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Exact Distribution of the Mean Reversion Estimator in the Ornstein-Uhlenbeck Process * Yong Bao Department of Economics Purdue University Aman Ullah Department of Economics University of California, Riverside Yun Wang § School of International Trade and Economics University of International Business and Economics August 31, 2014 Abstract: Econometricians have recently been interested in estimating and testing the mean reversion param- eter (κ) in linear diffusion models. It has been documented that the maximum likelihood estimator (MLE) of κ tends to over estimate the true value. Its asymptotic distribution, on the other hand, depends on how the data are sampled (under expanding, infill, or mixed domain) as well as how we spell out the initial condition. This poses a tremendous challenge to practitioners in terms of estimation and inference. In this paper, we provide new and significant results regarding the exact distribution of the MLE of κ in the Ornstein-Uhlenbeck process under different scenarios: known or unknown drift term, fixed or random start-up value, and zero or positive κ. In particular, we employ numerical integration via analytical evaluation of a joint characteristic function. Our numerical calculations demonstrate the remarkably reliable performance of our exact approach. It is found that the true distribution of the MLE can be severely skewed in finite samples and that the asymptotic distributions in general may provide misleading results. Our exact approach indicates clearly the non-mean-reverting behav- ior of the real federal fund rate. JEL Classification: C22, C46, C58 Key Words: Distribution, Mean Reversion Estimator, Ornstein-Uhlenbeck Process * We are thankful to Yacine A¨ ıt-Sahalia, Peter Phillips, and Jun Yu, for helpful comments. We also benefited from discussions with Victoria Zinde-Walsh on the subject matter. Corresponding Author: Department of Economics, Purdue University, 403 W. State Street, West Lafayette, IN 47907, USA. E-mail: [email protected]. Department of Economics, University of California, Riverside, CA 92521, USA. E-mail: [email protected]. § School of International Trade and Economics, University of International Business and Economics, Beijing, China. E-mail: [email protected].

Exact Distribution of the Mean Reversion Estimator in the ...Exact Distribution of the Mean Reversion Estimator in the Ornstein-Uhlenbeck Process Yong Baoy Department of Economics

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Exact Distribution of the Mean Reversion Estimator in

the Ornstein-Uhlenbeck Process∗

Yong Bao†

Department of Economics

Purdue University

Aman Ullah‡

Department of Economics

University of California, Riverside

Yun Wang§

School of International Trade and Economics

University of International Business and Economics

August 31, 2014

Abstract: Econometricians have recently been interested in estimating and testing the mean reversion param-eter (κ) in linear diffusion models. It has been documented that the maximum likelihood estimator (MLE) of κtends to over estimate the true value. Its asymptotic distribution, on the other hand, depends on how the dataare sampled (under expanding, infill, or mixed domain) as well as how we spell out the initial condition. Thisposes a tremendous challenge to practitioners in terms of estimation and inference. In this paper, we providenew and significant results regarding the exact distribution of the MLE of κ in the Ornstein-Uhlenbeck processunder different scenarios: known or unknown drift term, fixed or random start-up value, and zero or positive κ.In particular, we employ numerical integration via analytical evaluation of a joint characteristic function. Ournumerical calculations demonstrate the remarkably reliable performance of our exact approach. It is found thatthe true distribution of the MLE can be severely skewed in finite samples and that the asymptotic distributionsin general may provide misleading results. Our exact approach indicates clearly the non-mean-reverting behav-ior of the real federal fund rate.

JEL Classification: C22, C46, C58

Key Words: Distribution, Mean Reversion Estimator, Ornstein-Uhlenbeck Process

∗We are thankful to Yacine Aıt-Sahalia, Peter Phillips, and Jun Yu, for helpful comments. We also benefited from discussionswith Victoria Zinde-Walsh on the subject matter.†Corresponding Author: Department of Economics, Purdue University, 403 W. State Street, West Lafayette, IN 47907, USA.

E-mail: [email protected].‡Department of Economics, University of California, Riverside, CA 92521, USA. E-mail: [email protected].§School of International Trade and Economics, University of International Business and Economics, Beijing, China. E-mail:

[email protected].

1 Introduction

Since the seminal works of Merton (1971) and Black and Scholes (1973), continuous-time models have been used

extensively in financial economics, see the excellent survey by Sundaresan (2000). Econometricians have also

paid close attention to this line of literature. Maximum likelihood, generalized method of moments, simulated

method of moments, and nonparametric approaches have been developed for model estimation, see, for instance,

Singleton (2001), Bandi and Phillips (2003), Hong and Li (2005), and Phillips and Yu (2009a).

As shown in the literature, there exists serious bias in estimating the mean reversion parameter (κ) by

almost all the methods, especially when the diffusion process has a linear drift function and the speed of mean

reversion is slow (i.e., small values of κ). For example, Phillips and Yu (2005) found that the bias of the maximum

likelihood estimator (MLE) for κ in the CIR model (Cox, Ingersoll, and Ross, 1985) can be substantial for data

sets with very long time spans, regardless of data frequency. Recently, Tang and Chen (2009) showed that the

bias of κ is up to O(T−1) in the stationary Vasicek model (Vasicek, 1977), where T is the time span. They also

derived the approximate biases of the diffusion and drift estimators, and their simulations demonstrated that

the estimation biases of diffusion and drift parameters are virtually zero, but κ could be severely biased. Since

the mean reversion parameter κ is of most importance for asset pricing, risk management, and forecasting,

considerable attention in the literature has arisen to improve its estimation accuracy. Recent contributions

include indirect inference (Phillips and Yu, 2009b), bootstrapping (Tang and Chen, 2009), and analytical bias

approximation (Yu, 2012).

In addition to the classical asymptotic analysis under expanding domain (T →∞), asymptotic results under

infill (n → ∞, where n is the number of sample observations within a data span T ) and mixed (n → ∞

and T → ∞) domains are also analyzed in the literature. In the context of Vasicek and CIR processes with

unknown drift, Tang and Chen (2009) showed that asymptotic distributions of the MLE are quite different under

expanding and mixed domains. Aıt-Sahalia (2002) derived the asymptotic distribution of his approximate MLE

under the expanding domain in diffusions models. A striking observation from his simulations is that under the

stationary case, the asymptotic distribution of the estimated mean reversion parameter deviates more seriously

from its corresponding finite-sample distribution as the true parameter value deceases from 10 to 1, i.e., as the

process is getting closer to a unit root process, even with a very large sample size (n = 1000). Under the mixed

domain, Brown and Hewitt (1975) obtained the limit normal distribution for the MLE of κ in the Vasicek model

with a known drift term, see also Bandi and Phillips (2003, 2007), and Phillips and Yu (2009c) for asymptotic

analysis under mixed domain. In a recent paper, Zhou and Yu (2010) derived the asymptotic distributions of the

least squares (LS) estimator of κ in a general class of diffusion models under the three different domains. They

2

provided Monte Carlo evidence that the infill asymptotic distribution is much more accurate in approximating

the true finite-sample distribution than the asymptotic distributions under the other two domains.

The problems of estimation bias and inaccurate and different distribution approximations floating in the

literature are largely due to the absence of exact analytical distribution results. Moreover, in reality, given the

discretized data (with a given finite data span T and finite sample size n ), we do not really know under which

asymptotic domain our inference about κ shall be, but the asymptotic distribution results can behave quite

differently under expanding, infill, and mixed domains. To address these problems, in this paper we investigate

the exact distribution of the estimated mean reversion parameter in the Ornstein-Uhlenbeck process. To the

best of our knowledge, our paper is the first to examine the exact finite-sample distribution of the estimated κ in

continuous-time models. Since the MLE of κ is a simple transformation of the LS estimator of the autoregressive

coefficient φ in a first-order autoregressive (AR(1)) model with discrete data, our study is intrinsically related

to the vast literature studying the finite-sample distribution of the AR(1) coefficient estimator φ. The Imhof

(1961) technique, in conjunction with Davies (1973, 1980), was typically used to develop the exact distribution

of φ, see Ullah (2004) for a comprehensive review. Nevertheless, the Imhof (1961) technique is applicable only

when the process is strictly stationary with an initial random observation included in formulating φ, or when the

first observation is discarded. Computational burden of the Imhof (1961) technique also increases tremendously

as the sample size of the AR process increases, since it involves computation of eigenvalues of a matrix whose

dimension is the same as the sample size. In this paper, we take a different approach by first analytically

evaluating the joint characteristic function of the random numerator and denominator in defining φ, and then

inverting it via Gurland (1948) and Gil-Pelaez (1951) to calculate the exact finite-sample distribution. This

approach is in line with Tsui and Ali (1992, 1994) and Ali (2002). However, note that in Tsui and Ali (1992,

1994) and Ali (2002), no intercept term was included in the AR(1) model. This is equivalent to a known

drift term in the linear diffusion process. In this paper, we consider explicitly the case when the drift term is

unknown. Moreover, Tsui and Ali (1992, 1994) did not include the initial observation in formulating the LS

estimator φ, whereas Ali (2002) focused on the approximate distribution with the initial observation included.

The initial observation does matter in studying the exact distributions in finite samples; in fact, it also matters

even for the asymptotic distributions under several scenarios.

The remainder of our paper is as follows. In Section 2, we derive the exact distribution of the MLE of the

mean reversion parameter κ. We also presents simulation results and compare our exact distribution results

with the asymptotic results under the three different domains. In Section 3 we construct the exact confidence

intervals for the mean reversion parameter κ when the linear diffusion model is used to study the real federal

3

fund rate, and we find strong evidence of the non-mean-reverting behavior. Section 4 concludes. Technical

details are collected in the appendix.

2 Exact Distribution

We consider the Ornstein-Uhlenbeck (OU) process with the initial value x(0),

dx(t) = κ(µ− x(t))dt+ σdB(t), (2.1)

where κ ∈ R, µ ∈ R, σ > 0, and B(t) is a standard Brownian motion. We are interested in estimating the

parameter κ. When κ 6= 0, the solution to the above process is

x(t) = µ+ (x(0)− µ) exp (−κt) + σ

∫ t

0

exp (κ(s− t)) dB(s), t ≥ 0. (2.2)

Usually κ > 0 is assumed, and then as t→∞, the deterministic part of x tends to the mean level µ, so we have

a mean-reverting process. When κ = 0, the process is no longer mean reverting:

x(t) = x(0) + σB(t), (2.3)

where the parameter µ vanishes.

In practice, the observed data are discretely recorded at (0, h, 2h, · · · , nh) in the time interval [0, T ], where

h is the sampling interval and T is the data span. The exact discrete model corresponding to (2.1) is an AR(1)

model:

xih = α+ φx(i−1)h + εih, i = 0, 1, · · · , n, (2.4)

where φ = exp(−κh), α = µ[1−exp(−κh)], and εih ∼ i.i.d.N(0, σ2ε). The definition of the error term εih depends

on whether κ is positive or zero: εih = σεi√

(1− exp(−2κh))/(2κ) when κ > 0, εih = σ√hεi when κ = 0, where

εi ∼ i.i.d.N(0, 1). Correspondingly, σ2ε = σ2(1 − exp(−2κh))/(2κ) when κ > 0 and σ2

ε = σ2h when κ = 0.

Note that the autoregressive coefficient φ is always positive by definition. When κ = 0, φ = 1, α = 0, so (2.4)

becomes a random walk (with no drift). In the sequel, we suppress h in xih and εih for notational convenience.

It is well known that the LS/ML estimator of κ based on the discrete data is

κ = − ln(φ)

h, (2.5)

4

where φ is the LS estimator of φ in (2.4). When µ is known (without loss of generality, µ = 0), φ =∑ni=1 xi−1xi/

∑ni=1 x

2i−1; for the case of unknown µ, φ =

∑ni=1(xi−1 − x)xi/

∑ni=1(xi−1 − x)2, where x =

n−1∑ni=1 xi−1.

1

We are interested in studying the properties of κ estimated from the discrete sample via φ. As can be

expected, the exact properties of κ depend on how we spell out the initial observation x(0) = x0. It can be fixed

(at zero or a non-zero constant) or random. In this paper, when x0 is random, we assume that the time series

(x0, x1, · · · , xn) is stationary.

Note that (2.5) is defined only if φ > 0. However, φ can be negative with a non-zero probability. Thus, we

define exact distribution of κ− κ as Pr(κ− κ ≤ w) ≡ Pr(κ− κ ≤ w|φ > 0). With this definition, we can show

that

Pr (κ− κ ≤ w) =1− Fφ(φ exp (−hw)− φ)

1− Fφ(−φ), (2.6)

where Fφ(·) denotes the cumulative distribution function (CDF) of φ− φ.2

As can be seen, with a given sampling frequency h, the distribution of κ−κ follows from the distribution of

φ−φ. When κ > 0 and x0 is random, we can write φ−φ as a ratio of quadratic forms in the normal random vector

(x0, x1, · · · , xn)′, and the technique of Imhof (1961) can be used to evaluate Fφ, and thus Fκ. For a fixed x0, it is

not obvious how to directly apply Imhof (1961).3 More fundamentally, Imhof’s procedure requires computation

of eigenvalues of an (n + 1) × (n + 1) matrix, which becomes very cumbersome as the sampling interval h

decreases. Therefore, we proceed to derive the distribution function Fφ by using the results from Gurland

(1948) and Gil-Pelaez (1951) on a ratio of two random variables: Let Y1 and Y2 have the joint characteristic

function (CF) ϕ (u, v) = E(exp (iuY1 + ivY2)). If Pr (Y2 ≤ 0) = 0, then the distribution of φ − φ = Y1/Y2 is

given by

Fφ(y) = Pr(φ− φ ≤ y) =1

2− 1

π

∫ ∞0

Im

(ϕ(u,−uy)

u

)du. (2.7)

Given the CDF (2.6), one might be tempted to evaluate the probability distribution function (PDF) of

κ − κ (again conditional on φ > 0), fκ(w) = hφ exp (−hw) fφ(φ exp (−hw) − φ)/[1 − Fφ(−φ)], where fφ(·)

denotes the PDF of φ− φ and can be calculated from F ′φ

(y) = π−1∫∞0

Im (∂ϕ(u, v)/∂v|v=−uy) du. As pointed

out by Hillier (2001), the density function of a ratio of normal quadratic forms (for instance, in the case when

κ > 0 and x0 is random), can be nonanayltic at some points. Thus in this paper we focus on the CDF only.

1Since we are interested in studying the finite sample properties of κ, the initial condition x0 matters and we include it in theestimation procedure. This stands in contrast to the convention of Hurwicz (1950). For the case of known µ, if µ 6= 0, one cansimply define yi = xi − µ and work with yi.

2Note that (2.6) holds regardless of the distribution assumption.3If we discard x0 in formulating φ, then the Imhof (1961) technique is still applicable, as we can define φ in terms of quadratic

forms in the random vector (x1, x2, · · · , xn)′.

5

2.1 Joint Characteristic Function

For us to be able to use (2.7) to derive (2.6) for κ − κ, an essential task is to evaluate the joint characteristic

function of the numerator and denominator in defining φ − φ. To facilitate presentation, we first introduce

some notation. Let 0n be an n × 1 vector of zeros, In be the identity matrix of size n, ιn be an n × 1 vector

of ones, Mn = In − n−1ιnι′n, ei,n be a unit/elementary vector in the n-dimensional Euclidean space with its

i-th element being 1. Given an (n− 1)× (n− 1) matrix Cn−1, we define ACn as an n× n matrix with its lower

left block being Cn−1 and all other elements being zero, and BCn as an n× n matrix with its upper left block

being Cn−1 and all other elements being zero. When Cn−1 = In−1, we simply put An = AIn and Bn = BI

n.

For an n× n matrix Cn, we use cn,ij to denote its ij-th element, and c(ij)n to denote the ij-th element of C−1n ,

whenever it exists. Throughout, V n is an n× n matrix with its ij-th element φ|i−j|.

When κ > 0, define zi = (xi−µ)/σε, i = 0, · · · , n, and z = n−1∑ni=1 zi−1.Obviously, φ =

∑ni=1 zi−1zi/

∑ni=1 z

2i−1

for the case of known µ, and φ =∑ni=1(zi−1 − z)zi/

∑ni=1(zi−1 − z)2 for the case of unknown µ.

In the case of κ = 0, the parameter µ vanishes, and we define zi = xi/σε and ¯z = n−1∑ni=1 zi−1. In practice,

we may still proceed to estimate φ from the discrete AR(1) model without or with an intercept even when the

parameter µ is not defined. Correspondingly, φ =∑ni=1 zi−1zi/

∑ni=1 z

2i−1 or φ =

∑ni=1(zi−1− ¯z)zi/

∑ni=1(zi−1−

¯z)2.

Denote zn = (z1, · · · , zn)′ and ζn+1 = (z0, zn)′. Note that (z2, · · · , zn)′ = (0n−1, In−1) zn, (z1, · · · , zn−1)′ =

(In−1,0n−1) zn, and (z0 − z, · · · , zn−1 − z)′ = MnAnzn+z0Mne1,n. (Results pertaining to z can be obviously

defined.) Thus we can express the following sums in matrix notation:∑ni=1 zi−1zi = z0z

′ne1,n + z′nAnzn = ζ′n+1An+1ζn+1,∑n

i=1 z2i−1 = z20 + z′nBnzn = ζ′n+1Bn+1ζn+1,∑n

i=1(zi−1 − z)zi = z′nMnAnzn + z0z′nMne1,n = ζ′n+1A

Mn+1ζn+1,∑n

i=1(zi−1 − z)2 = z′nA′nMnAnzn + z20e

′1,nMne1,n + 2z0z

′nA′nMne1,n = ζ′n+1B

Mn+1ζn+1.

Consequently, when κ > 0, we can write the numerator and denominator (Y1 and Y2) in formulating

φ − φ in terms of quadratic forms in either zn (when x0 is fixed) or ζn+1 (when x0 is random). Define

the following matrices/vectors (note that these matrices and vectors depend on u, v, and model parameters; we

have suppressed their arguments):

Rn = In +(φ2 + 2iuφ− 2iv

)Bn − (φ+ iu) (An +A′n),

δn = iu(In − 2φA′n)Mne1,n + 2ivA′nMne1,n + φe1,n,

Sn = In + φ2Bn − φ(An +A′n)− iu(MnAn +A′nMn) + 2i(uφ− v)A′nMnAn,

T n+1 = (1− φ2)V −1n+1 − iu(AMn+1 +AM ′

n+1) + 2i(uφ− v)BMn+1.

6

Then we can present the characteristic function ϕ(u, v) under the different scenarios as follows (see the appendix

for detailed derivation; when κ = 0, Rn, δn, and Sn are defined with φ = 1 in their expressions).

Characteristic Function of φ− φ

κ µ (intercept in AR(1) or not) x0 ϕ (u, v)

> 0 Known (no intercept) Fixed exp[z202

(1− |Rn+1|

|Rn|

)]|Rn|−1/2

Random√

1− φ2(|Rn+1| − φ2 |Rn|

)−1/2Unknown (with intercept) Fixed exp

[−φ

2z202 − i(uφ− v)z20

(1− 1

n

)+ 1

2z20δ′nS−1n δn

]|Sn|−1/2

Random√

1− φ2 |T n+1|−1/2

= 0 No intercept Fixed exp[z202

(1− |Rn+1|

|Rn|

)]|Rn|−1/2

With intercept exp[−φ

2z202 − i(u− v)z20

(1− 1

n

)+ 1

2 z20δ′nS−1n δn

]|Sn|−1/2

With ϕ (u, v) in hand, we can directly use (2.7) to derive the distribution function of φ, which in turn

can be plugged into (2.6) to obtain the distribution function of κ. Clearly, in this procedure we need to find

determinants (|Rn| , |Rn+1| , |Sn| , and |T n+1|) and inverses (S−1n and T−1n+1). When n is small, this can be

done easily numerically. But for a moderately large n, for example, T = 10, h = 1/252, n = 2520 (daily data

over 10 years), this can be quite time consuming. Instead of numerically evaluating these determinants and

inverses, we proceed to derive direct analytical expressions, presented in Appendix B, by utilizing the special

structures of these matrices.

The essential merit of our approach is computational efficiency based on analytical, instead of numerical,

determinants and inverses. We make no attempt to control computational accuracy when applying numerical

integration in (2.7); instead we rely on Matlab’s adaptive Gauss-Kronrod quadrature integral procedure quadgk

by setting numerical absolute error tolerance (1e− 12). The eigenvalue-based approach via Imhof (1961), when

applicable, might be able to manually control the integration error and truncation error, see Davies (1973, 1980),

Ansley et al. (1992), and Lu and King (2002). Our numerical exercise in the next subsection demonstrates that

our numeral integration approach in fact produces very accurate results. Also, as emphasized before, the Imhof

(1961) approach is not always applicable.

7

2.2 Numerical Results

In this section, we conduct Monte Carlo simulations to illustrate the finite sample performance of our exact

distribution in comparison with the “true” distribution and the asymptotic distribution. The data generating

process follows the OU model in (2.4), and the error term is generated from a normal distribution. The

asymptotic distribution results are available from Zhou and Yu (2010).4 Note that under the infill asymptotics,

the results are conditional on the initial x0.

We set T = 1, 2, 5, 10, h = 1/12, 1/52, 1/252, κ = 0.01, 0.1, 1, µ = 0, 0.1, σ = 0.1, x0 = µ or x0 ∼

N(µ, σ2/(2κ)). Compared with Zhou and Yu (2010), we have a more comprehensive experiment design, so as

to have a better understanding of the finite-sample distributions. For the fixed start-up case (x0 = 0), we also

consider κ = 0. As pointed out in Zhou and Yu (2010), the values of 0.01 and 0.1 for κ are empirically realistic

for interest rate data while the value of 1 is empirically realistic for volatility.

Tables 1–4 report the cumulative distributions of T (κ− κ), where the “true” distribution results come from

1,000,000 replications, and we make comparison of the exact (p), true (pedf ), and asymptotic results under the

three asymptotics (pexp, pmix, pinf ).5 In calculating the exact distribution with the analytical characteristic

function, we still need to implement numerical integration in (2.7). Appendix C discusses how to overcome

the problem of discontinuity of the square root function in the complex domain. The complete experiment

results are available from the corresponding author upon request. To save space, we report only the results for

h = 1/12, 1/252 in Tables 1–4 (each with two panels corresponding to T = 1, 10, respectively). Tables 1 and

2 report the cumulative distributions of T (κ− κ) under a fixed start-up when κ = 0.01, with x0 = µ = 0, 0.1,

respectively, and Tables 3 and 4 report the results when x0 is random.

Several striking features are present in these tables. First, the exact distribution results match to at least

the third decimal place with those obtained by 1 million simulations, in all the cases considered. This indicates

high accuracy of the exact results calculated by our numerical integration algorithm. In consistent with the

asymptotic results in Zhou and Yu (2010), there is no much difference between the results under the expanding

and mixed domains, and the infill asymptotics provide relatively better performance. Yet, the asymptotic

distribution under the infill domain may still provide poor approximation to the true distribution when the

data span is short, especially so in the left tails. While increasing data frequency does not affect much the

4Zhou and Yu (2010) did not give the expanding and infill asymptotic distribution results when κ = 0 and µ 6= 0. Thiscorresponds to the scenario, in a discrete framework, when no intercept is present in the true model, but a constant term isincluded in the regression. The expanding and infill asymptotic distribution results easily follow via the generalized delta method.

5In simulating the asymptotic (non-normal) results, 10,000 replications are used and a sample size of 5,000 is used to approximatethe integrals involving the Brownian motion by the discrete Riemann sums, with the exception that the infill asymptotic resultswhen x0 is random are calculated as averaging over 2,000 replications, where in each replication, x0 ∼ N(µ, σ2/(2κ)) and thediscrete AR(1) process is of sample size of 2,000.

8

asymptotic distributions, it does affect the true distribution, and the remarkable performance of the exact

distribution is robust to data frequency, as well as to data span and other aspects of model specification.

Second, the true distribution of κ is highly skewed to the right. Normality is a terrible approximation of the

finite-sample distribution of κ. Moreover, we can infer from these tables the exact/true median of T (κ− κ) in

all cases are substantially positive. (A direct calculation of the median is also possible, see the last paragraph

in this section to follow.) This suggests that κ can significantly over estimate κ in finite samples. This degree

of overestimation does not decrease with a higher data frequency (given a fixed data span). This is in line with

the observations made by Phillips and Yu (2005) and Tang and Chen (2009). On the other hand, increasing

data span might help alleviate this problem, though somewhat marginally.

Third, how the initial observation is spelled out affects significantly the exact distribution of κ. For example,

for the fixed start-up case, the exact distribution is less skewed to the right when x0 = 0 compared with when

x0 6= 0. Comparing the random start-up case versus the fixed start-up case with a known drift term (Table

3 versus Table 1), we see quite a difference in the exact distributions across the two cases and the former one

is less skewed; on the other hand, with a unknown drift term (Table 4 versus Table 2), there is virtually no

significant difference in the exact distributions across the two cases.6 This feature is related to the role of initial

observation in the unit-root test literature, see, for example, Muller and Elliott (2003) and Elliot and Muller

(2006). It also suggests that the conclusions in Tsui and Ali (1992, 1994) with x0 discarded should be examined

with more scrutiny.

Given the CDF function (2.7), one might be tempted to calculate the quantile function F−1κ (t), t ∈ [0, 1]

by Newton’s method of interpolation. However, this involves calculation of the PDF function, which requires

another round of numerical integration, in addition to the possible problem pointed out by Hillier (2001).

Instead, we suggest employing a very simple bisection search algorithm. Since it is relatively cheap to simulate

the asymptotic results and we have observed that the infill asymptotic results are more reliable compared with

the expanding and mixed asymptotic results, we start with the t-th empirical quantile of the simulated sample

for approximating the in-fill asymptotic results, say c0. If Fκ(c0) < t, we set c1 as the min {2t, 1}-th empirical

quantile of the simulated sample. (Typically, Fκ(c1) > t. If not, one can set c1 as the min {ct, 1}-th empirical

quantile of the simulated sample, c = 3, 4, · · · , until one finds Fκ(c1) > t.) If Fκ(c0) > t, we set c1 as the

t/2-th empirical quantile of the simulated sample. (Typically, Fκ(c1) < t. If not, one can set c1 as the ct-th

empirical quantile of the simulated sample, c = 1/3, 1/4, · · · , until one finds Fκ(c1) < t.) Given the two initial

points c0 and c1, a bisection search can then be straightforwardly applied to search numerically for F−1κ (t). This

6The effects of the initial observation x0 can be examined more carefully by looking at the characteristic functions presentedin Section 2.1. For fixed x0, the characteristic functions behave differently under zero and non-zero x0. When the drift term isunknown, we see that in the characteristic function, the exponent has terms involving α that dominate the initial value x0.

9

algorithm is in a similar spirit of the algorithm in Lu and King (2002).

3 An Empirical Example

The linear diffusion model has been used to study the short-term interest rate in the literature. Even though the

term structure literature has documented that the short-term interest rate is highly persistent, an agreement

has yet to reach among economists regarding whether there is a unit root in the time series.

Figure 1: Real Federal Fund Rate

-2

-1

0

1

2

3

4

5

90 92 94 96 98 00 02 04 06 08 10 12

Figure 1 displays the monthly real federal fund rate from January 1990 to October 2012.7 If we use the

augmented Dickey-Fuller test or Phillips-Perron test, we fail to reject the null of unit root at any conventional

level. If we use the KPSS test, on the other hand, we fail to reject the null of stationarity at any conventional

level. The mixed results are in line with the observation from Bierens (2000).8

If we are willing to use the linear diffusion model for the real federal fund rate, then based on our exact

distribution approach, we can construct straightforwardly the exact confidence intervals of the mean reversion

parameter κ.9 For comparison, we also report the confidence intervals under the infill sampling scheme.

7The real federal fund rate is calculated as the effective H-15 federal fund rate adjusted for the core PCE inflation rate. Theformer is retrieved from www.federalreserve.gov and the latter is retrieved from www.bea.gov.

8One possibility, as discussed in Bierens (2000), is that the series is nonlinear trend stationary.9The distribution of κ depends on the diffusion and drift parameters. We set them equal to the estimated values from the

sample. (Recall from Tang and Chen (2009) that estimation biases of the diffusions and drift parameters are virtually zero.) Also,we regard the first sample observation as fixed and treat the drift term as unknown.

10

Confidence Intervals of κ for Real Federal Fund Rate

99% 95% 90%

Exact [−0.1054, 1.1005] [−0.0531, 0.7940] [−0.0213, 0.6607]

Infill [−0.1032, 1.0799] [−0.0492, 0.7671] [−0.0210, 0.6327]

It can be seen that the null value of κ = 0 is contained in the confidence intervals. The exact confidence

intervals are wider compared with those from the infill asymptotic distribution. Based on the infill confidence

intervals alone we might not be confident to conclude that κ = 0, since we have already seen in the previous

section that the asymptotic distribution under the infill domain in general is good but may still provide poor

approximation to the true distribution in the left tail. (Note that the value of k = 0 lies on the left tail.) With

the exact confidence intervals, we are more confident to believe the non-mean-reverting hypothesis regarding

the federal fund rate.

4 Conclusions

We have investigated the exact finite-sample distribution of the estimated mean-reversion parameter in the

Ornstein-Uhlenbeck diffusion process. We have considered several different set-ups: known or unknown drift

term, fixed or random start-up value, and zero or positive mean-reversion parameter. In particular, we employ

numerical integration via analytical evaluation of a joint characteristic function. Our numerical calculations

demonstrate the remarkably reliable performance of the exact approach. It is found that the true distribution

of the maximum likelihood estimator of the mean-reversion parameter can be severely skewed in finite samples.

The asymptotic results under expanding and mixed domains in general perform worse than those under the infill

domain, though the latter may still perform poorly in the left tails. Our exact approach provides distribution

results of high accuracy, and thus it could be useful for conducting hypothesis testing and constructing confidence

intervals.

We note that the linear diffusion model, although extensively studied in the literature, is simple and re-

strictive in modeling financial time series. Nonlinear diffusion, diffusion-jump, and self-exiting jump models

have been proposed in the recent literature to accommodate hectic scenarios with large drops and recurring

crises. The estimation strategy and inference procedure in these models are more complicated. Typically, no

closed-form solution might be available for the estimator of interest. Therefore, studying the exact distribution

theory for such estimators for both Gaussian and non-Gaussian cases are extremely difficult and challenging,

and they are beyond the scope of this paper. Our efforts in this paper can be regarded as a starting point in

11

studying the exact finite-sample distribution theory in continuous-time models. By no means a simple extension

of our methodology can deliver finite-sample results in the more general nonlinear and non-Gaussian models.

However, this paper provides a message that the crude asymptotics (expanding, mixed, or infill) may give mis-

leading inferences in finite or even moderately large samples. Thus this calls for more caution in interpreting

the existing results, and more need for developing the exact finite-sample results for the more general models.

When the exact finite-sample results are not available, Edgeworth approximations, see Zhang, Mykland and

Aıt-Sahalia (2011), might provide better approximations than the asymptotics, and they might be regarded as

standing in between the exact and asymptotic results.

Appendix A: Derivation of ϕ(u, v)

When µ is known (0) and κ > 0 (with x0 fixed or random), or when there is no intercept in the discrete AR(1)

model and φ = 1 (κ = 0), ϕ(u, v) can follow from Tsui and Ali (1994) with slight modification. (Recall that we

have the initial observation x0 included in formulating the LS estimator φ, whereas in Tsui and Ali (1994) the

initial observation was discarded.)

When µ is unknown, κ > 0, and x0 is fixed,

φ =z′nMnAnzn + z0z

′nMne1,n

z′nA′nMnAnzn + 2z0z′nA

′nMne1,n + z20e

′1,nMne1,n

.

The density function of zn (conditional on z0) is

f (zn) = (2π)−n2 exp

[−∑ni=1 (zi − φzi−1)

2

2

]

= (2π)−n2 exp

{−1

2[z′n

(In + φ2Bn − 2φAn

)zn − 2φz0z

′ne1,n + φ2z20 ]

},

and the joint CF of the numerator and denominator in defining φ− φ is

ϕ (u, v) = (2π)−n2 exp

(−φ

2z202− i(uφ− v)z20e

′1,nMne1,n

)·∫ +∞

−∞exp

(−1

2z′nSnzn + z0z

′nδn

)dzn.

Note that e′1,nMne1,n = 1− n−1. Thus we have

ϕ (u, v) = |Sn|−1/2 exp

[−φ

2z202− i(uφ− v)z20

(1− 1

n

)+

1

2z20δ′nS−1n δn

]. (A.1)

12

If κ = 0 and there is an intercept in the AR(1) model, with x0 fixed, one can inspect that setting φ = 1 in (A.1)

and replacing z0 with z0 yield the corresponding CF.

When µ is unknown and x0 is random (and κ > 0),

φ =ζ′n+1A

Mn+1ζn+1

ζ′n+1BMn+1ζn+1

,

which is invariant to µ and σ2ε.

10 Without loss of generality, assume µ = 0 and σ2 = 2κ/(1 − φ2), so that

ζn+1 ∼ N(0n+1,V n+1/(1− φ2)).11 Then the density of ζn+1 is

f(ζn+1

)= (2π)

−n+12

∣∣∣∣ V n+1

1− φ2

∣∣∣∣−1/2 exp

[−1

2ζ′n+1

(V n+1

1− φ2

)−1ζn+1

],

and the joint CF of the numerator and denominator in defining φ− φ is

ϕ (u, v) = (2π)−n+12

∣∣∣∣ V n+1

1− φ2

∣∣∣∣−1/2 · ∫ +∞

−∞exp

(−1

2ζ′n+1T n+1ζn+1

)dχn+1.

Therefore,

ϕ (u, v) =

√1− φ2 |T n+1|−1/2 . (A.2)

Appendix B: Analytical Determinants and Inverses

This appendix first gives the analytical determinants and inverses of various matrices involved in evaluating

ϕ(u, v) and then verifies that these analytical expressions are valid.

First we introduce the determinant and inverse of a tridiagonal matrix. Let Cn be an n × n tridiagonal

matrix with c0 on its main diagonal and c1 6= 0 on its super- and sub-diagonals. (When c1 = 0, the results are

trivial.)

From Bernstein (2009, page 235), the determinant of |Cn| is as follows:

|Cn| =

(n+1)cn0

2nc02c1

= ±1

cn1 sin((n+1)θ)sin θ

c02c16= ±1

, (B.1)

where θ = arccos(c0/(2c1)).12 From Hu and O’Connell (1996), the symmetric C−1n has elements c(ij)n =

10φ is independent of µ because AMn+11n+1 = 0n+1, AM ′

n+11n+1 = 0n+1 and BMn+11n+1 = 0n+1.

11This is different from the case when no intercept is included in the AR(1) model.

12When c0 6= ±2c1, Bernstein (2009, page 235) gives |Cn| = (bn+11 − bn+1

2 )/(b1 − b2), where b1 = (c0 +√c20 − 4c21)/2 and

13

(−1)i+j |Ci−1| |Cn−j | /(ci−j1 |Cn|) for i ≤ j. Substituting the determinant result (B.1) yields

c(ij)n =

2i(n−j+1)(n+1)c0

(− c0

2c1

)i−jc02c1

= ±1

(−1)i+j sin(iθ) sin((n−j+1)θ)c1 sin θ sin((n+1)θ)

c02c16= ±1

, i ≤ j, (B.2)

With the explicit expression of c(ij)n , we can derive the follow results:

ι′nC−1n ιn =

n(n+1)(n+2)

6c0c02c1

= −1

2n2+4n+1−(−1)n4c0(n+1)

c02c1

= 1

n+14c1 cos2(θ/2) −

tan2(θ/2)[(−1)n+cos((n+1)θ)]2c1 sin θ sin((n+1)θ)

c02c16= ±1

, (B.3)

e′1,nC−1n ιn =

nc0

c02c1

= −1

2n+1−(−1)n2c0(n+1)

c02c1

= 1

sin((2n+1)θ/2)−(−1)n sin(θ/2)2c1 sin((n+1)θ) cos(θ/2)

c02c16= ±1

, (B.4)

e′1,nC−1n e1,n =

2n

c0(n+1)c02c1

= ±1

sin(nθ)c1 sin((n+1)θ)

c02c16= ±1

, (B.5)

e′1,nC−1n en,n =

2(−c0/(2c1))n+1

c0(n+1)c02c1

= ±1

(−1)n+1 sin(θ)c1 sin((n+1)θ)

c02c16= ±1

. (B.6)

In the sequel, let c0 = 1 + φ2 + 2i(uφ − v), c1 = −(φ + iu), c2 = 2i(u + v − uφ), and c3 = i(2φu − 2v − u).

Since φ > 0, the case of c0 = 2c1, corresponding to φ = −1 and v = 0, is ruled out.

Determinant of Rn

Note that Rn is a tridiagonal matrix with its main diagonal elements rn,ii = c0, i = 1, · · · n − 1, rn,ii = 1,

i = n, and sub- and super-diagonal elements c1. Expanding along the last row of Rn leads to

|Rn| = |Cn−1| − c21 |Cn−2| , (B.7)

where the determinants of Cn−1 and Cn−2 follow from (B.1).

b2 = (c0 −√c20 − 4c21)/2. This can be numerically unstable when b1 is close to b2. Using polar representation, we write b1 =

c1 (cos θ + i sin θ) , b2 = c1 (cos θ − i sin θ). Then it follows that when c0 6= ±2c1, |Cn| = [cn1 sin((n + 1)θ)]/ sin θ. We thankRaymond Kan for pointing out this result and the results (B.3)–(B.6) to follow.

14

Determinant of Sn

Note that

A′nιnι′nAn =

ιn−1ι′n−1 0n−1

0′n−1 0

, ιnι′nAn =

ιn−1ι′n−1 0n−1

ι′n−1 0

.

So

Sn = In + φ2Bn − φ(An +A′n

)− iu(MnAn +A′nMn) + 2i(uφ− v)A′nMnAn

= In + φ2Bn − φ(An +A′n

)− iu(An +A′n) + 2i(uφ− v)A′nAn

+n−1iuιnι′nAn + n−1iuA′nιnι

′n − 2n−1i(uφ− v)A′nιnι

′nAn

= Rn +i

n

[uιnι

′nAn + uA′nιnι

′n − 2(uφ− v)A′nιnι

′nAn

]= Rn +

i

n

2(u+ v − uφ)ιn−1ι′n−1 uιn−1

uι′n−1 0

∆n−1 an−1

a′n−1 1

,

where

∆n−1 = Cn−1 +c2nιn−1ι

′n−1, an−1 =

iu

nιn−1 + c1en−1,n−1.

Then immediately,

|Sn| = |∆n−1|(1− a′n−1∆

−1n−1an−1

), (B.8)

where

|∆n−1| = |Cn−1|(

1 +c2nι′n−1C

−1n−1ιn−1

), (B.9)

and

∆−1n−1 = C−1n−1 −c2

n+ c2ι′n−1C−1n−1ιn−1

C−1n−1ιn−1ι′n−1C

−1n−1. (B.10)

Keep in mind that (B.8) is valid only if ∆n−1 is nonsingular; (B.9) is valid only if Cn−1 is nonsingular; (B.10)

is valid only if Cn−1 is nonsingular and n+ c2ι′n−1Cn−1ιn−1 6= 0.

From (B.1), we see that |Cn−1| 6= 0. From (B.3), we also see that n+ c2ι′n−1Cn−1ιn−1 6= 0 for any positive

integer n. Further, these two conditions ensure that |∆n−1| 6= 0 so that the expression for |Sn| given by (B.8)

is valid. With |Cn−1| from (B.1) and ι′n−1C−1n−1ιn−1 from (B.3), we can easily calculate |∆n−1| in (B.8) via

15

(B.9). Note that the remaining term

a′n−1∆−1n−1an−1 = −u

2

n2ι′n−1C

−1n−1ιn−1 + c21e

′1,n−1C

−1n−1e1,n−1

+2ic1u

ne′1,n−1C

−1n−1ιn−1

− 2ic1c2u

n(n+ c2ι′n−1C−1n−1ιn−1)

ι′n−1C−1n−1ιn−1e

′1,n−1C

−1n−1ιn−1

+c2u

2

n2(n+ c2ι′n−1C−1n−1ιn−1)

(ι′n−1C−1n−1ιn−1)2

− c21c2

n+ c2ι′n−1C−1n−1ιn−1

(e′1,n−1C−1n−1ιn−1)2, (B.11)

where ι′n−1∆−1n−1ιn−1, e

′1,n−1C

−1n−1ιn−1, and e′1,n−1C

−1n−1e1,n−1 follow directly from (B.3), (B.4), and (B.5),

respectively.

Inverse of Sn

With ∆−1n−1 given by (B.10), the inverse of Sn is straightforward:

S−1n =

∆−1n−1 0n−1

0′n−1 0

+

∆−1n−1an−1

−1

( a′n−1∆−1n−1 −1

)1− a′n−1∆

−1n−1an−1

, (B.12)

if ∆n−1 is nonsingular and 1− a′n−1∆−1n−1an−1 6= 0. We have already showed that ∆n−1 is nonsingular. From

(B.11), we can verify that 1− a′n−1∆−1n−1an−1 6= 0 for any positive integer n.

Note that we need S−1n as δ′nS−1n δn appears in the CF (A.1). Given δn = iu(In − 2φA′n)Mne1,n +

2ivA′nMne1,n + φe1,n, we partition it as follows:

δn =

iu(e1,n−1 − 1nιn−1) + 2i(φu−v)

n ιn−1 + φe1,n−1

− iun

δ1:n−1,n

− iun

.

16

So

δ′nS−1n δn = δ′n

∆−1n−1 0n−1

0′n−1 0

δn

+

δ′n

∆−1n−1an−1

−1

( a′n−1∆−1n−1 −1

)δn

1− a′n−1∆−1n−1an−1

= δ′1:n−1,n∆−1n−1δ1:n−1,n

+(δ′1:n−1,n∆−1n−1an−1)2 + 2iu

n δ′1:n−1,n∆−1n−1an−1 − u2

n2

1− a′n−1∆−1n−1an−1

, (B.13)

where a′n−1∆−1n−1an−1 follows from (B.11) and

δ′1:n−1,n∆−1n−1δ1:n−1,n =c23n2ι′n−1C

−1n−1ιn−1 +

2c1c3n

e′1,n−1C−1n−1ιn−1

+c21e′1,n−1C

−1n−1e1,n−1

− c2c23

n2(n+ c2ι′n−1C−1n−1ιn−1)

(ι′n−1C

−1n−1ιn−1

)2− c21c2

n+ c2ι′n−1C−1n−1ιn−1

(e′1,n−1C−1n−1ιn−1)2

− 2c1c2c3

n(n+ c2ι′n−1C−1n−1ιn−1)

e′1,n−1C−1n−1ιn−1ι

′n−1C

−1n−1ιn−1, (B.14)

δ′1:n−1,n∆−1n−1an−1 =iuc3n2ι′n−1C

−1n−1ιn−1 − c21e′1,n−1C

−1n−1en−1,n−1

−c1c2ne′1,n−1C

−1n−1ιn−1

+c21c2

n+ c2ι′n−1C−1n−1ιn−1

(e′1,n−1C−1n−1ιn−1)2

− iuc2c3

n2(n+ c2ι′n−1C−1n−1ιn−1)

(ι′n−1C−1n−1ιn−1)2

+c1c

22

n(n+ c2ι′n−1C−1n−1ιn−1)

e′1,n−1C−1n−1ιn−1ι

′n−1C

−1n−1ιn−1. (B.15)

which can be calculated by substituting (B.3)–(B.6).

Determinant of T n+1

Note that

T n+1 = (1− φ2)V −1n+1 − iu(AMn+1 +AM ′

n+1) + 2i(uφ− v)BMn+1

17

= (1− φ2)V −1n+1 − iu(An+1 +A′n+1) + 2i(uφ− v)Bn+1

+iu

n

0′n 0

ιnι′n 0n

+

0n ιnι′n

0 0′n

− 2i(uφ− v)

n

ιnι′n 0n

0′n 0

= Rn+1 − φ2e1,n+1e

′1,n+1

+i

n

2(v − uφ) (u+ 2v − 2uφ)ι′n−1 u

(u+ 2v − 2uφ)ιn−1 2(v + u− uφ)ιn−1ι′n−1 uιn−1

u uι′n−1 0

=

1 + 2i(uφ− v)− 2i(uφ−v)

n b′n−1iun

bn−1 ∆n−1 an−1

iun a′n−1 1

∆∗n a∗n

a∗′n 1

,

where

∆∗n =

1 + 2i(uφ− v)− 2i(uφ−v)n b′n−1

bn−1 ∆n−1

,

a∗n = (iu

n, a′n−1)′,

bn−1 = c1e1,n−1 −c3nιn−1.

Following the same strategy as before,

|T n+1| = |∆∗n|(1− a∗′n∆∗−1n a∗n

), (B.16)

where

|∆∗n| = |∆n−1|(

1 + 2i(uφ− v)− 2i(uφ− v)

n− b′n−1∆

−1n−1bn−1

), (B.17)

and

∆∗−1n =

0 0′n−1

0n−1 ∆−1n−1

18

+

−1

∆−1n−1bn−1

( −1 b′n−1∆−1n−1

)1 + 2i(uφ− v)− 2i(uφ−v)

n − b′n−1∆−1n−1bn−1

. (B.18)

For (B.16) to be valid, ∆∗n needs to be nonsingular; for (B.17) to be valid, ∆n−1 needs to be nonsingular;

for (B.18) to be valid, ∆n−1 needs to be nonsingular and 1 + 2i(uφ− v)− 2i(uφ− v)/n− b′n−1∆−1n−1bn−1 6= 0.

We have already shown that ∆n−1 is nonsingular. Note that

b′n−1∆−1n−1bn−1 =

c23n2ι′n−1C

−1n−1ιn−1 −

2c1c3n

e′1,n−1C−1n−1ιn−1

+c21e′1,n−1C

−1n−1e1,n−1

− c2c23

n2(n+ c2ι′n−1C−1n−1ιn−1)

(ι′n−1C−1n−1ιn−1)2

− c21c2

n+ c2ι′n−1C−1n−1ιn−1

(e′1,n−1C−1n−1ιn−1)2

+2c1c2c3

n(n+ c2ι′n−1C−1n−1ιn−1)

e′1,n−1C−1n−1ιn−1ι

′n−1C

−1n−1ιn−1, (B.19)

which can be evaluated with analytical expressions from (B.3)–(B.5), and we can verify that 1 + 2i(uφ − v) −

2i(uφ− v)/n− b′n−1∆−1n−1bn−1 6= 0 for any positive integer n.

For us to use (B.16), we still need expression for a∗′n∆∗−1n a∗n. By substitution,

a∗′n∆∗−1n a∗n = a′n−1∆−1n−1an−1

+−u2 − 2inua′n−1∆

−1n−1bn−1 + n2(a′n−1∆

−1n−1bn−1)2

n2 + 2in2(uφ− v)− 2in(uφ− v)− n2b′n−1∆−1n−1bn−1

, (B.20)

where a′n−1∆−1n−1an−1 is given by (B.11), b′n−1∆

−1n−1bn−1 is given by (B.19), and

a′n−1∆−1n−1bn−1 = − iuc3

n2ι′n−1C

−1n−1ιn−1 +

c1c2ne′1,n−1C

−1n−1ιn−1

+c21e′1,n−1C

−1n−1en−1,n−1

+iuc2c3

n2(n+ c2ι′n−1C−1n−1ιn−1)

(ι′n−1C−1n−1ιn−1)2

− c21c2

n+ c2ι′n−1C−1n−1ιn−1

(e′1,n−1C−1n−1ιn−1)2

− c1c22

n(n+ c2ι′n−1C−1n−1ιn−1)

e′1,n−1C−1n−1ιn−1ι

′n−1C

−1n−1ιn−1, (B.21)

which can be evaluated with analytical expressions from (B.3)–(B.6).

19

Appendix C: Numerical Integration

Given the characteristic functions in Section 2.1, we need to implement numerical integration to calculate (2.6)

via (2.7). This can be straightforwardly implemented using Matlab’s quadgk command. One caveat to note

is that the square root function in the complex domain is not continuous. One choice is to follow Perron

(1989) to identify explicitly the discontinuous points by grid search and then integrate by parts. The search,

however, might be inefficient and time-consuming. Instead, we use the following algorithm so that the integrand

function for quadgk is always continuous. Let g (t) =√a(t) + ib(t) denote the integrand function in question

with t ∈ [l, u] . quadgk requires the integrand function to accept a vector (t1, t2, · · · , tn) and returns a vector of

output. Let θi = arg (a(ti) + ib(ti)) ∈ [−π, π] and denote ai = a (ti) , bi = b (ti) , and gi = g (ti) .

1. Start with t1 and set g1 = sqrt (a1 + ib1) . Set k = 0.

2. Beginning with t2, if ai < 0, ai−1 < 0, and bibi−1 <= 0, set k = k + 1; otherwise, k is unchanged. Set

gi =√a2i + b2i (cos (θ∗i /2) + i sin (θ∗i /2)) , where θ∗i = θi + 2kπ.

20

Tab

le1,

Pan

elA

(T=

1):

Pr(T

(κ−κ

)≤w

),F

ixed

x0,κ

=0.

01,x0

=0,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0002

0.00

02

0.0

000

0.0

000

0.0

000

0.0

001

0.0

000

0.0

000

0.0

000

0.0

000

-30.

0037

0.00

36

0.0

000

0.0

000

0.0

013

0.0

013

0.0

013

0.0

000

0.0

000

0.0

014

-20.

0201

0.02

02

0.0

000

0.0

000

0.0

109

0.0

110

0.0

112

0.0

000

0.0

000

0.0

105

-1.5

0.04

870.

0485

0.0

000

0.0

000

0.0

317

0.0

323

0.0

326

0.0

000

0.0000

0.0

310

-10.

1126

0.11

29

0.0

000

0.0

000

0.0

884

0.0

892

0.0

888

0.0

000

0.0

000

0.0

876

-0.8

0.15

110.

1515

0.0

000

0.0

000

0.1

249

0.1

261

0.1

253

0.0

000

0.0000

0.1

245

-0.6

0.19

580.

1963

0.0

000

0.0

000

0.1

679

0.1

691

0.1

697

0.0

000

0.0000

0.1

688

-0.4

0.24

390.

2444

0.0

023

0.0

023

0.2

173

0.2

190

0.2

186

0.0

023

0.0023

0.2

171

-0.2

0.29

280.

2931

0.0

787

0.0

786

0.2

682

0.2

688

0.2

686

0.0

787

0.0786

0.2

682

-0.1

0.31

690.

3174

0.2

398

0.2

398

0.2

933

0.2

946

0.2

932

0.2

398

0.2398

0.2

934

-0.0

10.

3380

0.33

84

0.4

718

0.4

718

0.3

153

0.3

154

0.3

153

0.4

718

0.4

718

0.3

157

-0.0

010.

3401

0.34

05

0.4

972

0.4

972

0.3

175

0.3

180

0.3

175

0.4

972

0.4972

0.3

179

00.

3403

0.34

08

0.5

000

0.5

000

0.3

177

0.3

183

0.3

177

0.5

000

0.5

000

0.3

181

0.00

10.

3406

0.34

10

0.5

028

0.5

028

0.3

180

0.3

185

0.3

180

0.5

028

0.5

028

0.3

184

0.01

0.34

270.

3432

0.5

282

0.5

282

0.3

202

0.3

207

0.3

202

0.5

282

0.5282

0.3

203

0.1

0.36

320.

3638

0.7

602

0.7

602

0.3

411

0.3

421

0.3

414

0.7

602

0.7

602

0.3

414

0.2

0.38

530.

3856

0.9

213

0.9

214

0.3

644

0.3

651

0.3

644

0.9

213

0.9

214

0.3

649

0.4

0.42

710.

4271

0.9

977

0.9

977

0.4

081

0.4

095

0.4

088

0.9

977

0.9

977

0.4

086

0.6

0.46

600.

4660

1.0

000

1.0

000

0.4

492

0.4

512

0.4

507

1.0

000

1.0

000

0.4

516

0.8

0.50

240.

5026

1.0

000

1.0

000

0.4

889

0.4

904

0.4

899

1.0

000

1.0

000

0.4

907

10.

5366

0.53

72

1.0

000

1.0

000

0.5

255

0.5

267

0.5

263

1.0

000

1.0000

0.5

273

1.5

0.61

110.

6115

1.0

000

1.0

000

0.6

050

0.6

053

0.6

051

1.0

000

1.0

000

0.6

055

20.

6711

0.67

13

1.0

000

1.0

000

0.6

700

0.6

691

0.6

687

1.0

000

1.0000

0.6

695

30.

7592

0.75

94

1.0

000

1.0

000

0.7

628

0.7

638

0.7

634

1.0

000

1.0000

0.7

647

50.

8617

0.86

18

1.0

000

1.0

000

0.8

757

0.8

746

0.8

742

1.0

000

1.0000

0.8

755

80.

9318

0.93

18

1.0

000

1.0

000

0.9

490

0.9

485

0.9

484

1.0

000

1.0000

0.9

498

200.

9906

0.99

04

1.0

000

1.0

000

0.9

980

0.9

980

0.9

981

1.0

000

1.0

000

0.9

982

500.

9995

0.99

95

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

21

Tab

le1,

Panel

B(T

=10):

Pr(T

(κ−κ

)≤w

),F

ixed

x0,κ

=0.

01,x0

=0,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0000

0.00

00

0.1

319

0.1

318

0.0

000

0.0

000

0.0

000

0.1

318

0.1

318

0.0

000

-30.

0015

0.00

15

0.2

513

0.2

512

0.0

014

0.0

013

0.0

013

0.2

512

0.2

512

0.0

014

-20.

0124

0.01

24

0.3

274

0.3

274

0.0

114

0.0

116

0.0

115

0.3

274

0.3

274

0.0

120

-1.5

0.03

550.

0356

0.3

687

0.3

687

0.0

347

0.0

341

0.0

342

0.3

687

0.3687

0.0

348

-10.

0940

0.09

38

0.4

116

0.4

115

0.0

924

0.0

918

0.0

919

0.4

115

0.4

115

0.0

929

-0.8

0.13

100.

1308

0.4

290

0.4

290

0.1

291

0.1

288

0.1

289

0.4

290

0.4290

0.1

284

-0.6

0.17

490.

1745

0.4

467

0.4

466

0.1

734

0.1

725

0.1

729

0.4

466

0.4466

0.1

715

-0.4

0.22

260.

2221

0.4

644

0.4

644

0.2

207

0.2

194

0.2

206

0.4

644

0.4644

0.2

192

-0.2

0.27

150.

2710

0.4

822

0.4

822

0.2

703

0.2

677

0.2

698

0.4

822

0.4822

0.2

694

-0.1

0.29

570.

2952

0.4

911

0.4

911

0.2

958

0.2

928

0.2

941

0.4

911

0.4911

0.2

935

-0.0

10.

3171

0.31

66

0.4

991

0.4

991

0.3

169

0.3

152

0.3

155

0.4

991

0.4

991

0.3

153

-0.0

010.

3192

0.31

88

0.4

999

0.4

999

0.3

191

0.3

163

0.3

176

0.4

999

0.4999

0.3

175

00.

3194

0.31

90

0.5

000

0.5

000

0.3

194

0.3

166

0.3

178

0.5

000

0.5

000

0.3

177

0.00

10.

3197

0.31

93

0.5

001

0.5

001

0.3

195

0.3

168

0.3

181

0.5

001

0.5

001

0.3

179

0.01

0.32

180.

3213

0.5

009

0.5

009

0.3

216

0.3

190

0.3

201

0.5

009

0.5009

0.3

199

0.1

0.34

270.

3422

0.5

089

0.5

089

0.3

424

0.3

404

0.3

410

0.5

089

0.5

089

0.3

415

0.2

0.36

540.

3647

0.5

178

0.5

178

0.3

655

0.3

637

0.3

639

0.5

178

0.5

178

0.3

641

0.4

0.41

070.

4082

0.5

356

0.5

356

0.4

101

0.4

077

0.4

077

0.5

356

0.5

356

0.4

077

0.6

0.45

050.

4494

0.5

533

0.5

534

0.4

518

0.4

493

0.4

493

0.5

534

0.5

534

0.4

500

0.8

0.48

920.

4882

0.5

710

0.5

710

0.4

904

0.4

883

0.4

882

0.5

710

0.5

710

0.4

891

10.

5204

0.52

39

0.5

884

0.5

885

0.5

264

0.5

244

0.5

244

0.5

885

0.5885

0.5

252

1.5

0.60

300.

6017

0.6

313

0.6

313

0.6

059

0.6

027

0.6

033

0.6

313

0.6

313

0.6

044

20.

6663

0.66

53

0.6

726

0.6

726

0.6

683

0.6

664

0.6

674

0.6

726

0.6726

0.6

681

30.

7607

0.76

02

0.7

487

0.7

488

0.7

636

0.7

616

0.7

627

0.7

488

0.7488

0.7

629

50.

8720

0.87

17

0.8

681

0.8

682

0.8

735

0.8

735

0.8

740

0.8

682

0.8682

0.8

739

80.

9467

0.94

68

0.9

631

0.9

632

0.9

484

0.9

484

0.9

487

0.9

632

0.9632

0.9

489

200.

9977

0.99

77

1.0

000

1.0

000

0.9

981

0.9

982

0.9

981

1.0

000

1.0

000

0.9

982

501.

0000

1.00

00

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

22

Tab

le2,

Pan

elA

(T=

1):

Pr(T

(κ−κ

)≤w

),F

ixed

x0,κ

=0.

01,x0

=0.

1,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0001

0.00

01

0.0

000

0.0

000

0.0

000

0.0

001

0.0

000

0.0

000

0.0

000

0.0

000

-30.

0016

0.00

16

0.0

000

0.0

000

0.0

003

0.0

004

0.0

004

0.0

000

0.0

000

0.0

004

-20.

0060

0.00

60

0.0

000

0.0

000

0.0

021

0.0

020

0.0

022

0.0

000

0.0

000

0.0

021

-1.5

0.01

140.

0114

0.0

000

0.0

000

0.0

049

0.0

045

0.0

051

0.0

000

0.0000

0.0

049

-10.

0209

0.02

09

0.0

000

0.0

000

0.0

108

0.0

113

0.0

112

0.0

000

0.0

000

0.0

108

-0.8

0.02

630.

0264

0.0

000

0.0

000

0.0

146

0.0

152

0.0

151

0.0

000

0.0000

0.0

144

-0.6

0.03

290.

0330

0.0

000

0.0

000

0.0

194

0.0

188

0.0

199

0.0

000

0.0000

0.0

192

-0.4

0.04

080.

0409

0.0

023

0.0

023

0.0

258

0.0

263

0.0

262

0.0

023

0.0023

0.0

251

-0.2

0.05

010.

0501

0.0

787

0.0

787

0.0

332

0.0

339

0.0

339

0.0

787

0.0787

0.0

324

-0.1

0.05

530.

0554

0.2

398

0.2

398

0.0

373

0.0

379

0.0

383

0.2

398

0.2398

0.0

369

-0.0

10.

0603

0.06

03

0.4

718

0.4

718

0.0

417

0.0

425

0.0

425

0.4

718

0.4

718

0.0

412

-0.0

010.

0609

0.06

08

0.4

972

0.4

972

0.0

421

0.0

429

0.0

430

0.4

972

0.4972

0.0

418

00.

0609

0.06

09

0.5

000

0.5

000

0.0

422

0.0

430

0.0

430

0.5

000

0.5

000

0.0

418

0.00

10.

0610

0.06

09

0.5

028

0.5

028

0.0

423

0.0

430

0.0

431

0.5

028

0.5

028

0.0

419

0.01

0.06

150.

0615

0.5

282

0.5

282

0.0

427

0.0

435

0.0

436

0.5

282

0.5282

0.0

423

0.1

0.06

690.

0669

0.7

602

0.7

603

0.0

474

0.0

484

0.0

483

0.7

603

0.7

603

0.0

470

0.2

0.07

320.

0732

0.9

213

0.9

214

0.0

532

0.0

541

0.0

539

0.9

214

0.9

214

0.0

525

0.4

0.08

710.

0869

0.9

977

0.9

977

0.0

655

0.0

665

0.0

665

0.9

977

0.9

977

0.0

649

0.6

0.10

230.

1021

1.0

000

1.0

000

0.0

798

0.0

809

0.0

809

1.0

000

1.0

000

0.0

791

0.8

0.11

900.

1187

1.0

000

1.0

000

0.0

952

0.0

399

0.0

967

1.0

000

1.0

000

0.0

950

10.

1368

0.13

66

1.0

000

1.0

000

0.1

130

0.1

145

0.1

143

1.0

000

1.0000

0.1

125

1.5

0.18

540.

1851

1.0

000

1.0

000

0.1

620

0.1

643

0.1

641

1.0

000

1.0

000

0.1

635

20.

2380

0.23

80

1.0

000

1.0

000

0.2

187

0.2

207

0.2

206

1.0

000

1.0000

0.2

186

30.

3477

0.34

75

1.0

000

1.0

000

0.3

423

0.3

423

0.3

419

1.0

000

1.0000

0.3

410

50.

5460

0.54

56

1.0

000

1.0

000

0.5

641

0.5

634

0.5

629

1.0

000

1.0000

0.5

658

80.

7392

0.73

86

1.0

000

1.0

000

0.7

840

0.7

792

0.7

787

1.0

000

1.0000

0.7

812

200.

9562

0.95

62

1.0

000

1.0

000

0.9

879

0.9

873

0.9

872

1.0

000

1.0

000

0.9

877

500.

9977

0.99

77

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

23

Tab

le2,

Pan

elB

(T=

10):

Pr(T

(κ−κ

)≤w

),F

ixed

x0,κ

=0.

01,x0

=0.

1,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0000

0.00

00

0.1

319

0.1

318

0.0

000

0.0

000

0.0

000

0.1

318

0.1

318

0.0

000

-30.

0005

0.00

05

0.2

513

0.2

512

0.0

004

0.0

004

0.0

004

0.2

512

0.2

512

0.0

004

-20.

0025

0.00

26

0.3

274

0.3

274

0.0

023

0.0

022

0.0

022

0.3

274

0.3

274

0.0

024

-1.5

0.00

560.

0058

0.3

687

0.3

687

0.0

052

0.0

052

0.0

051

0.3

687

0.3687

0.0

054

-10.

0121

0.01

24

0.4

116

0.4

115

0.0

115

0.0

114

0.0

114

0.4

115

0.4

115

0.0

120

-0.8

0.01

600.

0165

0.4

290

0.4

290

0.0

152

0.0

153

0.0

152

0.4

290

0.4290

0.0

158

-0.6

0.02

130.

0215

0.4

467

0.4

466

0.0

199

0.0

202

0.0

203

0.4

466

0.4466

0.0

210

-0.4

0.02

760.

0279

0.4

644

0.4

644

0.0

260

0.0

257

0.0

265

0.4

644

0.4644

0.0

274

-0.2

0.03

540.

0357

0.4

822

0.4

822

0.0

333

0.0

341

0.0

341

0.4

822

0.4822

0.0

351

-0.1

0.03

980.

0401

0.4

911

0.4

911

0.0

376

0.0

384

0.0

385

0.4

911

0.4911

0.0

393

-0.0

10.

0441

0.04

45

0.4

991

0.4

991

0.0

420

0.0

425

0.0

426

0.4

991

0.4

991

0.0

436

-0.0

010.

0446

0.04

49

0.4

999

0.4

999

0.0

424

0.0

430

0.0

431

0.4

999

0.4999

0.0

442

00.

0446

0.04

50

0.5

000

0.5

000

0.0

425

0.0

430

0.0

432

0.5

000

0.5

000

0.0

443

0.00

10.

0447

0.04

50

0.5

001

0.5

001

0.0

426

0.0

431

0.0

432

0.5

001

0.5

001

0.0

444

0.01

0.04

510.

0455

0.5

009

0.5

009

0.0

430

0.0

434

0.0

437

0.5

009

0.5009

0.0

447

0.1

0.04

990.

0503

0.5

089

0.5

089

0.0

475

0.0

484

0.0

484

0.5

089

0.5

089

0.0

492

0.2

0.05

550.

0560

0.5

178

0.5

178

0.0

534

0.0

540

0.0

540

0.5

178

0.5

178

0.0

547

0.4

0.06

800.

0685

0.5

356

0.5

356

0.0

662

0.0

664

0.0

665

0.5

356

0.5

356

0.0

671

0.6

0.08

220.

0829

0.5

533

0.5

534

0.0

797

0.0

805

0.0

807

0.5

534

0.5

534

0.0

819

0.8

0.09

790.

0988

0.5

710

0.5

710

0.0

954

0.0

962

0.0

965

0.5

710

0.5

710

0.0

978

10.

1151

0.11

62

0.5

884

0.5

885

0.1

123

0.1

135

0.1

137

0.5

885

0.5885

0.1

148

1.5

0.16

400.

1651

0.6

313

0.6

313

0.1

613

0.1

627

0.1

629

0.6

313

0.6

313

0.1

632

20.

2195

0.22

07

0.6

726

0.6

726

0.2

175

0.2

186

0.2

190

0.6

726

0.6726

0.2

172

30.

3394

0.34

06

0.7

487

0.7

488

0.3

393

0.3

398

0.3

398

0.7

488

0.7488

0.3

383

50.

5585

0.55

97

0.8

681

0.8

682

0.5

624

0.5

613

0.5

613

0.8

682

0.8682

0.5

584

80.

7740

0.77

42

0.9

631

0.9

632

0.7

822

0.7

789

0.7

796

0.9

632

0.9632

0.7

781

200.

9857

0.98

56

1.0

000

1.0

000

0.9

884

0.9

880

0.9

881

1.0

000

1.0

000

0.9

885

501.

0000

1.00

00

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

24

Tab

le3,

Pan

elA

(T=

1):

Pr(T

(κ−κ

)≤w

),R

an

domx0,κ

=0.

01,µ

=0,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0000

0.00

00

0.0

000

0.0

000

0.0

099

0.0

000

0.0

000

0.0

000

0.0

000

0.0

099

-30.

0001

0.00

01

0.0

000

0.0

000

0.0

158

0.0

001

0.0

001

0.0

000

0.0

000

0.0

155

-20.

0008

0.00

09

0.0

000

0.0

000

0.0

210

0.0

005

0.0

005

0.0

000

0.0

000

0.0

203

-1.5

0.00

250.

0025

0.0

000

0.0

000

0.0

250

0.0

018

0.0

018

0.0

000

0.0000

0.0

242

-10.

0084

0.00

84

0.0

000

0.0

000

0.0

339

0.0

071

0.0

070

0.0

000

0.0

000

0.0

328

-0.8

0.01

440.

0145

0.0

000

0.0

000

0.0

423

0.0

127

0.0

127

0.0

000

0.0000

0.0

412

-0.6

0.02

640.

0265

0.0

000

0.0

000

0.0

581

0.0

241

0.0

242

0.0

000

0.0000

0.0

580

-0.4

0.05

360.

0536

0.0

023

0.0

023

0.0

919

0.0

506

0.0

508

0.0

023

0.0023

0.0

892

-0.2

0.13

430.

1340

0.0

787

0.0

787

0.1

715

0.1

302

0.1

297

0.0

787

0.0787

0.1

651

-0.1

0.24

300.

2432

0.2

398

0.2

398

0.2

658

0.2

382

0.2

378

0.2

398

0.2398

0.2

613

-0.0

10.

4202

0.42

08

0.4

718

0.4

718

0.4

232

0.4

152

0.4

145

0.4

718

0.4

718

0.4

227

-0.0

010.

4406

0.44

11

0.4

972

0.4

972

0.4

427

0.4

355

0.4

348

0.4

972

0.4972

0.4

427

00.

4428

0.44

34

0.5

000

0.5

000

0.4

449

0.4

377

0.4

370

0.5

000

0.5

000

0.4

450

0.00

10.

4451

0.44

56

0.5

028

0.5

028

0.4

471

0.4

400

0.4

393

0.5

028

0.5

028

0.4

472

0.01

0.46

530.

4658

0.5

282

0.5

282

0.4

669

0.4

602

0.4

596

0.5

282

0.5282

0.4

676

0.1

0.63

610.

6365

0.7

602

0.7

603

0.6

472

0.6

315

0.6

310

0.7

603

0.7

603

0.6

526

0.2

0.74

450.

7454

0.9

213

0.9

214

0.7

733

0.7

404

0.7

403

0.9

214

0.9

214

0.7

814

0.4

0.83

900.

8394

0.9

977

0.9

977

0.8

816

0.8

360

0.8

360

0.9

977

0.9

977

0.8

822

0.6

0.88

030.

8807

1.0

000

1.0

000

0.9

218

0.8

781

0.8

780

1.0

000

1.0

000

0.9

199

0.8

0.90

410.

9045

1.0

000

1.0

000

0.9

414

0.9

025

0.9

024

1.0

000

1.0

000

0.9

405

10.

9200

0.92

05

1.0

000

1.0

000

0.9

530

0.9

189

0.9

189

1.0

000

1.0000

0.9

526

1.5

0.94

460.

9451

1.0

000

1.0

000

0.9

684

0.9

441

0.9

443

1.0

000

1.0

000

0.9

676

20.

9590

0.95

93

1.0

000

1.0

000

0.9

760

0.9

590

0.9

591

1.0

000

1.0000

0.9

748

30.

9750

0.97

51

1.0

000

1.0

000

0.9

837

0.9

756

0.9

757

1.0

000

1.0000

0.9

826

50.

9886

0.98

86

1.0

000

1.0

000

0.9

901

0.9

897

0.9

897

1.0

000

1.0000

0.9

895

80.

9954

0.99

52

1.0

000

1.0

000

0.9

937

0.9

966

0.9

965

1.0

000

1.0000

0.9

935

200.

9995

0.99

95

1.0

000

1.0

000

0.9

975

0.9

999

0.9

999

1.0

000

1.0

000

0.9

974

501.

0000

1.00

00

1.0

000

1.0

000

0.9

990

1.0

000

1.0

000

1.0

000

1.0

000

0.9

990

100

1.00

001.

0000

1.0

000

1.0

000

0.9

995

1.0

000

1.0

000

1.0

000

1.0000

0.9

995

25

Tab

le3,

Pan

elB

(T=

10):

Pr(T

(κ−κ

)≤w

),R

an

domx0,κ

=0.

01,µ

=0,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0000

0.00

00

0.1

319

0.1

318

0.0

265

0.0

000

0.0

000

0.1

318

0.1

318

0.0

260

-30.

0002

0.00

02

0.2

513

0.2

512

0.0

418

0.0

002

0.0

001

0.2

512

0.2

512

0.0

407

-20.

0019

0.00

19

0.3

274

0.3

274

0.0

548

0.0

019

0.0

017

0.3

274

0.3

274

0.0

527

-1.5

0.00

630.

0065

0.3

687

0.3

687

0.0

639

0.0

062

0.0

062

0.3

687

0.3687

0.0

611

-10.

0235

0.02

37

0.4

116

0.4

115

0.0

850

0.0

231

0.0

230

0.4

115

0.4

115

0.0

811

-0.8

0.04

110.

0410

0.4

290

0.4

290

0.1

053

0.0

405

0.0

406

0.4

290

0.4290

0.1

013

-0.6

0.07

360.

0731

0.4

467

0.4

466

0.1

432

0.0

729

0.0

729

0.4

466

0.4466

0.1

404

-0.4

0.13

420.

1338

0.4

644

0.4

644

0.2

081

0.1

334

0.1

332

0.4

644

0.4644

0.2

077

-0.2

0.23

940.

2393

0.4

822

0.4

822

0.2

931

0.2

385

0.2

385

0.4

822

0.4822

0.2

944

-0.1

0.31

020.

3084

0.4

911

0.4

911

0.3

441

0.3

073

0.3

076

0.4

911

0.4911

0.3

458

-0.0

10.

3760

0.37

40

0.4

991

0.4

991

0.3

991

0.3

730

0.3

730

0.4

991

0.4

991

0.4

016

-0.0

010.

3805

0.38

04

0.4

999

0.4

999

0.4

052

0.3

795

0.3

797

0.4

999

0.4999

0.4

077

00.

3812

0.38

12

0.5

000

0.5

000

0.4

059

0.3

803

0.3

804

0.5

000

0.5

000

0.4

084

0.00

10.

3819

0.38

19

0.5

001

0.5

001

0.4

065

0.3

810

0.3

811

0.5

001

0.5

001

0.4

091

0.01

0.38

850.

3884

0.5

009

0.5

009

0.4

127

0.3

875

0.3

878

0.5

009

0.5009

0.4

153

0.1

0.45

120.

4510

0.5

089

0.5

089

0.4

779

0.4

502

0.4

505

0.5

089

0.5

089

0.4

813

0.2

0.51

350.

5134

0.5

178

0.5

178

0.5

553

0.5

126

0.5

132

0.5

178

0.5

178

0.5

588

0.4

0.61

130.

6108

0.5

356

0.5

356

0.7

052

0.6

106

0.6

111

0.5

356

0.5

356

0.7

094

0.6

0.68

040.

6803

0.5

533

0.5

534

0.7

949

0.6

799

0.6

801

0.5

534

0.5

534

0.7

980

0.8

0.73

090.

7308

0.5

710

0.5

710

0.8

479

0.7

305

0.7

311

0.5

710

0.5

710

0.8

509

10.

7694

0.76

93

0.5

884

0.5

885

0.8

805

0.7

691

0.7

695

0.5

885

0.5885

0.8

821

1.5

0.83

490.

8349

0.6

313

0.6

313

0.9

208

0.8

348

0.8

349

0.6

313

0.6

313

0.9

206

20.

8763

0.87

59

0.6

726

0.6

726

0.9

393

0.8

763

0.8

765

0.6

726

0.6726

0.9

389

30.

9249

0.92

49

0.7

487

0.7

488

0.9

585

0.9

251

0.9

251

0.7

488

0.7488

0.9

576

50.

9677

0.96

76

0.8

681

0.8

682

0.9

744

0.9

680

0.9

680

0.8

682

0.8682

0.9

738

80.

9891

0.98

90

0.9

631

0.9

632

0.9

838

0.9

894

0.9

896

0.9

632

0.9632

0.9

834

200.

9997

0.99

97

1.0

000

1.0

000

0.9

934

0.9

998

0.9

998

1.0

000

1.0

000

0.9

933

501.

0000

1.00

00

1.0

000

1.0

000

0.9

973

1.0

000

1.0

000

1.0

000

1.0

000

0.9

973

100

1.00

001.

0000

1.0

000

1.0

000

0.9

987

1.0

000

1.0

000

1.0

000

1.0000

0.9

987

26

Tab

le4,

Pan

elA

(T=

1):

Pr(T

(κ−κ

)≤w

),R

an

domx0,κ

=0.

01,µ

=0.

1,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0001

0.00

01

0.0

000

0.0

000

0.0

000

0.0

001

0.0

000

0.0

000

0.0

000

0.0

000

-30.

0016

0.00

16

0.0

000

0.0

000

0.0

003

0.0

004

0.0

004

0.0

000

0.0

000

0.0

003

-20.

0061

0.00

60

0.0

000

0.0

000

0.0

021

0.0

020

0.0

023

0.0

000

0.0

000

0.0

021

-1.5

0.01

140.

0114

0.0

000

0.0

000

0.0

049

0.0

045

0.0

053

0.0

000

0.0000

0.0

049

-10.

0210

0.02

10

0.0

000

0.0

000

0.0

109

0.0

113

0.0

115

0.0

000

0.0

000

0.0

109

-0.8

0.02

640.

0264

0.0

000

0.0

000

0.0

148

0.0

152

0.0

155

0.0

000

0.0000

0.0

147

-0.6

0.03

310.

0330

0.0

000

0.0

000

0.0

197

0.0

189

0.0

205

0.0

000

0.0000

0.0

197

-0.4

0.04

100.

0410

0.0

023

0.0

023

0.0

258

0.0

265

0.0

269

0.0

023

0.0023

0.0

258

-0.2

0.05

030.

0504

0.0

787

0.0

787

0.0

334

0.0

341

0.0

344

0.0

787

0.0787

0.0

335

-0.1

0.05

560.

0556

0.2

398

0.2

398

0.0

378

0.0

384

0.0

389

0.2

398

0.2398

0.0

379

-0.0

10.

0606

0.06

05

0.4

718

0.4

718

0.0

421

0.0

427

0.0

433

0.4

718

0.4

718

0.0

422

-0.0

010.

0611

0.06

10

0.4

972

0.4

972

0.0

426

0.0

432

0.0

437

0.4

972

0.4972

0.0

426

00.

0612

0.06

11

0.5

000

0.5

000

0.0

426

0.0

434

0.0

438

0.5

000

0.5

000

0.0

427

0.00

10.

0612

0.06

11

0.5

028

0.5

028

0.0

427

0.0

435

0.0

438

0.5

028

0.5

028

0.0

427

0.01

0.06

180.

0617

0.5

282

0.5

282

0.0

432

0.0

437

0.0

443

0.5

282

0.5282

0.0

432

0.1

0.06

720.

0671

0.7

602

0.7

603

0.0

479

0.0

487

0.0

491

0.7

603

0.7

603

0.0

479

0.2

0.07

350.

0736

0.9

213

0.9

214

0.0

535

0.0

544

0.0

548

0.9

214

0.9

214

0.0

536

0.4

0.08

740.

0873

0.9

977

0.9

977

0.0

661

0.0

668

0.0

674

0.9

977

0.9

977

0.0

662

0.6

0.10

280.

1026

1.0

000

1.0

000

0.0

805

0.0

813

0.0

818

1.0

000

1.0

000

0.0

805

0.8

0.11

940.

1194

1.0

000

1.0

000

0.0

965

0.0

974

0.0

979

1.0

000

1.0

000

0.0

966

10.

1373

0.13

74

1.0

000

1.0

000

0.1

141

0.1

150

0.1

154

1.0

000

1.0000

0.1

142

1.5

0.18

610.

1862

1.0

000

1.0

000

0.1

642

0.1

649

0.1

653

1.0

000

1.0

000

0.1

643

20.

2387

0.23

88

1.0

000

1.0

000

0.2

210

0.2

214

0.2

217

1.0

000

1.0000

0.2

211

30.

3485

0.34

85

1.0

000

1.0

000

0.3

433

0.3

430

0.3

436

1.0

000

1.0000

0.3

434

50.

5467

0.54

63

1.0

000

1.0

000

0.5

658

0.5

641

0.5

648

1.0

000

1.0000

0.5

659

80.

7397

0.73

95

1.0

000

1.0

000

0.7

825

0.7

796

0.7

800

1.0

000

1.0000

0.7

826

200.

9562

0.95

61

1.0

000

1.0

000

0.9

885

0.9

873

0.9

872

1.0

000

1.0

000

0.9

885

500.

9977

0.99

77

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

27

Tab

le4,

Pan

elB

(T=

10):

Pr(T

(κ−κ

)≤w

),R

an

domx0,κ

=0.

01,µ

=0.

1,σ

=0.

1

Month

lyD

ail

yw

ppedf

pexp

pmix

pinf

ppedf

pexp

pmix

pinf

-50.

0000

0.00

00

0.1

319

0.1

318

0.0

000

0.0

000

0.0

000

0.1

318

0.1

318

0.0

000

-30.

0005

0.00

05

0.2

513

0.2

512

0.0

004

0.0

004

0.0

004

0.2

512

0.2

512

0.0

004

-20.

0026

0.00

26

0.3

274

0.3

274

0.0

023

0.0

023

0.0

024

0.3

274

0.3

274

0.0

023

-1.5

0.00

760.

0060

0.3

687

0.3

687

0.0

054

0.0

055

0.0

054

0.3

687

0.3687

0.0

054

-10.

0127

0.01

29

0.4

116

0.4

115

0.0

118

0.0

120

0.0

118

0.4

115

0.4

115

0.0

119

-0.8

0.01

680.

0172

0.4

290

0.4

290

0.0

159

0.0

161

0.0

158

0.4

290

0.4290

0.0

160

-0.6

0.02

230.

0226

0.4

467

0.4

466

0.0

211

0.0

213

0.0

210

0.4

466

0.4466

0.0

212

-0.4

0.02

900.

0292

0.4

644

0.4

644

0.0

276

0.0

271

0.0

275

0.4

644

0.4644

0.0

277

-0.2

0.03

710.

0373

0.4

822

0.4

822

0.0

355

0.0

358

0.0

353

0.4

822

0.4822

0.0

357

-0.1

0.04

170.

0419

0.4

911

0.4

911

0.0

401

0.0

403

0.0

398

0.4

911

0.4911

0.0

402

-0.0

10.

0462

0.04

65

0.4

991

0.4

991

0.0

445

0.0

335

0.0

443

0.4

991

0.4

991

0.0

447

-0.0

010.

0467

0.04

70

0.4

999

0.4

999

0.0

450

0.0

450

0.0

447

0.4

999

0.4999

0.0

452

00.

0467

0.04

70

0.5

000

0.5

000

0.0

450

0.0

341

0.0

448

0.5

000

0.5

000

0.0

452

0.00

10.

0468

0.04

71

0.5

001

0.5

001

0.0

451

0.0

451

0.0

448

0.5

001

0.5

001

0.0

453

0.01

0.04

730.

0475

0.5

009

0.5

009

0.0

456

0.0

455

0.0

453

0.5

009

0.5009

0.0

457

0.1

0.05

220.

0525

0.5

089

0.5

089

0.0

504

0.0

411

0.0

501

0.5

089

0.5

089

0.0

506

0.2

0.05

800.

0584

0.5

178

0.5

178

0.0

562

0.0

524

0.0

559

0.5

178

0.5

178

0.0

564

0.4

0.07

100.

0712

0.5

356

0.5

356

0.0

691

0.0

799

0.0

689

0.5

356

0.5

356

0.0

694

0.6

0.08

570.

0859

0.5

533

0.5

534

0.0

837

0.0

840

0.0

834

0.5

534

0.5

534

0.0

840

0.8

0.10

190.

1022

0.5

710

0.5

710

0.0

999

0.1

003

0.0

994

0.5

710

0.5

710

0.1

002

10.

1196

0.12

00

0.5

884

0.5

885

0.1

176

0.1

180

0.1

172

0.5

885

0.5885

0.1

180

1.5

0.16

970.

1704

0.6

313

0.6

313

0.1

679

0.1

683

0.1

674

0.6

313

0.6

313

0.1

684

20.

2260

0.22

67

0.6

726

0.6

726

0.2

248

0.2

251

0.2

244

0.6

726

0.6726

0.2

253

30.

3466

0.34

68

0.7

487

0.7

488

0.3

468

0.3

470

0.3

459

0.7

488

0.7488

0.3

473

50.

5649

0.56

44

0.8

681

0.8

682

0.5

678

0.5

677

0.5

670

0.8

682

0.8682

0.5

683

80.

7778

0.77

74

0.9

631

0.9

632

0.7

833

0.7

827

0.7

818

0.9

632

0.9632

0.7

835

200.

9860

0.98

59

1.0

000

1.0

000

0.9

885

0.9

883

0.9

882

1.0

000

1.0

000

0.9

885

501.

0000

1.00

00

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

100

1.00

001.

0000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0

000

1.0000

1.0

000

28

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