production index; for Indonesia, it denotes grossnational product (GNI); for Thailand, it represents manufacturing production index; forSingapore, it indicates total manufacturing index.
5. For Malaysia, interest rate (i ) refers to Treasury bill rate; for both Indonesia and Thailand, itrefers to three-month discount rate; for Singapore, it denotes to three-monthTreasury-bill rate.
6. For all the four economies, inflation index ðpÞ refers to consumer price index.
7. For Malaysia, ci represents KLSE composite index; for Indonesia, it refers to Jakarta StockExchange Index; for Thailand, it is SET Stock Exchange Index; for Singapore, it is StraitTime Index.
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8. The unit root results showed that all the series are generally integrated of order one.The results are available upon request.
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Further reading
IMF (n.d.a) IMF Annual Report on Exchange Arrangement and Exchange Restriction, variousseries.
IMF (n.d.b) IMF Annual Report on International Financial Statistics, various series.
Corresponding authorChong Lee-Lee can be contacted at: [email protected]
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