dilemma not trilemma - 2013 rey
TRANSCRIPT
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DilemmanotTrilemma:
TheGlobal
Financial
Cycle
and
Monetary
Policy
Indepe
HlneRey*
LondonBusinessSchool,CEPRandNBER
August2013
Abstract
Thereisaglobalfinancialcycleincapitalflows,assetpricesandincreditgrowth.
withtheVIX,ameasureofuncertaintyandriskaversionofthemarkets.Assetma
withmorecreditinflowsaremoresensitivetotheglobalcycle.Theglobalfinanc
alignedwithcountriesspecificmacroeconomicconditions.Symptomscangofro
assetpricebubblesandexcesscreditcreation,whichareamongthebestpredict
crises.
A
VAR
analysis
suggests
that
one
of
the
determinants
of
the
global
financipolicyinthecentrecountry,whichaffectsleverageofglobalbanks,capitalflows
intheinternationalfinancialsystem.Whenevercapitalisfreelymobile,thegloba
constrainsnationalmonetarypoliciesregardlessoftheexchangerateregime.
Forthepastfewdecades,internationalmacroeconomicshaspostulatedthetril
capitalmobility,independentmonetarypoliciesarefeasibleifandonlyifexchan
floating.Theglobalfinancialcycletransformsthetrilemmaintoadilemmaora
duo:independent
monetary
policies
are
possible
if
and
only
if
the
capital
accoun
Soshouldpolicyrestrictcapitalmobility?Gainstointernationalcapitalflowshav
whetherincalibratedmodelsorinthedata. Largegrossflowsdisruptassetmar
intermediation,sothecostsmaybeverylarge.Todealwiththeglobalfinancialc
dilemma,wehavethefollowingpolicyoptions:(a)targetedcapitalcontrols;(b
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Introduction
Ifonelooksattheevolutionoffinancialintegrationoverthepasthalfcenturyin
onemightconcludethatfinancialopennessisanirresistiblelongruntrend,haile
andacademiceconomistsalike.Bothemergingmarketsandadvancedeconomie
openedtheirborderstofinancialflows. Thescopeforinternationalcapitalflows
gainsortodoharmhaswidenedconsiderablysincethe1990s.
Ininternationalmacroeconomicsandfinanceweoftenthinkwithintheframewo
trilemma:inafinanciallyintegratedworld,fixedexchangeratesexportthemo
centrecountrytotheperiphery.Thecorollaryisthatiftherearefreecapitalflow
haveindependentmonetarypoliciesonlybyhavingtheexchangeratefloat;and
floatingexchangeratesenablemonetarypolicyindependence(seee.g.Obstfeld
Butdoesthescaleoffinancialglobalizationandinparticulartheroleofglobalba
intoquestion?Arethefinancingconditionssetinthemainworldfinancingcentr
fortherestoftheworld,regardlessoftheexchangerateregime?Isthereaglob
ifyes,whatareitsdeterminants?
Riskyassetpricesaroundtheglobe,fromstockstocorporatebonds,haveastron
component. Sodocapitalflows. Creditflowsareparticularlyprocyclicalandvol
cyclesandcapitalflowsobeyglobalfactors,theymaybeinappropriateforthecy
many
economies.
For
some
countries,
the
global
cycle
can
lead
to
excessive
credtimesandexcessiveretrenchmentinbadtimes.Astherecentliteraturehasconf
creditgrowthisoneofthebestpredictorsofcrisis(GourinchasandObstfeld(201
Taylor(2012)).Globalfinancialcyclesareassociatedwithsurgesandretrenchme
b d b t i t i d i Th i t i i th t f
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Butevenifcapitalflows,especiallycreditflows,arelargelydrivenbyaglobalfac
bringimportantbenefitstotheworldeconomy. Abriefreviewoftheempiricale
quantificationofstandardgrowthmodels,however,showshowelusivewelfareg
flowsappeartobe,thoughitcouldjustbethattheyarehardtomeasure.
InpartI,Idescribethecharacteristicsofcapitalflows(grossandnet),showimpr
movementingrossflowsanddiscusshowtheyrelatetoglobalfactors,asproxie
theVIX. InpartII,Ishowtheexistenceofanimportantcommonfactorininterna
whichisalsocloselyrelatedtotheVIX. Iconcludethatthereisapotentglobalfi
grosscapitalflows,creditcreationandassetprices,whichhastightconnectionsw
uncertaintyandriskaversion.PartIIIanalysestheassociationofdifferenttypeso
theglobalfinancialcycleandreinforcestheconclusionthatcreditflowsareparti
theglobalfinancialcycle. InpartIV,Ihuntforthedeterminantsoftheglobalfina
anditstransmissionmechanism,focusinginparticularontheroleofmonetaryp
country,ontheleverageoffinancialintermediaries,creditcreationandcreditflo
thatourfindingsinvalidatethetrilemmaandleadtoadilemma,anirreconc
independentmonetarypoliciesarepossibleifandonlyifthecapitalaccountisma
indirectlyviamacroprudentialpolicies.PartVIdiscussesbrieflythefindingsofthe
gainstocapitalmobility. Iconcludethatmacroprudentialpoliciesarenecessary
policyindependenceforthenoncentralcountries.Theycansubstituteforcapita
iftheyarenotsufficient,capitalcontrolsmustalsobeconsidered.
I ) The global financial cycle and international capital flows
A)Characteristicsofinternationalcapitalflows
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spikes.Morerecently,ForbesandWarnock(2012)andBrunoandShin(2013a)e
incapitalflowsassociatedwiththeloweringoftheVIX.
Figure2plotscapitalinflowsdisaggregatedbyassettypes(FDI,portfolioequity,
credit)asaproportionoftheworldGDPfortheperiod1990Q12012Q4anditre
(invertedscale)onthesamegraph.Particularlystrikingistheprolongedlowering
theperiod20022007,duringwhichcapitalinflowssurged.Flowstendtobehigh
oneanotherandnegativelycorrelatedwiththeVIX(exceptFDI).Creditinflowsa
inflowsshowahighdegreeofcomovementovertime(correlationof0.52).Cred
morevolatileandprocyclicalcomponentofallflowswithaparticularlydramatic
tothecrisisandanequallydramaticcollapseduringthecrisis.Theircorrelationw
(invertedscale)is0.24onthewhole1990Q12012Q4sample(quarterlydata).
[Figure2here]
InTable1(a),Ipresentthecorrelationsbyregionsofeachtypeofinflowswithth
inflowsarenegativelycorrelatedwiththeVIX,evenatageographicallydisaggreg
Overwhelmingly,duringtranquilperiodscharacterisedbylowVIX,whenuncerta
aversionarelow,capitalinflowsarelarger.Inlinewithaggregatedata,theonlyc
exceptionsareFDIinflowsforwhichthecorrelationwiththeVIXispositiveinall
CreditflowsintodevelopedeconomiesinAsiaarealsopositivelycorrelatedwith
Table1(a):UnconditionalcorrelationsofliabilityflowswiththeVIX,quarterly,19
Correlations
inflows/VIXNorth
America
Latin
America
Central
Eastern
Europe
Western
Europe
Emerging
Asia
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fluctuationsincapitalinflows,exceptforFDIinflows.Theresultsaresimilarwith
theunconditionalandfortheconditionalcorrelationsfortheUSandWesternEu
weakerfortheothergeographicalareas. Incontrast,andinagreementwithour
thesamepatternofcorrelationsdoesnotholdfornetflows.Idonotreportthes
spaceconstraints.
Table1(b):ConditionalcorrelationsofliabilityflowswiththeVIX,quarterly,1990
Correlations
inflows/VIXNorth
America
Latin
America
Central
Eastern
Europe
Western
Europe
Emerging
Asia
Equity0.06 0.31 0.32 0.38 0.08
FDI0.10 0.35 0.07 0.06 0.08
Debt0.30 0.15 0.36 0.23 0.28
Credit0.29 0.15 0.16 0.24 0.26
InTable1(c),IinvestigatewhetherfluctuationsintheVIXarealsoassociatedwit
creation
and
leverage
using
various
measures.
We
report
the
conditional
correlaagainfortheclassicpushfactors(worldgrowthrateandshorttermrealrate). Fo
(2012),Imeasureleverageastheratioofprivatecreditbydepositmoneybanks
institutionstobankdeposits,includingdemand,timeandsavingdepositsinnonb
definitionsofleverageanddomesticcreditcanbefoundinAppendixB.
Table1(c)offersthisstrikingfinding:inallareasoftheworld,creditgrowthisne
theVIX.CorrelationstendtobethestrongestinNorthAmericaandWesternEur
leveragegrowtharealsonegativelyrelatedtotheVIXinallthemainfinancialce
America,WesternEuropeandAsia),whicharethehomesoftheglobalbanks. B
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Correlations
credit/VIXNorth
America
Latin
America
Central
Eastern
Europe
Western
Europe
Emerging
Asia
Domesticcredit
growth0.26 0.14 0.14 0.11 0.01
Leverage 0.17 0.05 0.30 0.09 0.12
Leverage
growth0.32 0.06 0.07 0.21 0.06
Tosumup,thedatashow(i)commonalityincapitalinflowsandoutflowsac
andtypesofassets(exceptforFDIflowsandasubsetofAsianandAfricanflow
commonalityisparticularlystrongforcreditandportfoliodebtinflows(seeFigu
isabsentfornetcapitalflows(Figure1c);(ii)surgesingrosscapitalflowsinper
volatilityanddeclineinflowswhentheVIXgoesup(withtheexceptionofFDIf
volatilityandprocyclicalityofcreditflows(seeFigure2andTables1a,b);(iii)in
creditgrowtharoundtheworldinparallelwithfallsoftheVIX(seeTable1c);(i
leverageandleveragegrowthinallthemainfinancialcentreswhentheVIXislo
1c).
AsnotedinBrunnermeieretal.(2012)andShin(2012),creditflowsgrewatav
the20032007precrisisperiodandcollapsedduringthefinancialcrisis.Thepa
inflowsandoutflowsfollowsaglobalfinancialcyclewhichissynchronizedwith
worldmarketriskaversionanduncertaintyasproxiedbytheVIX.Furthermore,
creditcreationinthebankingsectorandleveragearedancingtothesametune
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countryspecificandcompanyspecificfactors.But,asshownbyMirandaAgrippi
usingalargecrosssectionof858riskyassetpricesdistributedonthefivecontine
partofthevarianceofriskyreturns(25%)isexplainedbyonesingleglobalfactor
remarkablegiventhesizeandtheheterogeneityoftheset. Irrespectiveoftheg
ofthemarketinwhichtheassetsaretradedorthespecificassetclasstheybelon
loadtoalargeextentonthisglobalfactor.
AsapparentfromFigure3,takenfromMirandaAgrippinoandRey(2012),thefa
withthetimingofmajoreventssuchastheGulfWarstartingfromthesecondha
thefirstquarterof2009whenthemostrecentfinancialcrisisreacheditsclimax.
goesupfromtheearly1990suntilmid1998whentheRussiancrisiseruptsfollow
bankruptcy,andeventuallytheburstingofthedotcombubble.Fromthebeginni
index
increases
rapidly
until
the
beginning
of
the
third
quarter
of
2007.
This
is
shcollapseofthesubprimemarketandcoincideswiththefirstsignalsofincreased
financialmarkets. ThehighdegreeofcorrelationoftheglobalfactorwiththeVIX
BuildingontheanalysesofAdrianandShin(2008)andDanielsson,ShinandZygr
MirandaAgrippinoandRey(2012)proposeastructuralinterpretationofthefact
understoodasreflectingthejointevolutionoftheeffectiveriskappetiteofthem
realizedmarketvolatility.Inturntheeffectiveriskappetiteofthemarketcanbe
totheleverageofasubsetoffinancialmarketintermediarieswhoseinvestment
approximatedbyaVaRconstraint(brokerdealerintheUS,largeEuropeanbanks
tradingoperationsand,moregenerally,banksclassifiedinthecapitalmarketc
Bankscope5).Giventhatstructuralinterpretation,itisnotsurprisingthatthefact
empiricallybeclosely(negatively)correlatedwiththeVIX. AspointedoutinBru
(2012)andBorioandDisyatat(2011),thereisapositivefeedbackloopbetweeng
supply,assetpriceinflation,andacompressionofspreads.Smallerriskpremium
boom. Measured risk is low and balance sheets look healthier as asset prices go u
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Figure3:GlobalfactorandVIX. Source:MirandaAgrippinoandRey(2012).
Tosumup,wehavenowestablishedinflowdata(acrossmosttypesofflowsand
someexceptions)andinpricedata(acrossasectorallyandgeographicallywidec
assetprices)theexistenceofaglobalfinancialcycle.Interestingly,theVIXisapo
globalfinancialcycle,whetherforflowsorforreturns. Ouranalysissofarempha
correlationsandpatterns,butcannotaddresscausalityissues. Lowvalueofthe
longperiodsoftime,areassociatedwithabuildupoftheglobalfinancialcycle:m
andoutflows,morecreditcreation,moreleverageandhigherassetpriceinflatio
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volumesanddifferenttypesofcapitalflowsmatterforthesensitivityofnational
globalfactor.
Iinvestigatewhethercrosssectionally,thesensitivitiesofcountryspecificvariab
factor(logged)canberelatedtodifferenttypesandintensitiesofcapitalflo
market.Thecountryspecificvariables , arestockmarketreturns, ,banking
growth, , andhousepriceinflation, . Irunthefollowingsetofregressions
,
wheredenotesflowsintocountryi (inflows,outflows,differenttypesofflo
theGDPofcountryi, isavectorofcontrolvariables(laggedGDPgrowthofc
nominaleffectiveexchangerate ofcountryi). Ialsoinclude,thechangei
The
interaction
terms
and
are
meant
to
capture
the
pheterogeneoussensitivityofagivenmarkettotheglobalfinancialcycledependi
andtypesofcapitalflowsitreceivesorexports.Irunfixedeffectsestimatorswit
standarderrorsbycountryandincludealineartimetrend. Wecheckedthestat
usingaPesarantest.Wehavealargenumberofobservations(between2770an
onthespecification).Table2reportstheresultsofselectedspecifications.Panel
resultsforstockmarketreturns(logdifferenceoflocalstockmarketindices),App
resultsfor2(b)bankingsectorleveragegrowth(differenceofleverageratio)and
priceinflation(logdifferenceofpropertypriceindices).
Table2(a)Stockmarketreturnssi,t isthedependentvariable(1990
flit CreditL C.nonbankL CreditA DebtL DebtA E
VIXt
0.0952*** 0.0914*** 0.0951*** 0.0952*** 0.0962***
(12.64) (12.78) (12.25) (12.66) (12.34)
*** *** *** *** ***
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Panel
(a)
shows
that
stock
prices
are
significantly
negatively
related
to
the
globaltoitsgrowthrate.Creditflowsintoandoutofcountryitendtobeassociatedwi
sensitivityofthestockmarketofcountryitotheglobalfinancialcycle(theintera
significantlynegative).But,interestingly,debtoutflowsandespeciallyequityinfl
tendtobeassociatedwithalessersensitivitytotheglobalcycle(interactionterm
sectionally,justlikeinthetimeseries,creditflowsseemmorestronglyrelatedto
thanotherflowsandinparticularthanequityflows.
AscanbeseeninAppendixC,theresultsforbanksleverage(b)andhouseprices
somerespect. Thereisanegativecorrelationofbanksleverageandhouseprice
VIXandapositivecorrelationwiththegrowthrateoftheVIX.Thereishoweveri
nosignofanyflowsassociatedwithahighersensitivityofleverageofbanks(oro
theglobalfinancialcycle(theinteractiontermisneversignificant).
Onceagain,itisworthemphasizingthattheseregressionsindicatecorrelationsa
thetimeseriescreditflowsareveryprocyclical. Inthecrosssection,creditflows
associatedwithastrongercorrelationofstockmarketreturnswiththeglobalcyc
flowstendtobeassociatedwithaweakercorrelation6.
IV)Monetarypolicy,capitalflowsandtheglobalfinancia
A)RecursiveVARanalysis
Theglobalfinancialcycleappearsincomovementsofgrossflows,assetprices,le
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raisinglargequantitiesoffundsindollarsandtransferringthemtooverseasmar
globalbankswerenotonlyintermediatingsavingsbackintheUSmarketbutwer
Asian,LatinAmerican,AfricanandMiddleEasternmarkets. Iwillthereforetreat
Europeanbanksasakeyvariableoftheanalysis.Thedollaristhemaincurrency
Sincesurgesincapitalflows especiallycreditflows areassociatedwithincreas
worldwide,anaturalinterpretationisthatmonetaryconditionsinthecentrecou
transmittedworldwidethroughthesecrossbordergrosscreditflows. Itisthere
flowsthatshouldbetrackedinordertoassessfinancialfragilityandoverallcred
emphasizedbyBorioandDisyatat(2011),Gourinchas,TruemplerandRey(2012)
(2012). Itisalsoonlybylookingatgrossflowsthatonecankeeptrackofcurrenc
mismatchonbalancesheetsoffinancialintermediariesandhouseholds.Bothof
arewellknowncontributorstofinancialinstability.
Thisisofcoursenottosaythatnetflowsareirrelevant: currentaccountimbalan
longrunsustainabilityofthenetexternalassetposition,asalongliteratureshow
surveyedinGourinchasandRey(2013)).
Toanalyzethedynamicinteractionbetweenmonetarypolicy,riskaversionandu
leverageand
credit
flows,
Iperform
arecursive
VAR
analysis
7
.Ibuild
on
the
stud
HoerovaandLoDuca(2012).Theyshowthatmovementsinthefederalfundsrat
uncertainty(expectedstockmarketvolatility)andriskaversion,twocomponents
theVIX. Likethem,Ifocusonthedynamiclinksbetweenthefederalfundsratea
alsostudytheirdynamicinterrelationswithcreditcreation,leverageandcreditf
quarterlydatafortheperiod19902012.Iimposecontemporaneousrestrictions
responsesofthevariables,basedoninstitutionalknowledge.Iorderthevariable
variablecannotrespondtocontemporaneousshocks(withinthequarter)ofany
secondonecanrespondtocontemporaneousshocksaffectingvariable1butnot
I th t GDP d i d ith l th l i hil
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banksleverage(definedasthemedianofEUbankleverage)(EULEV),FedFundst
VIX(logged).8
Inotethatsincewearefirstandforemostinterestedintheimpactoftheshocks
variablesintheVAR(VIX,FFRandleverage),howtheothervariablesareordered
differenceforthosethreeshocks(allIneedispartialidentification). Forexampl
bothcreditandflowswillstayputinthefirstquarterandthenarefreetoreact,
ofthosetwodoesnotmattertoFFR.Thatorderonlymattersinbetweenthetwo
assuming thatiftherewereashockoncrossborderflows, globalcreditwouldt
reacttothat,butIamnotfocusingonthis.
IuseatwolagVAR,usingtheusualcriteria(BICandLR). Bootstrappedconfiden
computedusing1000replications;lightanddarkgreyshadedareascorrespondt
confidenceintervalsrespectively. Ireportasubsetofkeyimpulseresponsesint
and4b).ThecompletesetofimpulseresponsefunctionsarereportedinFigure5
Ourkeyfindingsarethefollowing:
(i) Anincreaseintheeffectivefederalfundsrate(FFR)leadstoanincreabout5quartersanduntil11quarters. (Figure4a)
(ii) AnincreaseintheVIXleadstoafallinEuropeanbanksleverage.(Fig(iii) AfallintheVIXleadstoanincreaseincrossbordercreditflowsupto
4b)
(iv) AnincreaseintheVIXleadstoafallinglobaldomesticcreditfrom4(Figure
4b)
(v) AnincreaseintheVIXleadstodeclineintheFFR.(Figure4b)(vi) AnincreaseintheFFRleadstoafallinEUbankleverageafter15qua(vii) AnincreaseintheFFRleadstoafallingrosscreditflowsafter12qua
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TheVARresultsarethereforeconsistentwiththefollowinginterpretation.When
rategoesdown,theVIXfalls(afterabout5quarters),Europeanbanksleverager
creditflows(after12quarters). AfallintheVIXleadstoanincreaseinglobaldo
quarters.
FurthermoreIfindthatincreasedbankleverageandcapitalflows,aswellascred
(thoughforcredititisonlymarginallysignificant)areassociatedwithasubseque
index.Thisisconsistentwiththefollowingmechanism:ascreditandcapitalflow
asnotedinparticularbyAdrianandShin(2010),thequasiconstancyofriskweig
balancesheetofglobalbanks(mostlythebankshavinglargecapitalmarketdivis
theunweightedvolumeofassetsrisessubstantiallysuggestsafallinmeasuredr
times. Whenleverageishighandcreditisabundant,spreadsarecompressedan
low.ThistranslatesintoadeclineintheVIX. Thereisthereforeapositivefeedba
loosemonetarypolicy,fallintheVIX, riseincredit,capitalflowsandleveragean
VIX9.
FromFigure5,IalsonotethatanincreaseintheVIXhasasignificantnegativeef
Bloom(2009))andontheGDPdeflator.Asexpected,anincreaseintheFFRrate
effectonprices. IalsonotethatmonetarypolicyloosenswhentheVIXgoesup(
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Figure4b:Responsestoa1%increaseintheVIX.
B)Robustness
Icheckrobustnessontheprecrisissample19902007.Ialsocheckrobustnessby
ourvariables(Idropsuccessivelycredit,leverage,flowsonebyone)andbydrop
sureoverfittingisnotanissue. Importantly,twostudieswithadifferentfocusb
results(Bekaertetal.(2012)andBrunoandShin(2013b),allowustoassessfurth
ofsomeofthefindings.
Bekaertetal.(2012)decomposetheVIXindexintoacomponentreflectingexpec
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BrunoandShin(2013b)runsa4variablerecursiveVARwithFFR,logVIX,leverag
effectivedollarexchangerateonquarterlydatafortheperiod19952007.Form
measurestheyusetherealFFRandtherealeffectiveFFR,growthofUSM1,and
Taylorrule.TheyuseUSbrokerdealerleverageinsteadofthebroadermeasureo
TheyfindthatapositivemonetarypolicyshockleadstoanincreaseintheVIXaft
declineinUSbrokerdealerleverageafterabout10quarters;anincreaseintheV
inUSbrokerdealerleverageafterquarter10.Theseresultsarecompatiblewith
(ii) withsomedifferencesintiming. Theauthorsalsofind,afteraugmentingthe
increaseintheFFRreducescreditflows(intheircasedefinedasthefirstdifferen
liabilitiesofbankslocatedoutsidetheUS)afterabout7quarters;thatanincreas
flows.Theseadditionalresultsarealsocompatiblewithmine(see(vii),(iii))with
intiming.BrunoandShin(2013b)presentinadditionveryinterestingevidenceo
effectiveexchangeratedynamicsandthedelayedovershootingpuzzle.
C)Economicsignificanceoftheresults
Aretheshockstothefederalfundsrateanimportantsourceofvariationfortheglobalfinancialcycle,indexedbytheVIX?
Intheir4variableVAR,BrunoandShin(2013b)findthatshockstotheFFRexplai
varianceoftheVIXathorizonslongerthan10quarters.
Similarlyintheir4variablestructuralVARmodel,Bekaertetal(2012)findthatm
shocksaccountforover20%ofthevarianceofriskaversionathorizonslongerth
alsoaccountforacomparablepartofthevarianceofuncertainty.Intheirsixvar
monetarypolicyshockaccountsforabout12%ofthevarianceofriskaversionat
than10quarters.
DependingontheexactspecificationoftheVARanalysis,Ifindthatshockstothe
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V)Takingstock:monetaryconditions,capitalflowsand
financialcycle
Thereisaglobalfinancialcycleincapitalflows,assetpricesandincreditgrowth.
withtheVIX,ameasureofuncertaintyandriskaversionofthemarkets. Assetm
creditinflowstendtobemoresensitivetotheglobalcycle.Theglobalfinancialc
withcountriesspecificmacroeconomicconditions.Inanumberofcountries,thi
creditgrowth(oralternativelytomonetaryconditionswhicharetootight).Exces
oneofthebestpredictorsofcrisis.GourinchasandObstfeld(2012)showthatac
crisis,threevariablesplayastatisticallyandeconomicallysignificantrole:therat
credittooutput,therealexchangerate,andtheratioofofficialreservestooutp
Taylor(2012)demonstratethatcreditgrowthisapowerfulpredictoroffinancial
thatsuchcrisesarecreditboomsgonewrongandthatpolicymakersignorecr
SimilarfindingsareechoedinLundJensen(2012),whofindsthathighassetprice
associatedwithsystemicbankingcrises.Ouranalysisclearlyimpliesthatgrossflo
creditanddebt)shouldbemonitoredclosely(inparallelwithnetflowswhichare
sustainabilityissues)inordertoassessfinancialfragilityandoverallcreditcondit
bylookingatgrossflowsandgrosscrossborderpositions(theentirebalanceshe
thatonecankeeptrackofcurrencyandmaturitymismatch. Bothofthesemism
tocontributetofinancialinstability10
.
Theimportanceoftheglobalfinancialcycleincreatingboomandbustcyclesin
andadvancedeconomiesalikewithcapitalinflowssurgesgoesbackalongwaya
mentionedindifferentcontextsbyDiazAlejandro(1983),Calvoetal.(1996),(ide
factorsforcapitalflows),EichengreenandPortes(1987),ReinhartandReinhart
flowsbonanzas),LaneandMcQuade(2012)andmanyothers.Theroleofcross
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aworldoffreecapitalmobility,independentmonetarypoliciesarefeasibleifand
ratesarefloating.Instead,whileitiscertainlytruethatcountrieswithfixedexch
haveindependentmonetarypoliciesinaworldoffreecapitalmobility,myanaly
crossborderflowsandleverageofglobalinstitutionstransmitmonetaryconditio
underfloatingexchangerateregimes.
Soshouldpolicyrestrictcapitalmobility?
VI)Benefitsofinternationalcapitalflows
Ifrestrictingthemovementofcapitalacrossborderistobeapolicyoption,itspo
shouldbeassessedagainstitscosts.Sowhatdoweknowaboutthegainstointe
mobility?
Theliteraturehasattemptedtomeasuregainstofreecapitalmobilitymostlyint
calibratingstandardinternationalmacroeconomicmodelsandevaluatingwelfare
fromautarkytofinanciallyintegratedmarkets;bytestingforgrowtheffectsand
(lowervolatility)followingfinancialintegration,usingeitherpaneldataorevent
A)Calibrationofstandardmodels
Theneoclassicalgrowthmodelisbehindmanyofoureconomicintuitionsregard
freeflowofcapitalcouldbebeneficial. Withinthismodel,financialintegrationb
improvementsinallocativeefficiency(capitalflowstoplaceswiththehighestma
d b i k h i I i l i hi h di li i lib
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orderofafewtenthsofapercentofpermanentconsumptionforrealisticcalibra
B)Empiricalevidencefrompaneldataandeventstudies
Crossborderinvestmentpositionshaverisenforadvancedeconomiesfrom68%
438%ofGDPin2007;foremergingmarketstheyhavegonefrom35%to73%of
sameperiod(LaneandMilesiFerretti2007andLane(2012)). Ifcapitalflowsbrin
beobservinglargeeffectsinthedata,duetothesheerscaleoffinancialglobalisa
1990s.Therearenumerousstudiesthattrytotestforeffectsofinternationalcap
growthoronconsumptionvolatility.Surprisingly,theseeffectsarehardtofindin
data. Asattestedbythemostrecentsurveysreviewingalonglistofempiricalpa
find
robust
evidence
of
an
impact
of
financial
openness
on
growth
or
on
improveEichengreen2002;Jeanneetal.2012;Koseetal.2006;Obstfeld2009). Somepa
theexistenceofthresholdeffects:capitalflowsarebeneficialonlyafteracountr
certainamountofinstitutionalorfinancialsectordevelopment(seeBekaerteta
alsosomedifferencesifonelooksacrossdifferenttypesofcapitalflows:FDIflow
deliveringgrowthandrisksharingbenefitsthanothers. Butthisevidenceisnotv
becausethesampleusedoftenmakesadifference(seeJeanneetal.(2012)). Th
oneventstudiesisoftenmorepositive(seeHenry(2007))andpointstowardsaf
capitalandincreasedinvestmentatthetimeoffinancialintegration. Butthesim
economicreformsorpoliciesputinplaceatthetimeoffinancialopeningishowe
concern. Further,fromatheoreticalpointofview,evaluatingwelfaregainsrequ
pathofintegratingeconomiesfromthepointofcapitalaccountintegrationtoth
Alongsuchpaths,onecanobserveinitialinvestmentincreasesandcurrentaccou
thenreverselateronascountrieshavetorepaytheirexternaldebt.Welfaregain
are found to be small (see Coeurdacier et al (2013))
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ofcertaintypesofflows. Theexistingliteratureonthistopichastodealwithhar
issues andisalsonotveryconclusive(foradiscussionseeObstfeld2009,p.89).
possibilityisthatfinancialFDIfavoursfinancialmarketdeepeningandtherebyim
prospects11
. Yetanotherpossibilityistoinvestigatemorecloselytherisksharing
theexternalbalancesheetofcountriesduringcatastrophiceventssuchasthe20
financialcrisis.Gourinchasetal.(2012)showthatthereweremassivewealthtra
theUSandtherestoftheworldwhentheglobalfinancialcrisishit(about2trillio
valuationlossesontheUSnetexternalassetposition,whichisequivalenttoaw
totherestoftheworld).TheUS,centreoftheinternationalmonetarysystem,ac
insurer. Itiseasytoseehowthisinsurancetransferisimplemented:sinceemerg
tendtobelonginUSgovernmentdebt(thereserveasset)andshortequityandF
versafortheUnitedStates)12
,intimesofcrisisthevalueofalargepartoftheira
governmentbonds)isstableorevengoesupwhilethevalueoftheirliabilities,co
riskyassets,collapses.Thus,whilelargeexternalbalancesheetscanhelppropag
crisis,theycanalsocontributetorisksharingdependingontheirexactstructure
furtherreasonwhymonitoringgrossflowsandgrosspositions(asopposedtoon
currentaccounts)isessential.
Tosumup, gainstointernationalcapitalflowshaveprovedelusivewhetherinca
inthedata,thoughperhapsthisisjustbecausethosegainsarehardtomeasure.
mightoccurthroughimprovementsinTFP,whichwehavenotbeenabletomeas
thenwhydontweseethemingrowthrates?) ortheymightmanifestthemselve
large
shocks
hit.
One
thing
is
clear
at
this
stage:
we
cannot
take
them
for
grante
VII)Policyoptions:dealingwiththedilemma
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analysessuggestmonetaryconditionsaretransmittedfromthemainfinancialc
theworld throughgross credit flowsand leverage, irrespectiveof theexchang
putsthetraditionaltrilemmaviewoftheopeneconomyintoquestion.Fluctua
cannotinsulateeconomiesfromtheglobalfinancialcycle,whencapitalismobil
morphs into a dilemma independent monetary policies are possible if an
accountismanaged,directlyorindirectly,regardlessoftheexchangerateregim
Thisimplies
that
gross
flows,
particularly
credit
flows,
are
of
great
importance
fo
andhavetobemonitoredcarefully.Itisalsoonlybylookingatgrossflowsandg
positions(theentirebalancesheetofcountries)thatonecankeeptrackofcurre
mismatch. Bothofthesemismatcheshaveprovedtocontributetofinancialinsta
timeagain(seeforexampleFarhietal.(2012)). Oncemore,thisisnottosaynet
matter,astheyareimportantforsustainabilityissues14
.
Aswelfaregainsfromcapitalflowscannotbetakenforgranted(thoughthejury
shouldconsiderthefollowingrangeofoptionstoweakenthepotencyoftheglob
andtherebyincreasefinancialstability.Onecould:a) imposetargetedcapitalco
ofthesourcesofthefinancialcycleitself:themonetarypolicyoftheFedandoth
banks;c)actonthetransmissionchannelcyclicallybylimitingcreditgrowthand
upturnofthecycleusingnationalpolicies(andpossiblydoingthereverseduring
puttinginplacemacroprudentialpolicies;d)actonthetransmissionchannelstr
imposingstricterlimitsonleverageforallfinancialintermediaries.
a) CapitalcontrolsOnecouldconsidercapitalcontrolseithercyclicalorpermanenttoinsulatethee
global financial cycle. Permanent capital controls can be applied on subset of ass
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Temporarycontrols,especiallyoncreditflowsandportfoliodebtwhenthecycle
couldbeused.Thisoptionhasbeentestedinvariouscontexts: theChileanencaj
2010and2011Braziliantaxesonequityinflowsetc Oftenthough,controlshav
theprimaryaimofpreventingexcessiveappreciationoftheexchangerate.Whe
excessiveexchangerateappreciationmayhurttheexportsector. Asaresult,Ce
wishtointerveneontheforeignexchangemarkettokeepthecurrencydown,ac
reserves.Theyfacethetradeoffofhigherinflationorincreasedsterilizationcosts
effectofanincreasedinterestrateleadingtofurtherinflows(alsoreinforcedby
furtherappreciationoftheexchangerate).Taxinginflows,ifeffectivelyimpleme
circuitbreakerinsuchasituation. Thereisalivelydebateastherearealsodiffi
issueslinkedtoselectionandendogeneity ontheeffectivenessandsideeffects
controlsinthiscontext(seeforexampleForbesetal. (2012),ChamonandGarcia
(2012),Werning(2012)).
Ultimately,sinceinourcontext,itisreallyexcessivecreditgrowththatisthema
capitalcontrolsshouldbeviewedmoreaspartialsubstituteswithmacroprudent
tendtobemoretargeted. Butcapitalcontrolsmaybeappropriateifthereisalo
borderlendingandthebankingsystemcanbecircumvented(seeOstryetal(201
tonotethatmacroprudentialpoliciescanweakenthelinkbetweendomesticmo
capitalinflows,withouttheimpositionofcapitalcontrols.Forinstance,bypreve
creditgrowthinboomtimes,theCentralBankmayreducetheincentiveforbank
externallywhendomesticmonetarypolicytightens.
b) InternalisationoftheglobalspilloversofthecentresmonetarypolicyOnecouldconsideractingononeofthesourcesoftheglobalcycleitself,themo
inthemainfinancialcentres. Monetaryconditionsinlargefinancialcentressuch
theglobalfinancialcycleviatheendogenousresponseofleverageandtheprocy
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GlobalFinancialSystemoftheBIS.Thisgroupwoulddiscussandassesstheimpli
policiesforgloballiquidity,leverage,andexposures,andtheappropriatenessof
andcreditpoliciesfromthepointofviewofglobalprice,output,andfinancialsta
issueashortreportdiscussingpolicytradeoffsandinternationalinconsistencies.
shouldatleasthelptounderstandbetterthesecomplexissuesalsobystimulat
theseareasandmightencourageCentralBankerstointernalizesomeoftheex
thepolicies.Thedifficultiesofsuchapolicyoptionareobvious:internationalcoo
monetaryspilloversmayconflictwiththedomesticmandatesofcentralbanks.F
internationalfinancialstabilityanddomesticactivityandinflationtargetsmaybe
theshorttomediumrun. Furthermorethemanagementofaggregatedemandin
importanteconomiesalsohasimportantconsequencesforeconomicactivityint
world.Itiseasytoseethatthetradeoffsareextraordinarilycomplex.
c) Mutingthetransmissionchanneloftheglobalcyclebytakingcyclicalmeprudentialmeasures)tolimitexcessivecreditgrowth.
Since,foracountry,themostdangerousoutcomeofinappropriatelyloosegloba
conditionsisexcessivecreditgrowth,asensiblepolicyoptionistomonitordirect
andleverageineachmarket. Recently,muchefforthasgoneintoputtinginplac
measureshavingjustthisgoal.Thearsenalhasseverallayers. Basel3hasacoun
cushionthatcanbeactivatedinboomtimes.Loantovalueratiosanddebttoin
usedinordertorestrictlendingandkeeprealestatepricesincheck.Oneshould
lendingstandardsandtradingstrategiesduringperiodsofhighcreditgrowth. Th
experiencebeinggatheredaroundtheworldrecentlyonthepracticalimplement
prudentialtools(seeforexampletheReserveBankofIndiaortheBankofKorea
macroprudentialmeasureswereimposedincludingleveragecapsonFXderiv
d i l bili l li bili i f b k ( k f
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OneoptionistodeviseautomaticrulesbasedonthecredittoGDPratioandact
thresholdiscrossed(Borioetal.(2011)).Thishastheadvantageofbeingrobustt
interestedparties.Italsoovercomesthewellknownbiastowardsinactionwhen
unfoldingandeveryoneishappilysharingthedividendsofincreasingassetretur
theriskbuildingup.
Anotheroptionistostresstestthebalancesheetofthefinancialsector(banksa
banks)
very
frequently,
either
in
a
targeted
way
or
broadly,
and
judge
whether
larealisticchangesinassetpricescouldjeopardizefinancialstability.Stresstesting
exerciseingeneralandestimatingsecondroundeffectsisparticularlychallengin
Furthermore,thisisnotapopularundertakingwithmarketparticipants,asitreq
inputsontopofmandatoryreportings.Italsorequirescarefulthinkingaboutcom
policy(and/orabsoluteconfidentialityasthecasemaybe).Moreover,fiscalback
areneededtoguaranteethecredibilityofthestresstesting.Noneofthisiseasy.
stresstestsregularlyandoften,evenifthisisanimperfectprocess,isanecessary
tool. Itimprovestheknowledgeofsupervisorsandinsurestheyareuptodatew
marketdevelopments;importantlyitmayalsogiveconstructivechallengestoth
monitoringofinstitutions.Itmayrevealfailuresincorporategovernanceinorga
incentivesarenotnecessarilyalignedtokeepriskincheckorwhereinformation
orcentralizedadequately.Itmayevenrevealblindspotsofrisktakingactivitie
belowtheradarscreenoftheChiefRiskOfficer.Anaggressivepolicyoffrequent
sometargeted,somebroad,isthereforeanappropriateandflexiblewaytotackl
excessivecreditgrowthandleverage. Insteadofseekingtoidentifybubbles,sup
stresstestwhetherwhencurrentfinancingconditions(includingintheshadowb
getdisruptedandassetpricesdecline,financialstabilitycouldbeendangered15
.
brakesshouldbeappliedimmediately.
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Attheheartofthetransmissionmechanismdescribedinthispaperistheability
intermediaries,whetherbanksorshadowbankstoleverageupquicklytoveryhi
financingconditionsarefavourable.Creditisexcessivelysensitivetothefinancin
again,asinc)withtheusefulobservationthatthemostdangerousoutcomeofin
globalfinancialconditionsisexcessivecreditgrowth. Hence,asensiblepolicyop
additiontoorinsteadofmonitoringthecyclicalpropertiesofcreditgrowthisto
abilityoffinancialintermediariestobeexcessivelyprocyclical.Onepolicyleverse
appropriatefordoingthis:theleverageratio. Byputtingatougherlimitonlever
usefullyreducetheabilityofthefinancialsystemtoengageinthefeedbackloop
sectionsVandVI. Byusingsuchastraightforwardtool,onewouldalsohelpmak
macroprudentialpoliciesdescribedabovemorerobust.Errorsofjudgementsby
RiskOfficers,CEOsandboardsarepossibleandevenlikelyinourexcessivelycom
regulatoryenvironment.Tougherleverageratiosareasensiblewaytodecrease
costoftheseerrors,withoutimposinganylargecosts,ifatall,ontherealeconom
(2012),Jenkins(2012),AdmatiandHellwig(2013))16
.
Conclusion
Ofthesefouroptions,ifhistoryisofanyguidance,puttinginaplaceaneffective
cooperationamongthemaincentralbankstointernalisethespilloversoftheirm
therest
of
the
world
seems
out
of
reach
17
.
Andthere
are
some
reasons
for
that:
cooperationonmonetaryspilloversmayconflictwiththedomesticmandatesof
example,internationalfinancialstabilityanddomesticactivityandinflationtarge
atleastintheshorttomediumrun. Furthermorethemanagementofaggregate
g p y g ,
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levelofeconomicactivityanddemandstimulusinthesamecountries.Tradeoffs
complexandpolicyactionwillmostlikelyremainbiasedtowardsnationalpriorit
foruminwhichthecollectivemonetarypolicystanceofthesystemicallyimporta
activelydiscussedandinconsistenciesanalysedwouldneverthelessbebeneficial
Themostappropriatepoliciestodealwiththedilemmaareprobablytotakeac
aimedatthemainsourceofconcerns(excessiveleverageandcreditgrowth). Th
aconvexcombinationofawellthoughtoutimplementationofmacroprudential
aggressivestresstesting(b)andtougherleverageratios(c). Dependingontheso
instabilityandinstitutionalsettings,theuseofcapitalcontrols(a)asapartialsub
macroprudential measuresshouldnotbediscarded.
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AppendixA
Listofcountriesincluded:
NorthAmerica LatinAmerica Central&EasternEurope WesternEurope EmergingAsia ACanada Argentina Belarus Austria China A
US Bolivia Bulgaria Belgium Indonesia Ja
Brazil Croatia Cyprus Malaysia K
Chile CzechRepublic Denmark Thailand N
Z
Colombia Hungary Finland
CostaRica Latvia France
Ecuador Lithuania Germany
Mexico Poland Greece
Romania Iceland
RussianFederation Ireland
Serbia Italy
SlovakRepublic Luxembourg
Slovenia Malta
Turkey Netherlands
Norway
Portugal
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DataonCapitalflows:
Sourceof
flow
data:
quarterly
gross
capital
inflows
and
outflows
from
the
Intern
FundsInternationalFinancialStatistics(accessedthroughIMFwebsiteinMarch
PortfolioEquityInflows,OutflowsandNetFlowsconstructedasOutflowsInflow
FDIInflows,OutflowsandNetFlows
PortfolioDebtInflows,OutflowsandNetFlows,and
OtherInvestmentInflows,OutflowsandNetFlows
Datatransformations:FlowsarereportedinmillionsofU.S.dollars
IFSdoesnotdifferentiatebetweentruezerosandnotavailables;mostofthetim
valuesaserrorsandomissions,unlesstheyevidentlyrepresentzeroflows.
Mapping
of
the
flows
from
BPM5
(until
2004
Q4)
to
BP6
(2005
Q1
onwards)
in
acguidelinesofthe6theditionoftheBalanceofPaymentsandInternationalInvest
ManualofIMFReconciliationforquarters2005Q12008Q4forwhichthereis
ConstructionofNetFlowsonlywhendataonInflowsandOutflowsareavailable
WorldGDPGrowth(Quarterly):InternationalMonetaryFundsInternational
(accessedthroughIMFwebsiteinMarch2013).
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AppendixB
GlobalFactor:commonfactorextractedfromacollectionof858assetpriceserie
Pacific,Australia,Europe,LatinAmerica,NorthAmerica,CommodityandCorpora
detailsonextractionandoriginalassetpricesdatasetcompositionpleasereferto
andRey(2012).
BankingSectorLeverage:constructedastheratiobetweenClaimsonPrivateSec
TransferableplusOtherDepositsincludedinBroadMoneyofDepositoryCorpora
CentralBanks.DataareinnationalcurrenciesfromtheOtherDepositoryCorpora
MonetaryStatistics,InternationalFinancialStatisticsdatabase.Classificationofd
formerDepositMoneyBanksSurveycorrespondstoDemand,Time,Savingsand
Deposits.
EUBankingSectorLeverage:constructedasthemedianBankingSectorLeverage
EuroAreaCountries(Austria,Belgium,Finland,France,Germany,Greece,Ireland
theNetherlands,PortugalandSpain)andtheUK.
USBrokersDealersFinancialLeverage:constructedastheratioofSecurityBrok
FinancialAssetsandTotalLiabilities;FederalReserveBoard;FinancialAccounts,
DomesticCredit:constructedasthesumofdomesticclaimsofDepositoryCorpo
CentralBanks.DomesticclaimsaredefinedasClaimsonPrivateSector,PublicNo
Corporations,
Other
Financial
Corporations
and
Net
Claims
on
Central
or
Genera(ClaimslessDeposits);OtherDepositoryCorporationSurveyandDepositMoney
MonetaryStatistics;IFS.Originaldatainnationalcurrencies.
DirectCrossBorderCredit:measuredasdifferenceinclaimsonallsectorsorno
givencountryofallBISreportingcountriesinallcurrencies;LocationalStatistics
InternationalBankPositionsbyResidence;BIS;Tables7Aand7B.
GlobalInflows:constructedasthesumofdirectcrossbordercredittononbank
countriessampledforthepaneldataanalysis;listofcountriessampledattheen
NominalGDPDatainUSD:originaldatainnationalcurrenciesfromNationalSta
HaverAnalyticsconversionusingspotendofperiodFXrates.
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USINFLATION:GrossDomesticProduct:ImplicitPriceDeflator(Index2005=100)
EconomicAnalysis
FFRUS:EffectiveFederalFundRates,EndofPeriod(%p.a.);FederalReserveBoa
InterestRates,releaseH.15
Countriesinthepanel:Argentina,Australia,Austria,Belarus,Belgium,Bolivia,Br
Canada,Chile,Colombia,CostaRica,Croatia,Cyprus,CzechRepublic,Denmark,
France,Germany,Greece,HongKong,Hungary,Iceland,Indonesia,Ireland,ItalyLatvia,Lithuania,Luxembourg,Malaysia,Malta,Mexico,Netherlands,NewZeala
Portugal,Romania,Russia,Serbia,Slovakia,Slovenia,SouthAfrica,Spain,Sweden
Thailand,Turkey,UnitedKingdom,UnitedStates.
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AppendixC
Table2
Table2(b)BankingSectorLeverageGrowth, , isthedependantvaria
flit CreditL C.nonbankL CreditA DebtL DebtA
VIXt
0.0125*** 0.0122*** 0.0127*** 0.0121*** 0.0127***
(3.84) (3.82) (3.87) (4.02) (3.87)
VIXt
0.0164*** 0.0167*** 0.0171*** 0.0167*** 0.0174***
(4.06) (4.4) (4.44) (4.26) (4.39)
flit*VIXt0.00 0.0014 0 0.0007 0
(1.28) (1.39) (0.67) (1.09) (0.89)
flit
1*VIXt1
0.0002 0.0014 0 0.0001 0.0001
(0.61) (1.43) (0.56) (0.34) (0.67)
Adj.R2 0.01 0.008 0.008 0.009 0.008
N 2352 2405 2370 2273 2332
Fixedeffectestimator,standarderrorsadjustedforclusteringoncountry,tstati
specificationsincludethecontrolvariablesandalineartrend.
Table2(c)House priceinflation , isthedependantvariable(19902013)
flit CreditL C.nonbankL CreditA DebtL DebtA
VIXt
0.0174*** 0.0127*** 0.0170*** 0.0183*** 0.0179***
(3.66) (3.68) (3.52) (3.52) (3.74)
VIXt
0.0073*** 0.0051** 0.0072*** 0.0076*** 0.0082***
(2.91) (2.03) (2.88) (2.87) (3.5)
flit*VI
Xt
0.00 0.001 0.0001 0.0003 0
(1.04) (0.99) (1.07) (1.16) (0.3)
flit
1*VIX0.0001 0.0018 0 0.0001 0
(1 00) ( 1 11) ( 0 09) (0 56) (0 08)
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AppendixD:
Figures1a,b,c:heatmapsofcorrelationsofgrossinflows,grossoutflowsandne
Figure2: plotscapitalinflowsdisaggregatedbyassettypes(FDI,portfolioequit
andcredit)asaproportionoftheworldGDPfortheperiod1990Q12012Q4an
(invertedscale)onthesamegraph.
Figure5:CompletesetofImpulseresponsefunctionsoftheVAR.
CCCCCCC
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FDILatAm
0.41
0.10
0.08
0.29
0.3
20
.07
0.04
0.68
1.00
FDICE.EU
0.46
0.11
0.08
0.18
0.2
30
.12
0.09
0.61
0.65
1.00
FDI
W.EU
0.57
0.21
0.19
0.38
0.3
5
0.01
0.16
0.61
0.59
0.75
1.00
FDIEm.As
0.47
0.24
0.16
0.34
0.3
60
.04
0.04
0.65
0.77
0.69
0.64
1.00
FDI
Asia
0.36
0.16
0.03
0.29
0.3
00
.17
0.05
0.60
0.70
0.57
0.51
0.69
1.00
FDI
Africa
0.33
0.01
0.10
0.18
0.0
30
.16
0.19
0.31
0.36
0.35
0.35
0.34
0.27
1.0
0
DebtN.Am
0.42
0.17
0.32
0.51
0.2
9
0.21
0.31
0.40
0.39
0.55
0.51
0.48
0.37
0.0
8
1.00
DebtLatAm
0.20
0.40
0.33
0.16
0.1
3
0.00
0.05
0.16
0.35
0.13
0.05
0.31
0.26
0.0
6
0.10
1.00
DebtCE.EU
0.37
0.42
0.50
0.43
0.1
3
0.17
0.19
0.14
0.35
0.14
0.12
0.47
0.21
0.0
4
0.37
0.52
1.00
DebtW.EU
0.49
0.05
0.33
0.50
0.2
3
0.27
0.47
0.29
0.10
0.44
0.27
0.25
0.02
0.1
0
0.58
0.13
0.28
1.00
DebtEm.As
0.40
0.58
0.65
0.35
0.2
0
0.23
0.20
0.13
0.24
0.25
0.37
0.35
0.15
0.0
2
0.32
0.38
0.53
0.14
1.00
Debt
Asia
0.16
0.18
0.24
0.22
0.1
60
.04
0.16
0.35
0.31
0.30
0.30
0.45
0.26
0.1
4
0.45
0.27
0.42
0.19
0.39
1.00
DebtAfrica
0.26
0.27
0.39
0.18
0.0
7
0.14
0.09
0.12
0.21
0.10
0.01
0.41
0.21
0.0
7
0.21
0.46
0.61
0.15
0.44
0.32
1.
CreditN.Am.
0.29
0.02
0.21
0.38
0.1
50
.01
0.32
0.20
0.02
0.19
0.20
0.12
0.09
0.0
4
0.37
0.14
0.23
0.25
0.23
0.25
0.
CreditLatAm
0.41
0.34
0.21
0.26
0.1
2
0.04
0.22
0.38
0.35
0.42
0.27
0.48
0.35
0.2
4
0.35
0.25
0.41
0.30
0.29
0.46
0.
CreditCE.EU
0.42
0.25
0.27
0.28
0.3
2
0.15
0.21
0.54
0.38
0.72
0.55
0.47
0.36
0.2
8
0.54
0.14
0.13
0.56
0.25
0.48
0.
CreditW.EU
0.19
0.03
0.24
0.31
0.1
90
.16
0.26
0.27
0.08
0.20
0.30
0.19
0.13
0.1
5
0.45
0.20
0.25
0.33
0.26
0.45
0.
CreditEm.As
0.25
0.54
0.39
0.21
0.1
0
0.16
0.05
0.22
0.16
0.30
0.29
0.38
0.24
0.0
0
0.40
0.31
0.33
0.15
0.56
0.51
0.
CreditAsia
0.08
0.03
0.02
0.01
0.0
00
.40
0.12
0.23
0.23
0.32
0.24
0.31
0.23
0.2
5
0.32
0.18
0.17
0.01
0.13
0.37
0.
CreditAfrica
0.11
0.06
0.01
0.15
0.0
10
.20
0.12
0.40
0.30
0.35
0.33
0.24
0.37
0.1
8
0.32
0.11
0.00
0.13
0.03
0.34
0.
DDDDDDDCCCCCCC
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FDILatAm
0
.04
0.07
0.12
0.07
0.27
0.30
0.16
0.55
1.00
FDICE.EU
0
.03
0.21
0.18
0.04
0.42
0.44
0.11
0.65
0.63
1.00
FDI
W.EU
0
.26
0.26
0.40
0.23
0.53
0.66
0.26
0.66
0.62
0.77
1.00
FDIEm.As
0
.09
0.09
0.18
0.02
0.44
0.35
0.18
0.66
0.54
0.68
0.64
1.00
FDI
Asia
0
.12
0.09
0.02
0.18
0.45
0.37
0.30
0.49
0.60
0.57
0.58
0.68
1.00
FDI
Africa
0
.06
0.29
0.16
0.20
0.04
0.06
0.48
0.17
0.02
0.15
0.04
0.10
0.16
1.00
DebtN.Am
0
.37
0.50
0.51
0.52
0.21
0.25
0.20
0.21
0.18
0.06
0.04
0.02
0.14
0.44
1.00
DebtLatAm
0
.17
0.21
0.43
0.41
0.08
0.09
0.12
0.25
0.15
0.04
0.19
0.08
0.12
0.07
0.30
1.00
DebtCE.EU
0
.11
0.20
0.11
0.04
0.32
0.24
0.08
0.22
0.40
0.36
0.38
0.14
0.23
0.11
0.02
0.30
1.00
DebtW.EU
0
.46
0.56
0.61
0.56
0.02
0.23
0.14
0.35
0.01
0.25
0.29
0.05
0.20
0.28
0.59
0.37
0.25
1.00
DebtEm.As
0
.30
0.52
0.46
0.45
0.39
0.20
0.07
0.38
0.12
0.36
0.33
0.37
0.10
0.34
0.30
0.31
0.06
0.36
1.00
Debt
Asia
0
.25
0.27
0.20
0.19
0.06
0.20
0.02
0.35
0.12
0.14
0.23
0.38
0.13
0.22
0.20
0.01
0.03
0.27
0.10
1.00
DebtAfrica
0
.18
0.10
0.12
0.04
0.27
0.33
0.40
0.51
0.27
0.33
0.46
0.59
0.31
0.07
0.04
0.03
0.12
0.03
0.29
0.19
1.
CreditN.Am.
0
.25
0.15
0.27
0.32
0.24
0.14
0.17
0.14
0.05
0.10
0.20
0.03
0.18
0.18
0.35
0.02
0.12
0.40
0.07
0.14
0.
CreditLatAm
0
.17
0.25
0.09
0.20
0.09
0.27
0.05
0.42
0.30
0.22
0.35
0.51
0.49
0.05
0.08
0.14
0.00
0.19
0.04
0.21
0.
CreditCE.EU
0
.01
0.02
0.10
0.11
0.35
0.33
0.25
0.47
0.52
0.61
0.59
0.45
0.49
0.05
0.16
0.15
0.20
0.20
0.13
0.13
0.
CreditW.EU
0
.42
0.16
0.43
0.25
0.19
0.20
0.25
0.39
0.11
0.19
0.33
0.12
0.09
0.34
0.28
0.21
0.17
0.53
0.20
0.25
0.
CreditEm.As
0
.36
0.41
0.55
0.44
0.41
0.38
0.01
0.43
0.16
0.35
0.47
0.35
0.26
0.16
0.43
0.34
0.26
0.45
0.47
0.24
0.
CreditAsia
0
.32
0.07
0.22
0.03
0.07
0.18
0.16
0.24
0.17
0.16
0.18
0.28
0.05
0.25
0.17
0.10
0.19
0.17
0.28
0.08
0.
CreditAfrica
0
.22
0.06
0.21
0.28
0.22
0.16
0.16
0.07
0.10
0.17
0.18
0.14
0.13
0.07
0.18
0.29
0.14
0.12
0.15
0.12
0.
DDDDDDDCCCCCCC
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FDILatAm
0
.26
0.01
0.14
0.29
0.01
0.07
0.13
0.18
1.00
FDICE.EU
0
.26
0.03
0.35
0.12
0.13
0.37
0.10
0.11
0.37
1.00
FDI
W.EU
0
.05
0.21
0.17
0.19
0.19
0.28
0.03
0.09
0.30
0.40
1.00
FDIEm.As
0
.03
0.05
0.23
0.11
0.13
0.09
0.07
0.11
0.32
0.21
0.31
1.00
FDI
Asia
0
.23
0.27
0.08
0.24
0.22
0.08
0.27
0.08
0.36
0.23
0.16
0.03
1.00
FDI
Africa
0
.07
0.00
0.16
0.17
0.16
0.13
0.52
0.04
0.31
0.19
0.12
0.14
0.24
1.0
0
DebtN.Am
0
.04
0.04
0.14
0.11
0.18
0.02
0.02
0.16
0.40
0.53
0.33
0.31
0.35
0.0
81.00
DebtLatAm
0
.06
0.14
0.04
0.11
0.04
0.02
0.23
0.12
0.14
0.09
0.14
0.09
0.23
0.0
60.01
1.00
DebtCE.EU
0
.06
0.04
0.12
0.02
0.47
0.07
0.07
0.28
0.14
0.12
0.01
0.32
0.15
0.1
20.04
0.30
1.00
DebtW.EU
0
.11
0.03
0.04
0.05
0.55
0.13
0.08
0.02
0.04
0.16
0.44
0.05
0.17
0.0
30.00
0.04
0.28
1.00
DebtEm.As
0
.23
0.01
0.04
0.34
0.44
0.04
0.09
0.27
0.21
0.10
0.02
0.20
0.07
0.0
60.06
0.20
0.48
0.27
1.00
Debt
Asia
0
.15
0.33
0.14
0.16
0.01
0.02
0.15
0.03
0.01
0.21
0.06
0.20
0.04
0.0
50.13
0.10
0.07
0.00
0.02
1.00
DebtAfrica
0
.15
0.02
0.12
0.09
0.22
0.15
0.01
0.37
0.10
0.22
0.08
0.19
0.06
0.1
30.06
0.40
0.39
0.03
0.33
0.12
1.
CreditN.Am.0
.14
0.03
0.18
0.15
0.02
0.15
0.07
0.22
0.13
0.02
0.11
0.10
0.00
0.0
10.32
0.08
0.35
0.00
0.06
0.05
0.
CreditLatAm
0
.20
0.01
0.12
0.02
0.18
0.04
0.16
0.16
0.07
0.15
0.06
0.06
0.03
0.0
20.01
0.30
0.22
0.06
0.05
0.20
0.
CreditCE.EU
0
.11
0.16
0.09
0.15
0.03
0.15
0.40
0.06
0.06
0.22
0.28
0.13
0.04
0.0
60.29
0.06
0.19
0.24
0.01
0.50
0.
CreditW.EU
0
.01
0.10
0.09
0.25
0.05
0.19
0.08
0.21
0.11
0.02
0.15
0.07
0.07
0.1
40.04
0.03
0.01
0.51
0.08
0.18
0.
CreditEm.As
0
.02
0.28
0.22
0.18
0.14
0.03
0.17
0.11
0.20
0.17
0.25
0.23
0.00
0.0
90.11
0.25
0.13
0.01
0.06
0.04
0.
CreditAsia
0
.13
0.26
0.02
0.06
0.02
0.36
0.19
0.09
0.20
0.00
0.01
0.24
0.18
0.1
50.00
0.03
0.09
0.03
0.04
0.73
0.
CreditAfrica
0
.14
0.04
0.07
0.16
0.26
0.39
0.25
0.08
0.18
0.44
0.34
0.04
0.32
0.1
30.25
0.17
0.09
0.08
0.05
0.03
0.
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200
0Q10Q31Q11Q32Q12Q33Q13Q34Q14Q35Q15Q36Q16Q37Q17Q38Q18Q39Q19Q30Q10Q31Q11Q32Q12Q33Q13Q34Q14Q35Q15Q36Q16Q37Q17Q3
20
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
19
20
20
20
20
20
20
20
20
20
20
20
20
20
20
20
20
40
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