Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Do high-frequency measures of volatility improve forecasts of return distributions?

John M. Maheu and Thomas H. McCurdy

January 31, 2012

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Contents 1

Introduction

2

Data & RV estimation Effects of MSN on RV estimation

3

Return-RV models

4

Density Forecasts

5

Results

6

Conclusion John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Introduction

Predict distribution of returns rather than point estimates Option pricing Value-at-Risk Portfolio choice without quadratic utility or normality Can realized volatility (RV) estimates improve forecasts? Comparative study Joint return-RV models Longer forecast horizon

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Data

1 equity index (S&P500), 1 individual stock (IBM) 02/01/1996-29/08/2007, 04/01/1993-29/08/2007 5 minute prices Cont. compounded log returns Daily: rt , t = 1, ..., T Intraday: ri,t , i = 1, ..., I , t = 1, ..., T

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

RV estimation

Each day RV is estimated: P 2 Na¨ıve estimator: RVt,u = Ii=1 rt,i Et−1 (RVt ) = Vart−1 (rt ) = σt2 Adjust for Microstructure P Noise (MSN) RVt,ACq = ω0 γˆ0 + 2 qj=1 ωj γˆj P −j γˆj = Ii=1 rt,i rt,i+j Bartlett weights: ωj = 1 −

j q+1

Consider q = 1, 2, 3

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Bai, Russel & Tiao (2004)

Exchange rate data 87-96 15-minute returns Dollar/Deutsche Mark, Dollar/Yen, Dollar/French Franc Mondays excluded Mean zero, left-skewed Adjusted for time-of-day effects

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Sample Autocorrelation function (a) Dollar / Deutschmark 0.1 0.0 -0.1 -0.2 1

12

24

48

Autocorrelation

(b) Dollar / French Franc 0.1 0.0 -0.1 -0.2 1

12

24

48

(c) Dollar / Japanese Yen 0.1 0.0 -0.1 -0.2 1

12

John M. Maheu and Thomas H. McCurdy

24

48

DoLag high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

(a) Dollar / Deutchmark 0.3 0.2 0.1 0.0 1

12

24

48

Autocorrelation

(b) Dollar / French Franc 0.3 0.2 0.1 0.0 1

12

24

48

(c) Dollar / Japanese Yen 0.3 0.2 0.1 0.0 1

12

24

48

Lag Figure 4: Sample ACF of Squared MA(1) innovations

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Findings Evidence of MA(1) structure Residual ACF suggests clustering They find: Higher frequency leads to worse estimates True price process pt not observed Due to Market Microstructure Noise Bid-Ask spread Rounding Noisy quotes Lagged reporting Trades on different markets Human error Information effects John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

The Problem

Suppose we observe Xt = pt + Ut , Ut ∼ (0, σu2 ), Ut iid for now) ∗ +U −U rt,i = rt,i t,i t,i−1

`

pt (&

Bias in RV h i Pnt 2 |r ∗ = E [RVt,u |r ∗ ] = i=1 E rt,i   Pnt Pnt 2 = RV ∗ + 2I σ 2 ∗ 2 t,u u i=1 E (Ut,i + Ut,i−1t ) i=1 (rt,i ) + Increasing in sampling frequency RVt,u → ∞ as I → ∞

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Sparse Sampling Andersen, Bollerslev, Diebold & Labys (1999) propose Volatility Signature Plots Efficient Sampling Tradeoff: observations vs. bias Volatility signature plots Figure 6 Representative Volatility Signature Plots Observations ”thrown away” Liquid and Illiquid Assets Average Realized Volatility

0.0008

Liquid

0.0007 0.0006 0.0005 0.0004 0.0003 0

100

200

300

400

500

k

John M. Maheu and Thomas H. McCurdy 1.3

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Multiple Scales Zhang, Mykland & A¨ıt-Sahalia (2005) Optimal sample size Sub-grids and averaging 2 Determined by IQ and σu2 Two Scale bias correction (TSRV): Highest frequency to estimate 2σu2 (I −1 RVt,u ) Low frequency ¯I to estimate σt2 + 2¯I σu2 (RVt,sparse ) ¯ TSRVt = RVt,sparse − II RVt,u

Converges to σt2 at rate I 1/6

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Extensions Bandi & Russel (2005) Pre-filtering Optimal sampling with dependent noise Using RVt,sparse Zhang (2006): More than two scales (MSRV) Fastest possible rate I 1/4 when all possible scales used Optimal choice of weights

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Dependent Noise Autocorrelogram from AIG Transactions

Autocorrelogram from MMM Transactions

1

1

0.75

0.75

0.5

0.5

0.25

0.25

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

- 0.25

- 0.25

- 0.5

- 0.5

Autocorrelogram from INTC Transactions

Autocorrelogram from MSFT Transactions

1

1

0.75

0.75

0.5

0.5

0.25

0.25

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

- 0.25

- 0.25

- 0.5

- 0.5

1.0

1.0

0.5

0.5

0.0

0.0

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20

- 0.5

- 0.5

Fig. 4. Top and middle panels: Log-return autocorrelograms from transactions for American International Group, Inc. (AIG), 3M Co. (MMM), Intel (INTC) and Microsoft (MSFT), last ten trading days in April 2004. Bottom panel: log-return autocorrelogram from the same transactions for Intel and Microsoft, superimposed M. Maheu and McCurdy Do high-frequency measures of volatility improve forecasts of retu with theJohn autocorrelogram fittedThomas from theH.basic i.i.d. plus AR(1) model for the noise.

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Extensions II

A¨ıt-Sahalia, Mykland & Zhang (2010) Evidence for dependence in Ut in NYSE & NASDAQ stocks More likely in liquid stocks TSRV and MSRV robust Empirical findings: Largely unaffected by choice of I and ¯I MSRV very close to TSRV Both improvement over RV

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Realized Kernels

Barndorff-Nielsen, Hansen, Lunde & Shepherd (2006) Kernel estimation Define: Realized autocorrelation: P t γh (Xδ ) = nj=1 (Xjδ − X(j−1)δ )(X(j−h)δ − X(j−h−1)δ ) γ˜h (Xδ ) = γh (Xδ ) + γ−h (Xδ )  P ˜ (Xδ ) = γ0 (Xδ ) + H k h−1 γ˜ (Xδ ) Realized Kernel: K h=1 H

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Effects of MSN on RV estimation

Results ˜ (Xδ ) consistent estimator of K H, I → ∞

R1 0

σ(t − 1 + τ )2 dτ for

Mixed normal, complicated variance Rate of convergence depends on H(I ) I 1/6 if H = cI 2/3 I 1/4 if H = cI 1/2 (if k 0 (0) = k 0 (1) = 0) c may be chosen to minimize the variance

Flat top kernels robust to dependent, endogenous noise or endogenous timing Estimation more accurate than RVt,sparse

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

6.377 6.362

82.091 Introduction Data & RV estimation 81.024 Return-RV models Density Forecasts

0.114 0.010

Effects of MSN on RV estimation

66.594 65.235

adjustment, and RVACq , q = 1, 2, 3, are constructed Results as in Eq. (2.2). Conclusion

ation , we their

ights ch, a

(2.2) j , q +1

et al. ype. , are d the plays mates ance

Fig. 1. ACF of 5-minute return data.

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

ARTICLE

Effects of MSN on RV estimation

J.M. Maheu, T.H. McCurdy / J

Table 1 Summary statistics: daily returns and realized volatility. Mean SPY rt RVu RVAC 1 RVAC 2 RVAC 3 IBM rt RVu RVAC 1 RVAC 2 RVAC 3

Variance

S

0.018 1.210 1.079 1.013 0.978

0.967 2.640 2.373 2.115 2.054

0 6 7 7 8

0.037 2.825 2.623 2.558 2.531

2.602 9.161 9.433 9.875 10.095

0 5 6 6 6

rt are daily returns, RVu are constructed from raw 5-minute returns with no adju John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Benchmark model

EGARCH: rt 2 log (σt )

= µ + εt , εt = σt ut ut ∼ NID(0, 1) 2 = ω + βlog (σt−1 ) + γut−1 + α|ut−1 |

Allows for leverage effect Estimated from daily returns

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

RV-based models

Joint modeling of returns and RV allows multi horizon forecasts Component-RV (2Comp) Heterogeneous Autoregressive-RV (HAR) Extensions: t-distributed noise in rt Mixed normal noise in log (RVt ) GARCH dynamics in log (RVt ) Observed stochastic volatility (OSV)

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

2Comp-RV

2 component model with different decay rates: = µ + εt , εt = σt ut ut ∼ NID(0, 1) 2 X log (RVt ) = ω + φi si,t + γut−1 + ηvt , vt ∼ NID(0, 1) rt

i=1

si,t

= (1 − αi )log (RVt−1 ) + αi si,t−1 , 0 < αi < 1, i = 1, 2

σt2 = Et−1 (RVt ) = exp (Et−1 log (RVt ) + .5Vart−1 (log (RVt )))

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

2Comp-RV Due to Maheu & McCurdy (2007) Estimated by max likelihood RVt estimated from intra day data No infinite exponential smoothing No mean reversion in volatility Degenerate in asymptotic limits Weighting parameters φi ∈ (0, 1) and mean ω

Variance targeting sets ω = mean(log (RV ))(1 − φ1 − φ2 ) No leverage term

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

HAR-RV

Define RVt−h,h = rt

1 h

Ph−1 j=0

log (RVt−h+j ).

= µ + εt , εt = σt ut ut ∼ NID(0, 1)

log (RVt ) = ω + φ1 log (RVt−1 ) + φ2 log (RVt−5,5 ) +φ3 log (RVt−22,22 ) + γut−1 + ηvt , vt ∼ NID(0, 1) σt2

= Et−1 (RVt ) = exp (Et−1 log (RVt ) + .5Vart−1 (log (RVt )))

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

HAR-RV

Due to Corsi (2009), Andersen et al. (2007) Captures long memory dependence No leverage term

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Extensions

Robustness is tested w.r.t. certain alternatives: t-distributed noise (ut ∼ tυ (0, 1)) Mixed normality: η = 1 vt ∼ (0, σv2,1 ) w/ prob π; vt ∼ (0, σv2,2 ) w/ prob 1 − π η follows GARCH(1,1) 2 ηt2 = κ0 + κ1 [log (RVt−1 ) − Et−2 log (RVt−1 )]2 + κ2 ηt−1 Set σt2 = RVt (OSV model)

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

How to evaluate density forecasts? Predictive Likelihood Evaluate density forecast at realized return Usually 1-step ahead Φt is the information set at time t, θ a set of parameters Consider out of sample observations t = τ + kmax , ..., T − k. fM,k (x|Φt , θ) denotes k-step ahead forecasted likelihood of model M For S&P, T = 2936, τ = 1200 kmax = 60

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Average predictive likelihood: DM,k

1 = T − τ − kmax + 1

T −k X

log (fM,k (rt+k |Φt , θ))

t=τ +kmax −k

Compare models A and B with test stat due to Diebold & Mariano (1995) and Amisano & Giacomini (2007): √ (DA,k − DB,k ) T − τ − kmax + 1 k tA,B = σ ˆAB,k Asymptotically N(0, 1).

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Computation

If k > 1, fM,k (rt+k |Φt , θ) is unknown. Can be estimated by monte carlo (MC), i = 1, .., N = 10000 Distribution know conditional on variance Rao-Blackwellization Reduces variance of MC estimates

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Computation Consider the EGARCH: Z 2 2 2 fM,k (rt+k |Φt , θ) = f (rt+k |µ, σt+k )p(σt+k |Φt )dσt+k ≈

N 1 X 2(i) f (rt+k |µ, σt+k ), N

2(i)

2 σt+k ∼ p(σt+k |Φt )

i=1

Other models require simulation of RV N times 2(i)

2(i)

σt+k = Et+k−1 RVt+k

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

General Results

Unrestricted models > variance targeting When σt2 = Et−1 RVt , t-innovations > N 2 components > 1 Intraday info, timing and non-normality are important Focus on best models

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

ARTICLE IN PRESS

S&P 6

J.M. Maheu, T.H. McCurdy / Journal of Econometrics (

)



Fig. 4. IBM, robustne Fig. 2.H.S&P 500, joint models EGARCH. measures of volatility improve John M. Maheu and Thomas McCurdy Doversus high-frequency forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

IBM

Fig. 2. S&P 500, joint models versus EGARCH.

Fig. 4. IBM, robustnes

functional forms (either 2out we forecast. The three best bivaria 2Comp and HAR. For the S for IBM forecasts the 2Co The additional informatio volatility (OSV) assumptio to in-sample fit as shown b density forecasts for long 500. The OSV assumption the IBM case, as shown b Fig. 3 for ‘2Comp-OSV vs 2 Fig. 4 evaluates the robu for IBM to a generalizatio log(RV). In particular, as Eq. (3.10) to allow eithe parameterization of the co neither of these generaliz sample density forecasts that a mixture-of-Norma log(RV) improves densit distributed alternative for Table 2 provides full-s bestimprove bivariate specificatio Fig.H. 3. McCurdy IBM, joint modelsDo versus EGARCH. John M. Maheu and Thomas high-frequency measures of volatility forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Results

Forecast performance deteriorates as k increases 2COMP, 2COMP-OSV and HAR perform best Intraday data improves forecasts significantly Advantage of flexible models increase in k

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Robustness ARTICLE IN PRESS

.M. Maheu, T.H. McCurdy / Journal of Econometrics (

s EGARCH.

)



John M. Maheu and Thomas H. McCurdy Do high-frequency measures of volatility improve forecasts of retu Fig. 4. IBM, robustness to non-normal innovations to log (RV).

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

S&P Estimation Results

ARTICLE IN PRES J.M. Maheu, T.H. McCurdy / Journal of Econometrics (

Table 2 S&P 500 model estimates. 2Comp-OSV model

p

rt = µ + ✏t , ✏t = RVt ut , ut ⇠ D(0, 1) P2 log(RVt ) = ! + i=1 i si,t + ut 1 + ⌘vt , vt ⇠ NID(0, 1), si,t = (1 ↵i ) log(RVt 1 ) + ↵i si,t 1 , i = 1, 2. 2Comp model

rt = µ + ✏t , ✏t = t ut , ut ⇠ tv (0, 1) 1 2 t = exp Et 1 log(RVt ) + 2 Vart 1 (log(RVt ))

P2

log(RVt ) = ! + i=1 si,t = (1 ↵i ) log(RVt Parameter

µ ! 1 2

↵1 ↵2 ⌘ 1/⌫ lgl

i si,t

1

+ ut 1 + ⌘vt , vt ⇠ NID(0, 1), ) + ↵i si,t 1 , i = 1, 2.

2Comp-OSV: ut ⇠ N (0, 1) 0.038 (0.011) 0.026 (0.012) 0.476 (0.007) 0.476 0.888 (0.017) 0.435 (0.037) 0.129 (0.010) 0.531 (0.009)

5646.725

2Comp: ut ⇠ t⌫ (0, 1) 0.018 (0.014) 0.025 (0.013) 0.402 (0.147) 0.543 (0.154) 0.911 (0.045) 0.508 (0.105) 0.141 (0.011) 0.528 (0.009) 0.089 (0.016) 5916.342

)



Using the predict intraday data is imp daily data as in our a flexible function fo important for the d marginally improves 500 but is essentially of returns with Nor volatility directed b function of log(RV) p of out-of-sample hor

Acknowledgements

We thank the edi Zhongfang He, Lars S conference on Realiz ment Conference, th and Risk Manageme the Federal Reserve B Guangyu Fu and Xia tance. We are also gr

John M. Maheu and Thomas H. McCurdy Do high-frequency measures of volatility References improve forecasts of retu The main features of our results are as follows. Bivariate

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Robustness/S&P Estimation

Mixed-Normal log (RV ) dynamics: improvement GARCH dynamics (not shown): no improvement In sample: OSV preferred Out of sample: no difference Parameter estimates very similar

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Conclusion

Joint models of return and RV Comparison by predictive likelihood Intraday info can be exploited RV improves forecasts

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Introduction Data & RV estimation Return-RV models Density Forecasts Results Conclusion

Critique

Why 5 minutes? Could give more info on MSN; different solutions Jumps Many models, few reported Leverage not included in return-RV models More than 2 components? How is HAR specification chosen? Discussion of leverage not adjusted...

John M. Maheu and Thomas H. McCurdy

Do high-frequency measures of volatility improve forecasts of retu

Do high-frequency measures of volatility improve forecasts of return ...

Jan 31, 2012 - Can realized volatility (RV) estimates improve forecasts? Comparative study. Joint return-RV models ..... Average predictive likelihood: DM,k = 1.

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