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. 2021 Jun 23;9:e11651. doi: 10.7717/peerj.11651

Simultaneous confidence intervals for all pairwise differences between the coefficients of variation of rainfall series in Thailand

Noppadon Yosboonruang 1, Sa-Aat Niwitpong 1, Suparat Niwitpong 1,
Editor: María Ángeles Esteban
PMCID: PMC8234927  PMID: 34221731

Abstract

The delta-lognormal distribution is a combination of binomial and lognormal distributions, and so rainfall series that include zero and positive values conform to this distribution. The coefficient of variation is a good tool for measuring the dispersion of rainfall. Statistical estimation can be used not only to illustrate the dispersion of rainfall but also to describe the differences between rainfall dispersions from several areas simultaneously. Therefore, the purpose of this study is to construct simultaneous confidence intervals for all pairwise differences between the coefficients of variation of delta-lognormal distributions using three methods: fiducial generalized confidence interval, Bayesian, and the method of variance estimates recovery. Their performances were gauged by measuring their coverage probabilities together with their expected lengths via Monte Carlo simulation. The results indicate that the Bayesian credible interval using the Jeffreys’ rule prior outperformed the others in virtually all cases. Rainfall series from five regions in Thailand were used to demonstrate the efficacies of the proposed methods.

Keywords: Bayesian, Coefficient of variation, Fiducial generalized confidence interval, Rainfall, Delta-lognormal distribution

Introduction

Thailand is located in Southeast Asia and is classed as a tropical area. It is influenced by both the southwest and northeast monsoons. The southwest monsoon crosses Thailand between mid-May to mid-October (the rainy season) and brings moist air from the Indian Ocean that causes clouds and heavy rain. The northeast monsoon crosses Thailand from mid-October to mid-February (the winter season) causing cold and dry weather. Moreover, the South receives additional heavy rainfall due to moisture coming in from the Gulf of Thailand. The season changes from mid-February to mid-May (the summer season) due to uncertainty in the weather and is influenced by tropical cyclones in the South China Sea, and thus, the weather is generally hot and dry but often with heavy rain and thunderstorms (Thai Meteorological Department, 2015). Thailand often endures flooding due to thunderstorms, which can take lives and damage property, especially on farms due to Thailand being an agricultural country. Thailand is divided into five regions according to its climate pattern and meteorological conditions (Table 1) (Thai Meteorological Department, 2015). Therefore, it is important to investigate rainfall dispersion in each area to gain preliminary information for formulating policies to mitigate such incidents.

Table 1. The provinces of each regions in Thailand.

Regions Provinces
Northern Chiang Rai, Mae Hong Son, Chiang Mai, Phayao, Lamphun, Lampang, Phrae, Nan,
Uttaradit, Phitsanulok, Sukhothai, Tak, Phichit, Kamphaeng Phet, Phetchabun
Northeastern Nong Khai, Bueng Kan, Loei, Udon Thani,Nong Bua Lam Phu, Nakhon Phanom,
Sakon Nakhon, Mukdahan, Khon Kaen, Kalasin, Maha Sarakham, Roi Et,
Chaiyaphum, Yasothon, Amnat Charoen, Ubon Ratchathani, Sri Sa Ket,
Nakhon Ratchasima, Buri Ram, Surin
Central Nakhon Sawan, Uthai Thani, Chai Nat, Sing Buri, Lop Buri, Ang Thong, Sara buri,
Suphan Buri, Ayutthaya, Pathum Thani, Kanchanaburi, Ratchaburi, Nakhon Pathom,
Nonthaburi, Bangkok Metropolis, Samut Prakan, Samut Sakhon, Samut Songkhram
Eastern Nakhon Nayok, Prachin Buri, Sra Kaeo, Chachoeng Sao, Chon Buri, Rayong,
Chanthaburi, Trat
Southern Phetchaburi, Prachuap Khiri Khan, Chumphon, Surat Thani, Nakhon Si Thammarat,
Phatthalung, Songkhla, Pattani, Yala, Narathiwat, Ranong, Phang Nga, Krabi, Phuket
Trang, Satun

There have been numerous studies on rainfall series that have used the delta-lognormal distribution. Fukuchi (1988) derived the distribution of correlation coefficients of rainfall rates from two areas as bivariate lognormal (delta-lognormal). Kedem (1990) showed that the average rain rate over an area follows a delta-lognormal distribution. Shimizu (1993) and Kong et al. (2012) presented the maximum likelihood estimation of the parameters of rainfall series containing zeros that followed a bivariate lognormal distribution. Moreover, examples of rainfall series that conform to a delta-lognormal distribution can be founded in various studies by Maneerat, Niwitpong & Niwitpong (2019a); Maneerat, Niwitpong & Niwitpong (2019b); Maneerat, Niwitpong & Niwitpong (2020a); Maneerat, Niwitpong & Niwitpong (2020b); Yosboonruang, Niwitpong & Niwitpong (2019b); Yosboonruang, Niwitpong & Niwitpong (2020), and Yosboonruang & Niwitpong (2020). In addition, a delta-lognormal distribution has been applied in other fields, such as Ingram Jr. et al. (2010); Owen & DeRouen (1980); Fletcher (2008); Wu & Hsieh (2014), and Zhou & Tu (2000). Constructing the confidence intervals for several parameters of a delta-lognormal distribution used in statistical inference has been of interest to many researchers. Confidence intervals for the delta-lognormal mean were proposed by Owen & DeRouen (1980); Kvanli, Shen & Deng (1998); Zhou & Tu (2000); Tian (2005); Chen & Zhou (2006); Tian & Wu (2006); Fletcher (2008); Li, Zhou & Tian (2013); Wu & Hsieh (2014); Hasan & Krishnamoorthy (2018), and Maneerat, Niwitpong & Niwitpong (2018); Maneerat, Niwitpong & Niwitpong (2019a); Maneerat, Niwitpong & Niwitpong (2019b). Furthermore, the confidence intervals for variance and the coefficient of variation (CV) of a delta-lognormal distribution were presented by Buntao & Niwitpong (2012); Buntao & Niwitpong (2013); Yosboonruang, Niwitpong & Niwitpong (2018); Yosboonruang, Niwitpong & Niwitpong (2019a); Yosboonruang, Niwitpong & Niwitpong (2019b); Yosboonruang, Niwitpong & Niwitpong (2020); Yosboonruang & Niwitpong (2020), and Maneerat, Niwitpong & Niwitpong (2020a); Maneerat, Niwitpong & Niwitpong (2020b).

For statistical inference, the CV, the ratio of the standard deviation to the mean, is a good tool for investigating rainfall dispersion. The advantage of using the CV is that it is unitless and thus, is useful for measuring dispersion in data series with different units or drastically different means. Focusing on inferential statistics, the confidence intervals and functions of the CV for several distributions have been presented. Wong & Wu (2002) suggested a small-sample asymptotic method for constructing the confidence intervals for the CV of normal and non-normal distributions when the sample size is very small. Mahmoudvand & Hassani (2009) proposed two new methods for constructing the confidence intervals for the CV of a normal distribution and compared them with Miller’s, Makay’s, Vangel’s, and Sharma-Krishna’s methods; they found that their proposed methods are more appropriate than the others. Buntao & Niwitpong (2012) proposed the generalized pivotal approach (GPA) and a closed-form method for variance estimation for the difference between the CVs of lognormal and delta-lognormal distributions; their results show that the GPA is the most suitable. After that, they constructed the confidence intervals for the ratio of the CVs of delta-lognormal distributions using GPA and the method of variance estimates recovery (MOVER) (Buntao & Niwitpong, 2013); their results were similar to the confidence intervals for the difference between the CVs. Wongkhao, Niwitpong & Niwitpong (2015) presented the generalized confidence interval (GCI) and MOVER to construct the confidence intervals for the ratio of CVs of normal distributions and then compared their methods with the Verrill and Johnson and bootstrapping methods; they found that GCI and MOVER performed better than the others. Sangnawakij & Niwitpong (2017a) proposed MOVER, GCI, and the asymptotic confidence interval (ACI) for constructing the confidence interval for the CV and difference between the CVs of two-parameter exponential distributions; their results show that GCI was appropriate for a single CV and ACI worked well for the difference between the CVs. In addition, confidence intervals were extended by Sangnawakij & Niwitpong (2017b) based on the score and Wald intervals for the difference between and ratio of CVs of two gamma distributions; their proposed methods performed well in a comparative study. Recently, Yosboonruang, Niwitpong & Niwitpong (2018) proposed GCI and a modified Fletcher method to construct the confidence intervals for the CV of a delta-lognormal distribution and found that GCI was the best. Afterward, they introduced the fiducial GCI (FGCI) and MOVER to construct the confidence intervals for the CV of a delta-lognormal distribution (Yosboonruang, Niwitpong & Niwitpong, 2019a). Moreover, they compared the confidence intervals based on FGCI and a Bayesian method for the CV of a delta-lognormal distribution (Yosboonruang, Niwitpong & Niwitpong, 2019b); their results indicate that the Bayesian method outperformed FGCI. Yosboonruang & Niwitpong (2020) constructed confidence intervals using GCI and MOVER based on variance stabilizing transformation, the Wilson score, and Jeffreys’ method for the ratio of the CVs of delta-lognormal distributions; their results show that GCI was the most suitable. Yosboonruang, Niwitpong & Niwitpong (2020) presented FGCI and a Bayesian method to construct the confidence interval for the difference of CVs of delta-lognormal distributions; they concluded that the Bayesian method was the most appropriate.

Since dispersion in the precipitation series for different areas can be the same or different, simultaneous estimation of this for multiple areas has been investigated using various distributions and parameters. Mandel & Betensky (2008) introduced an algorithm for simultaneous confidence interval (SCI) construction and then compared bootstrapped and normal-based SCIs in which the limits of the bootstrap intervals were smaller than the normal-based intervals. Donner & Zou (2011) used a two-step MOVER approach for constructing SCIs for multiple contrasts of binomial proportions; their proposed method was reasonable for small-to-moderate sample sizes. Abdel-Karim (2015) considered three methods: FGCI-MOVER, MOVER-MOVER, and simultaneous FGCI to construct SCIs for the ratio of means of lognormal distributions; they reported that the MOVER-MOVER method outperformed the others. Li, Song & Shi (2015) suggested parametric bootstrapping to construct SCIs for all pairwise differences between the means of two-parameter exponential distributions. Thangjai, Niwitpong & Niwitpong (2019) presented three methods: MOVER, a computational approach, and FGCI to construct SCIs for all of the differences between the CVs of lognormal distributions; their results show that MOVER was the best and the computational approach performed similarly to MOVER when the sample size was large. In addition, Thangjai & Niwitpong (2020) used parametric bootstrapping, GCI, and MOVER for SCI construction for all of the differences between CVs in two-parameter exponential distributions; their results indicate that GCI was the most appropriate in most cases, while MOVER was the best for large sample sizes.

As mentioned above, rainfall series data follow a delta-lognormal distribution. Since our focus is on comparing the dispersion of rainfall from five regions in Thailand, the pairwise differences between the CVs of their rainfall data distributions are an interesting topic to study. Although there have been numerous methods published for constructing SCIs for the differences between the parameters of several types of distributions, constructing SCIs for all of the pairwise differences between the CVs of delta-lognormal distributions has not yet been reported. GCI is a general method that is often used to construct confidence intervals, but FGCI is stronger than GCI since it provides asymptotically correct frequentist coverage (Hannig, Abdel-Karim & Iyer, 2006). Moreover, previous researchers have reported that MOVER is an appropriate method for constructing the SCIs for various parameters of several types of distributions. Therefore, one of ours aims was to construct SCIs for this scenario based on FGCI and compare them with ones based on MOVER and Bayesian methodology. The coverage probability, the probability that the confidence interval of the estimate covers the value of the parameter, together with the expected length were used to estimate the performance of the confidence intervals.

Methods

Let Xi=Xi1,Xi2,,Xini, i = 1, 2, …, k be a random sample from k independent delta-lognormal distributions, denoted by XijΔμi,σi2,δi0, where δi0=PXij=0. Since this distribution contains zero and positive values, then the zero values follow a binomial distribution and the positive values a lognormal distribution denoted by Xij=0Binni,δi0 and Yij= lnXijNμi,σi2, respectively. Moreover, let ni0 and ni1 be the numbers of zero and positive values, respectively, where ni=ni0+ni1. The distribution function of a delta-lognormal distribution is given by

fxij;μi,σi2,δi0=δi0;xij=0δi112πσi1xij explnxijμi22σi2;xij>0, (1)

where δi1=1δi0. Following Aitchison (1955), the respective population mean and variance of Xi are

EXi=μXi=δi1 expμi+σi22 (2)

and

VarXi=σXi2=δi1 exp2μi+σi2expσi2δi1. (3)

Following this, the CV of Xi can be expressed as

CVXi=νi= expσi2δi1δi1. (4)

Since we are interested in constructing the SCIs for all pairwise differences between the CVs, then

νil=νiνl= expσi2δi1δi1 expσl2δl1δl1, (5)

where il =1 , 2, …, k and i ≠ l. The maximum likelihood estimators of δi1 and μi are δ ˆi1=ni1ni and μ ˆi=j=1ni1 lnxijni1, respectively. Furthermore, the unbiased estimator for σi2 is σ ˆi2=j=1ni1lnxijμ ˆi2ni11.

Assume that δ ˆi1 and σ ˆi2 are independent, then the maximum likelihood estimator of νi can be defined as

ν ˆi= expσ ˆi2δ ˆi1δ ˆi1. (6)

Similarly,

ν ˆil=ν ˆiν ˆl= expσ ˆi2δ ˆi1δ ˆi1 expσ ˆl2δ ˆl1δ ˆl1, (7)

where il =1 , 2, …, k and i ≠ l.

According to Yosboonruang, Niwitpong & Niwitpong (2020), the estimated variance of ν ˆiν ˆl can be expressed as

Var ˆν ˆiν ˆl=lnδ ˆi1+ln expσ ˆi2δ ˆi1δ ˆi1+1 expσ ˆi2δ ˆi1δ ˆi1+122ni expσ ˆi2δ ˆi1δ ˆi1+lnδ ˆl1+ln expσ ˆl2δ ˆl1δ ˆl1+1 expσ ˆl2δ ˆl1δ ˆl1+122nl expσ ˆl2δ ˆl1δ ˆl1, (8)

where il =1 , 2, …, k and i ≠ l.

The simultaneous FGCIs

To construct the simultaneous FGCIs, a fiducial generalized pivotal quantity (FGPQ), which is a subclass of the generalized pivotal quantity (GPQ) (Hannig, Iyer & Patterson, 2006), is presented as follows.

Definition 1

Let Xi=Xi1,Xi2,,Xini,i=1,2,,k be a random sample from k independent delta-lognormal distributions with parameters of interest (σi2,δi1) and nuisance parameter μi. Let xi=xi1,xi2,,xini,i=1,2,,k be an observed value of Xi. GPQ RXi;xi,μi,σi2,δi1 is called an FGPQ if it corresponds with the following two conditions (Weerahandi, 1993; Hannig, Iyer & Patterson, 2006): 1. For a given xi, the conditional distribution of RXi;xi,μi,σi2,δi1 is free of μi. 2. The observed value of RXi;xi,μi,σi2,δi1 at Xi=xi,rxi;xi,μi,σi2,δi1 is the parameter of interest.

The FGPQs for σi2 and δi1 can be constructed by applying Definition 1. According to Hannig, Iyer & Patterson (2006) and Li, Zhou & Tian (2013), the respective FGPQs for δi1 and σi2 are

Rδi112Betani1,ni0+1+12Betani1+1,ni0 (9)

and

Rσi2=ni11σ ˆi2Ui, (10)

where Uiχni112. Following this, the FGPQ for νi is simply

Rνi= expRσi2Rδi1Rδi1. (11)

Hence, the FGPQ for the differences between two independent CVs can be expressed as

Rνil=RνiRνl= expRσi2Rδi1Rδi1 expRσl2Rδl1Rδl1, (12)

where i, l =1 , 2, …, k and i ≠ l.

Therefore, the 1001α% two-sided SCI for νi − νl based on the FGCI method can be written as Lil ⩽ νil ⩽ Uil, where Lil and Uil are the α∕2-th and 1α2-th quantiles of Rνil, respectively.

Theorem 1

Let Xi=Xi1,Xi2,,Xini,i=1,2,,k be a random sample from k independent delta-lognormal distributions with mean μi, variance σi2, and probability of zero values δi0. Let νi=expσi2δi1δi1 and νl=expσl2δl1δl1 for il =1 , 2, …, k and i ≠ l be the CV of Xi and Xl, respectively. Furthermore, let ν ˆi and ν ˆl be the estimators of νi and νl, respectively. The estimator for the variance of the difference between νi and νl is Var ˆν ˆiν ˆl. Let ni be the sample size of the i-th random sample and n = n1 + n2 + … + nk. Assume that nin → ri as n → ∞ where 0 < ri < 1. Therefore,

PRνilα2RνilRνil1α2,il1α. (13)

Proof

Since

PRνilα2RνilRνil1α2,il=PLilνiνlUil,il,

where Lil,Uil=ν ˆiν ˆl±d1αVar ˆν ˆiν ˆl and d1−α denotes the 1α-th quantile of Rνil. Thus,

PLilνiνlUil,il=Pmaxilν ˆiν ˆlνiνlVar ˆν ˆiν ˆld1α=PDnd1α.

Accordingly,

PLilνiνlUil,il1α.

This implies that

PRνilα2RνilRνil1α2,il1α.

The Bayesian method

According to the distributions of Xi for i = 1, 2, …, k with the unknown parameters μi,σi2, and δi0, where δi0=1δi1, the joint likelihood function of k independent delta-lognormal distributions is

Lμi,σi2,δi1xiji=1k1δi1ni0δi1ni1σi2ni12 exp12σi2j=1ni1lnxijμi2. (14)

By applying the second-order partial derivative of the log-likelihood function with respect to the unknown parameters, the Fisher information matrix of the unknown parameters can be written as

Iμi,σi2,δi1=diagn11δ11δ11n1δ11σ12n1δ112σ122nk1δk1δk1nkδk1σk2nkδk12σk22. (15)

In this paper, we constructed both of equal-tailed SCIs based on simulation data and simultaneous credible intervals based on information from a simulation study of their prior distributions using two forms of Bayesian prior; the suitability of the Jeffreys’ rule and uniform priors was determined by considering the values of a random variable of their posterior distributions that correspond to those for a delta-lognormal distribution. See also, Yosboonruang, Niwitpong & Niwitpong (2019b) and Yosboonruang, Niwitpong & Niwitpong (2020).

The Jeffreys’ rule prior

The Jeffreys’ rule prior is obtained from the square root of the determinant of the Fisher information matrix (Jeffreys, 1946). It is well known that a delta-lognormal distribution comprises lognormal and binomial distributions. From the CVs in Eq. (4), the parameters of interest are σi2 and δi1, and the Jeffreys’ rule priors for these parameters are pσi2σi3 and pδi11δi112δi112, respectively. Assuming that σi2 and δi1 are independent, the prior distribution for a delta-lognormal distribution can be defined as pσi2,δi1σi31δi112δi112. By combining the likelihood function and the prior distribution of a delta-lognormal distribution, the joint posterior density function can be written as

pσi2,δi1xij=i=1k1Betani0+12,ni1+321δi1ni0+121δi1ni1+321×12πσini1 exp12σi2ni1μiμ ˆi2ni1σ ˆi22ni12Γni12σi2ni121× expni1σ ˆi22σi2, (16)

where μ ˆi=j=1ni1 lnxijni1, and σ ˆi2=j=1ni1lnxijμ ˆi2ni11.

By integrating Eq. (16), the respective posterior distributions of σi2 and δi1 are derived as

pσi2xiji=1kni1σ ˆi22ni12Γni12σi2ni121 expni1σ ˆi22σi2, (17)

and

pδi1xiji=1k1Betani0+12,ni1+321δi1ni0+121δi1ni1+321. (18)

It should be noted that pσi2xij follows an inverse gamma distribution and pδi1xij follows a beta distribution, denoted by σi2xijInvGammani12,ni1σ ˆi22 and δi1xijBetani0+12, ni1+32, respectively. Consequently, σi2xij and δi1xij can be substituted into (5) to construct the equal-tailed SCI and the simultaneous credible interval, respectively.

The uniform prior

Since the uniform prior has a constant function for the prior probability (Stone, 2013), then the uniform priors of σi2 and δi1 are 1, denoted by pσi21 and pδi11, respectively. Afterward, the uniform prior for a delta-lognormal distribution becomes pσi2,δi11. Similar to Eq. (16), the joint posterior density function is obtained by combining pσi2,δi1 with the likelihood function from Eq. (14). Subsequently, we obtain the posterior of σi2 and δi1 by integrating the joint posterior density function with respect to the others. Thus, the posterior distribution is σi2xijInvGammani122,ni12σ ˆi22 for σi2 and δi1xijBetani0+1,ni1+1 for δi1.

Therefore, the 1001α% equal-tailed SCI and simultaneous credible interval for νil based on the Bayesian method are Lil ≤ νil ≤ Uil, where Lil and Uil are the lower and upper bounds of the intervals, respectively.

Theorem 2

Let Xi=Xi1,Xi2,,XiniΔμi,σi2,δi1, where i = 1, 2, …, k and δi0=1δi1, with sample sizes n1n2, …, nk and n = n1 + n2 + … + nk. Let ri = nin as n → ∞, where 0 < ri < 1. For il =1 , 2, …, k and i ≠ l, let νi=expσi2δi1δi1 and νl=expσl2δl1δl1 be the CVs of Xi and Xl, respectively. Let ν ˆi and ν ˆl be the estimators of νi and νl, respectively. An estimator for the variance of the difference between νi and νl is Var ˆν ˆiν ˆl. Let pσi2,δi1 and pσi2,δi1xij be the prior distribution and the joint posterior density function for delta-lognormal distribution, respectively. Therefore,

PLilνilUil,il1α. (19)
Proof

The proof is similar to Theorem 1.

Algorithm 1: For the FGCI and Bayesian methods

  • Step 1.

    Generate random samples Xi, i = 1, 2, …, k, with sample sizes n1n2, …, nk and calculate δ ˆi1 and σ ˆi2.

  • Step 2.

    Generate Uiχni112,Betani1,ni1+1,Betani1+1,ni1,Betani0+12,ni1+32,Betani0+1,ni1+1,InvGammani12,ni1σ ˆi22,andInvGammani122,ni12σ ˆi22.

  • Step 3.

    Calculate Rδi1,Rσi2,Rνi,Rνl,νi,andνl.

  • Step 4.

    Repeat Steps 2–3 5,000 times.

  • Step 5.

    Compute the 95% SCIs for νil.

  • Step 6.

    Repeat Steps 1–5 15,000 times.

MOVER

The concept of MOVER proposed by Donner & Zou (2012) can be applied to construct the 1001α% two-sided confidence interval of νi − νl for il =1 , 2, …, k and i ≠ l, for which Lil ≤ νil ≤ Uil where Lil and Uil denote the lower and upper limits of the confidence interval, respectively, expressed as

Lil=ν ˆiν ˆlν ˆili2+ulν ˆl2 (20)

and

Uil=ν ˆiν ˆl+uiν ˆi2+ν ˆlll2, (21)

where il =1 , 2, …, k and i ≠ l. From (4), the parameters of interest are δi1 and σi2, and so the confidence intervals for these parameters can be constructed.

Since the unbiased estimator of σi2 is given by σ ˆi2=j=1ni1lnxijμ ˆi2ni11, for i = 1, 2, …, k and where ni11σ ˆi2σ2χni112. Consequently, the respective lower and upper bounds for σi2 are defined as

lσi2=ni11σ ˆi2χ1α2,ni112 (22)

and

uσi2=ni11σ ˆi2χα2,ni112. (23)

The score method proposed by Wilson (1927) is used to construct the confidence limits for δi1. According to Brown, Cai & DasGupta (2001) and Donner & Zou (2011), the respective lower and upper limits of δi1 are given by

lδi1=ni1+Ziα222ni+Ziα22Ziα2ni0ni1ni+Ziα224ni+Ziα22 (24)

and

uδi1=ni1+Ziα222ni+Ziα22+Ziα2ni0ni1ni+Ziα224ni+Ziα22, (25)

where Zii = 1, 2, …, k follow a standard normal distribution. This approach is similar to constructing the confidence limits for σl2 and δl1.

Therefore, the 1001α% two-sided SCIs for νi − νl based on the MOVER method are

SCIil=Lil,Uil, (26)

where il =1 , 2, …, k and i ≠ l.

Theorem 3

Let Xi=Xi1,Xi2,,Xini,i=1,2,,k, be random samples from k independent delta-lognormal distributions with mean μi, variance σi2, and probability of zero values δi0. Furthermore, let the sample size of the i-th random sample be ni, where n = n1 + n2 + … + nk and ri = nin as n → ∞, for which 0 < ri < 1. Let νi=expσi2δi1δi1 and νl=expσl2δl1δl1, for il =1 , 2, …, k and i ≠ l, be the CVs of Xi and Xl, respectively. In addition, let ν ˆi and ν ˆl be the estimators of νi and νl, respectively. Let Lil=ν ˆiν ˆlν ˆili2+ulν ˆl2 and Uil=ν ˆiν ˆl+uiν ˆi2+ν ˆlll2, where il =1 , 2, …, k and i ≠ l, be the respective lower and upper limits of the confidence interval for νil = νi − νl. Therefore,

PLilνilUil,il1α. (27)
Proof

Suppose that the respective lower and upper limits of the confidence interval for νil = νi − νl are

Lil=ν ˆiν ˆlν ˆili2+ulν ˆl2=ν ˆilν ˆili2+ulν ˆl2

and

Uil=ν ˆiν ˆl+uiν ˆi2+ν ˆlll2=ν ˆil+uiν ˆi2+ν ˆlll2,

where i, l =1 , 2, …, k and i ≠ l. Thus, the respective estimators of variance for ν ˆi and ν ˆl at νi = li and νl = ll are

Var ˆν ˆi=ν ˆili2zα22

and

Var ˆν ˆl=ν ˆlll2zα22,

where zα∕2 is the α∕2-th quantile of the standard normal distribution. Similarly, the respective estimators of variance for ν ˆi and ν ˆl at νi = ui and νl = ul are

Var ˆν ˆi=uiν ˆi2zα22

and

Var ˆν ˆl=ulν ˆl2zα22.

Hence, the respective lower and upper limits can be expressed as

Lil=ν ˆilzα2ν ˆili2zα22+ulν ˆl2zα22=ν ˆilzα2Var ˆν ˆi+Var ˆν ˆl

and

Uil=ν ˆil+zα2uiνi ˆ2zα22+ν ˆlll2zα22=ν ˆil+zα2Var ˆν ˆi+Var ˆν ˆl.

Therefore,

PLilνilUil=Pνilν ˆil±zα2Var ˆν ˆi+Var ˆν ˆl,il=Pmaxilν ˆilνilVar ˆν ˆi+Var ˆν ˆlzα2=PDnzα2.

Suppose that ninri0,1 as n → ∞, i = 1, 2, …, k where n = n1 + n2 + … + nk. From the central limit theorem, nν ˆiνidZi,i=1,2,,k, where ZiiidN0,σi2ri, while from Slutsky’s theorem, DnD, where D=maxilZiZlσi2ri+σl2rl.

Following Skorokhod’s theorem, let Yn and Y be random variables from the common probability space with distributions Dn and D′, respectively. Thus, Yn converges to Y almost surely, denoted by Yna.s.Y, and Dn converges to D′ almost surely, denoted by Dna.s.D. Assume that Zi and Zi are independent and identically distributed random variables. Thus, TX,X,μ,σ2D, where D=maxilZiZlσi2ri+σl2rl, for il =1,2, …, k, and i ≠ l. Since the limiting distribution of TX,X,μ,σ2 is continuous and zα2Xqα2, where qα∕2 is the α∕2-th quantile of the distribution of D, we can obtain

PDnzα2PDqα2=PDqα2=1α,asn.Therefore,
Pνilν ˆil±zα2Var ˆν ˆi+Var ˆν ˆl,il1α,

which implies that

PLilνilUil,il1α.

Algorithm 2: For MOVER

  • Step 1.

    Generate random samples Xi, i = 1, 2, …, k with sample size n1n2, …, nk and calculate δ ˆi1 and σ ˆi2.

  • Step 2.

    Generate χ1α2,ni112,χα2,ni112,andZiN0,1.

  • Step 3.

    Calculate lσi2,lσl2,uσi2,uσl2,lδi1,lδl1,uδi1,anduδl1.

  • Step 4.

    Repeat Steps 2–3 5,000 times.

  • Step 5.

    Compute the 95% SCIs for νil.

  • Step 6.

    Repeat Steps 1–5 15,000 times.

Simulation Results

Here, the performances of the proposed methods via Monte Carlo simulation with the R statistical program are presented. The best method attains a coverage probability equal to or greater than the nominal simultaneous confidence level of 0.95 together with the shortest expected length. The simulations were conducted with 15,000 iterations for each combination of parameters. Furthermore, 5,000 replications for the FGCI and Bayesian methods for each case of parameter combination were carried out. Sample sizes were set as 25, 50, and 100; δi1=0.2,0.5,0.8; and σi2=0.5,1.0,2.0.

The results in Tables 24 and Figs. 13 show that the coverage probabilities of FGCI and the equal-tailed Bayesian using Jeffreys’ rule prior were close to or greater than the nominal confidence level for almost all k values. Similarly, the coverage probabilities of the equal-tailed Bayesian using the uniform prior, the Bayesian credible intervals using Jeffreys’ rule and uniform priors, and MOVER were close to or greater than the nominal confidence level for all cases. For most cases, the Bayesian credible interval using Jeffreys’ rule prior attained the shortest expected length, except for ni = 50; δi1=0.5,0.8; and σi2=0.5,1.0, for which the expected lengths of FGCI were the shortest.

Table 2. The coverage probabilities and expected lengths for the 95% SCIs and credible intervals for all pairwise differences between the CVs of delta-lognormal distributions for k = 3.

n1:n2:n3 δ11:δ21:δ31 σ12:σ22:σ32 Coverage probabilities (Expected lengths)
FGCI B.Jrule-E B.Uni-E B.Jrule-C B.Uni-C MOVER
25:25:25 0.5:0.5:0.5 0.5:0.5:0.5 0.9642 0.9788 0.9842 0.9956 0.9980 0.9986
(2.1698) (2.1537) (2.5030) (2.0848) (2.4026) (3.4408)
1.0:1.0:1.0 0.9573 0.9605 0.9718 0.9957 0.9984 0.9941
(6.8818) (6.2442) (7.9188) (5.7177) (7.1021) (9.6034)
2.0:2.0:2.0 0.9516 0.9465 0.9631 0.9978 0.9991 0.9838
(68.0142) (53.9752) (88.1169) (37.9389) (55.1280) (85.1444)
0.5:1.0:2.0 0.9557 0.9540 0.9678 0.9708 0.9820 0.9878
(24.7584) (20.5209) (31.5389) (13.1644) (17.7557) (31.4612)
0.8:0.8:0.8 0.5:0.5:0.5 0.9542 0.9632 0.9725 0.9834 0.9894 0.9954
(1.2558) (1.2613) (1.3684) (1.2412) (1.3444) (1.8437)
1.0:1.0:1.0 0.9533 0.9526 0.9636 0.9857 0.9915 0.9868
(3.2363) (3.1117) (3.4638) (2.9940) (3.3202) (4.2113)
2.0:2.0:2.0 0.9499 0.9458 0.9570 0.9930 0.9963 0.9756
(16.6440) (15.4579) (18.2078) (13.7933) (16.0213) (20.0584)
0.5:1.0:2.0 0.9513 0.9496 0.9598 0.9659 0.9750 0.9797
(7.3206) (6.8777) (7.9629) (5.5921) (6.3072) (8.7800)
50:50:50 0.2:0.2:0.2 0.5:0.5:0.5 0.9692 0.9869 0.9906 0.9991 0.9997 0.9994
(4.3383) (4.1487) (5.2706) (3.9321) (4.8731) (7.2083)
1.0:1.0:1.0 0.9593 0.9672 0.9778 0.9988 0.9996 0.9965
(17.7495) (14.6338) (23.0519) (12.3745) (17.8689) (25.8720)
2.0:2.0:2.0 0.9525 0.9489 0.9668 0.9984 0.9996 0.9882
(813.5319) (360.7209) (3.75E+03) (130.6376) (338.9741) (1.00E+03)
0.5:1.0:2.0 0.9560 0.9567 0.9719 0.9742 0.9846 0.9910
(131.2015) (80.4363) (238.4643) (36.1680) (67.2572) (169.2385)
0.5:0.5:0.5 0.5:0.5:0.5 0.9609 0.9797 0.9827 0.9904 0.9926 0.9990
(1.2086) (1.2989) (1.3657) (1.2849) (1.3499) (1.9562)
1.0:1.0:1.0 0.9536 0.9613 0.9678 0.9870 0.9907 0.9934
(3.0015) (2.9770) (3.1957) (2.8997) (3.1064) (4.2360)
2.0:2.0:2.0 0.9496 0.9488 0.9579 0.9910 0.9942 0.9831
(13.0784) (12.5308) (13.8315) (11.6629) (12.8048) (16.6567)
0.5:1.0:2.0 0.9510 0.9541 0.9619 0.9644 0.9712 0.9872
(6.2117) (6.0214) (6.5869) (5.1934) (5.6079) (7.9402)
0.8:0.8:0.8 0.5:0.5:0.5 0.9545 0.9652 0.9702 0.9764 0.9804 0.9960
(0.7563) (0.7866) (0.8128) (0.7810) (0.8069) (1.1146)
1.0:1.0:1.0 0.9512 0.9530 0.9582 0.9744 0.9788 0.9870
(1.7222) (1.7159) (1.7838) (1.6925) (1.7587) (2.2244)
2.0:2.0:2.0 0.9489 0.9476 0.9528 0.9832 0.9863 0.9746
(6.2458) (6.1250) (6.4310) (5.9199) (6.2078) (7.4204)
0.5:1.0:2.0 0.9534 0.9532 0.9592 0.9644 0.9690 0.9816
(3.2059) (3.1646) (3.3108) (2.8957) (3.0156) (3.8254)
100:100:100 0.2:0.2:0.2 0.5:0.5:0.5 0.9655 0.9862 0.9876 0.9955 0.9969 0.9995
(2.1032) (2.2970) (2.4455) (2.2649) (2.4065) (3.5694)
1.0:1.0:1.0 0.9572 0.9696 0.9746 0.9935 0.9959 0.9966
(5.5368) (5.4606) (6.0091) (5.2547) (5.7570) (8.2473)
2.0:2.0:2.0 0.9528 0.9546 0.9629 0.9951 0.9973 0.9891
(28.1449) (26.2788) (30.4653) (23.6063) (27.0268) (37.4768)
0.5:1.0:2.0 0.9541 0.9585 0.9665 0.9672 0.9744 0.9903
(12.6988) (12.0766) (13.7614) (9.9027) (11.0231) (16.9562)
0.5:0.5:0.5 0.5:0.5:0.5 0.9595 0.9793 0.9803 0.9852 0.9866 0.9988
(0.7728) (0.8596) (0.8774) (0.8547) (0.8723) (1.2568)
1.0:1.0:1.0 0.9558 0.9646 0.9673 0.9806 0.9824 0.9949
(1.7356) (1.7761) (1.8252) (1.7576) (1.8058) (2.4523)
2.0:2.0:2.0 0.9501 0.9513 0.9555 0.9803 0.9831 0.9832
(6.1101) (6.0586) (6.2714) (5.9140) (6.1174) (7.6906)
0.5:1.0:2.0 0.9518 0.9565 0.9603 0.9613 0.9653 0.9889
(3.1854) (3.1976) (3.2977) (2.9846) (3.0716) (4.0742)
0.8:0.8:0.8 0.5:0.5:0.5 0.9542 0.9668 0.9691 0.9721 0.9739 0.9966
(0.5013) (0.5298) (0.5376) (0.5273) (0.5350) (0.7395)
1.0:1.0:1.0 0.9495 0.9526 0.9554 0.9654 0.9678 0.9864
(1.0816) (1.0919) (1.1103) (1.0843) (1.1025) (1.3892)
2.0:2.0:2.0 0.9517 0.9516 0.9546 0.9739 0.9756 0.9766
(3.4703) (3.4545) (3.5212) (3.4088) (3.4741) (4.0656)
0.5:1.0:2.0 0.9496 0.9518 0.9552 0.9579 0.9608 0.9814
(1.8867) (1.8883) (1.9231) (1.8062) (1.8377) (2.2430)
25:50:100 0.5:0.5:0.5 0.5:0.5:0.5 0.9614 0.9782 0.9840 0.9829 0.9885 0.9984
(1.4118) (1.4647) (1.6172) (1.4069) (1.5307) (2.2374)
1.0:1.0:1.0 0.9525 0.9572 0.9670 0.9764 0.9838 0.9941
(3.9253) (3.7120) (4.3712) (3.3455) (3.7992) (5.4323)
2.0:2.0:2.0 0.9525 0.9502 0.9609 0.9827 0.9875 0.9826
(27.5125) (23.2226) (33.9099) (16.5621) (20.9132) (34.6995)
0.5:1.0:2.0 0.9551 0.9600 0.9648 0.9793 0.9827 0.9901
(3.8830) (3.8512) (4.0951) (3.6913) (3.9292) (5.2078)
25:50:100 0.8:0.8:0.8 0.5:0.5:0.5 0.9572 0.9679 0.9740 0.9754 0.9825 0.9958
(0.8600) (0.8810) (0.9323) (0.8589) (0.9050) (1.2513)
1.0:1.0:1.0 0.9516 0.9525 0.9596 0.9709 0.9775 0.9869
(2.0776) (2.0320) (2.1907) (1.9232) (2.0528) (2.6582)
2.0:2.0:2.0 0.9513 0.9486 0.9558 0.9776 0.9826 0.9751
(8.8667) (8.4294) (9.4811) (7.3245) (8.0262) (10.4756)
0.5:1.0:2.0 0.9532 0.9545 0.9592 0.9702 0.9735 0.9833
(2.2424) (2.2348) (2.3100) (2.1757) (2.2505) (2.7807)

Notes.

B.Jrule-E, B.Uni-E represented the equal-tailed Bayesian confidence intervals using Jeffreys’ rule and uniform priors, respectively, and B.Jrule-C and B.Uni-C represented the Bayesian credible intervals using Jeffrey’s rule and uniform priors.

Table 4. The coverage probabilities and expected lengths for the 95% SCIs and credible intervals for all pairwise differences between the CVs of delta-lognormal distributions for k = 10.

n1:…:n10 δ11::δ101 σ12::σ102 Coverage probabilities (Expected lengths)
FGCI B.Jrule-E B.Uni-E B.Jrule-C B.Uni-C MOVER
2510 0.510 0.510 0.9644 0.9796 0.9852 0.9958 0.9981 0.9987
(2.1718) (2.1549) (2.5017) (2.0864) (2.4056) (3.4437)
1.010 0.9559 0.9596 0.9717 0.9952 0.9982 0.9935
(6.9095) (6.2680) (7.9343) (5.7342) (7.1201) (9.6381)
2.010 0.9513 0.9466 0.9627 0.9970 0.9990 0.9832
(64.2109) (51.6243) (83.5403) (37.5819) (54.7163) (81.8119)
0.810 0.510 0.9558 0.9645 0.9733 0.9836 0.9899 0.9958
(1.2509) (1.2566) (1.3621) (1.2369) (1.3398) (1.8373)
1.010 0.9518 0.9513 0.9621 0.9855 0.9914 0.9871
(3.2511) (3.1246) (3.4760) (3.0068) (3.3358) (4.2290)
2.010 0.9511 0.9468 0.9581 0.9931 0.9962 0.9759
(16.2516) (15.1258) (17.7445) (13.5223) (15.6914) (19.6085)
5010 0.210 0.510 0.9678 0.9859 0.9892 0.9988 0.9995 0.9993
(4.3466) (4.1581) (5.2771) (3.9368) (4.8806) (7.2207)
1.010 0.9600 0.9680 0.9784 0.9988 0.9997 0.9966
(17.6759) (14.5839) (22.8034) (12.3672) (17.8805) (25.7964)
2.010 0.9525 0.9491 0.9671 0.9988 0.9997 0.9881
(584.809) (314.782) (1958.586) (130.579) (314.105) (825.014)
0.510 0.510 0.9614 0.9800 0.9828 0.9905 0.9927 0.9989
(1.2078) (1.2981) (1.3643) (1.2842) (1.3493) (1.9553)
1.010 0.9543 0.9614 0.9676 0.9874 0.9909 0.9942
(2.9985) (2.9750) (3.1898) (2.8975) (3.1028) (4.2323)
2.010 0.9505 0.9497 0.9577 0.9915 0.9944 0.9834
(13.0586) (12.5061) (13.7967) (11.6493) (12.7980) (16.6309)
0.810 0.510 0.9543 0.9653 0.9699 0.9761 0.9799 0.9960
(0.7572) (0.7873) (0.8131) (0.7817) (0.8075) (1.1153)
1.010 0.9510 0.9530 0.9584 0.9747 0.9791 0.9872
(1.7261) (1.7192) (1.7869) (1.6958) (1.7624) (2.2287)
2.010 0.9500 0.9485 0.9541 0.9835 0.9866 0.9749
(6.2757) (6.1553) (6.4591) (5.9506) (6.2399) (7.4567)
10010 0.210 0.510 0.9658 0.9868 0.9885 0.9957 0.9968 0.9994
(2.1038) (2.2979) (2.4450) (2.2660) (2.4078) (3.5707)
1.010 0.9573 0.9684 0.9738 0.9937 0.9959 0.9968
(5.5609) (5.4793) (6.0256) (5.2730) (5.7794) (8.2780)
2.010 0.9515 0.9523 0.9612 0.9950 0.9972 0.9881
(27.8994) (26.0553) (30.1289) (23.3884) (26.7565) (37.1355)
10010 0.510 0.510 0.9595 0.9799 0.9813 0.9856 0.9869 0.9989
(0.7720) (0.8589) (0.8767) (0.8540) (0.8718) (1.2559)
1.010 0.9536 0.9622 0.9653 0.9784 0.9810 0.9945
(1.7364) (1.7768) (1.8256) (1.7582) (1.8066) (2.4531)
2.010 0.9505 0.9518 0.9557 0.9815 0.9841 0.9838
(6.1121) (6.0620) (6.2702) (5.9173) (6.1188) (7.6931)
0.810 0.510 0.9541 0.9668 0.9689 0.9720 0.9741 0.9964
(0.5013) (0.5298) (0.5376) (0.5272) (0.5351) (0.7395)
1.010 0.9508 0.9542 0.9569 0.9665 0.9689 0.9874
(1.0804) (1.0907) (1.1089) (1.0832) (1.1014) (1.3878)
2.010 0.9503 0.9502 0.9530 0.9726 0.9747 0.9753
(3.4656) (3.4492) (3.5157) (3.4036) (3.4692) (4.0610)

Notes.

2510 represents 25:25:25:25:25:25:25:25:25:25.

Figure 1. Comparison of the performances of the proposed methods in terms of their coverage probabilities and expected lengths with various sample sizes: (A) k = 3 (B) k = 5 (C) k = 10.

Figure 1

Figure 3. Comparison of the performances of the proposed methods in terms of their coverage probabilities and expected lengths with various variances: (A) k = 3 (B) k = 5 (C) k = 10.

Figure 3

Empirical study

Thailand is generally divided into five areas by topography, i.e., Northern (A1), Northeastern (A2), Central (A3), Eastern (A4), and Southern (A5). The daily rainfall data from these areas in August 2020 were used to assess the performances of the proposed methods for SCI construction. The distributions of these data are presented in Fig. 4, which shows right-skewness for all of the datasets. Thus, the minimum Akaike information criterion (AIC) and the lowest Bayesian information criterion (BIC) were used to test the fitting of the distributions to such data. From AIC and BIC results in Table 5, it is evident that the positive values in the rainfall datasets from the five areas conform to lognormal distributions. Moreover, normal Q-Q plots were constructed to show the distributions of the log-transformed positive rainfall data from the five areas (Fig. 5), which verified the AIC and BIC results that these datasets follow lognormal distributions. A summary of these data are

n1=31,δ ˆ1=0.7097,μ ˆ1=0.7715,σ ˆ12=3.4565,η ˆ1=6.6088,
n2=31,δ ˆ2=0.6774,μ ˆ2=1.4332,σ ˆ22=2.9550,η ˆ2=5.2294,
n3=31,δ ˆ3=0.6452,μ ˆ3=1.5512,σ ˆ32=2.8638,η ˆ3=5.1154,
n4=31,δ ˆ4=0.4839,μ ˆ4=1.4178,σ ˆ42=2.1487,η ˆ4=4.0888,
n5=31,δ ˆ5=0.4839,μ ˆ5=1.8040,σ ˆ52=2.1962,η ˆ5=4.1930.

Table 6 reports the 95% SCIs and credible intervals for all pairwise differences between the CVs of the daily rainfall series from five areas in Thailand. The results show that the expected length of the Bayesian credible interval using the Jeffreys’ rule prior was the shortest, which corresponds with the simulation results. Therefore, it is a good choice for constructing the SCI for all of the pairwise differences between the CVs of the precipitation series from the five areas in Thailand.

Figure 4. The density of daily rainfall data in the five areas of Thailand in August 2020.

Figure 4

Table 5. AIC and BIC results for testing the distributions of the positive daily rainfall data from the five areas of Thailand in August 2020.

Regions AIC BIC
Normal Lognormal Cauchy Exponential Normal Lognormal Cauchy Exponential
Northern 200.1677 126.6431 154.5509 143.7143 202.3498 128.8252 156.7329 144.7143
Northeastern 186.9685 145.5208 170.8114 151.8661 189.0576 147.6098 172.9005 152.9106
Central 187.4002 142.8220 159.7491 148.7169 189.3916 144.8135 161.7405 149.7126
Eastern 129.2900 99.5405 110.7899 100.7356 130.7061 100.9566 112.2060 101.4437
Southern 140.0174 111.4550 124.1323 114.2896 141.4335 112.8711 125.5484 114.9977

Figure 5. Normal Q-Q plots of the log-transformed positive daily rainfall data from the five areas of Thailand in August 2020.

Figure 5

Table 6. The 95% two-sided confidence intervals and credible intervals for all pairwise differences between the CVs of daily rainfall data from the five areas of Thailand in August 2020.

Regions CIFGCI CIB.JruleE CIB.UniE CIB.JruleC CIB.UniC CIMOVER
A1-A2 [−18.6001,34.6174] [−18.9230,29.7356] [−17.4271,40.6785] [−20.0641,27.7802] [−22.5574,31.0130] [−24.4099,41.5271]
A1-A3 [−17.9489,34.8373] [−14.7811,30.1761] [−19.4179,40.0759] [−18.8783,24.1259] [−20.8181,36.4352] [−24.6036,41.6372]
A1-A4 [−12.0747,36.3137] [−11.4058,31.0863] [−13.2535,43.2976] [−15.6054,24.9219] [−18.9824,33.3564] [−19.2874,42.6266]
A1-A5 [−14.6835,36.5005] [−12.4631,30.6305] [−15.3529,42.0874] [−15.9005,25.3713] [−18.3991,35.6191] [−20.8273,42.5263]
A2-A3 [−19.1684,19.8007] [−15.4068,20.8296] [−21.9396,19.5370] [−16.9424,18.6778] [−18.6853,21.7661] [−25.8643,25.7772]
A2-A4 [−14.2284,20.9574] [−12.1077,21.4176] [−15.2508,20.4711] [−12.3215,21.1200] [−16.0818,19.4744] [−20.5246,26.7455]
A2-A5 [−15.1643,20.7719] [−14.3124,21.0636] [−16.9309,20.4638] [−15.1223,19.4770] [−15.7284,20.9116] [−22.0733,26.6474]
A3-A4 [−14.0533,20.3410] [−12.8066,16.4067] [−16.1177,22.6669] [−13.4979,15.6852] [−17.3305,21.2102] [−20.6315,26.9413]
A3-A5 [−15.2305,20.4287] [−14.3490,16.8954] [−17.6976,22.7643] [−14.9963,16.0516] [−16.0804,23.8267] [−22.1806,26.8432]
A4-A5 [−17.1536,14.8658] [−15.0784,13.8954] [−18.1792,16.4151] [−14.9530,14.0968] [−18.1763,16.4173] [−23.1424,21.4920]

Table 3. The coverage probabilities and expected lengths for the 95% SCIs and credible intervals for all pairwise differences between the CVs of delta-lognormal distributions for k = 5.

n1:…:n5 δ11::δ51 σ12::σ52 Coverage probabilities (Expected lengths)
FGCI B.Jrule-E B.Uni-E B.Jrule-C B.Uni-C MOVER
255 0.55 0.55 0.9643 0.9794 0.9854 0.9958 0.9981 0.9986
(2.1555) (2.1428) (2.4893) (2.0756) (2.3915) (3.4245)
1.05 0.9558 0.9597 0.9717 0.9954 0.9982 0.9935
(6.9019) (6.2584) (7.9374) (5.7313) (7.1150) (9.6234)
2.05 0.9519 0.9470 0.9625 0.9973 0.9993 0.9834
(62.1565) (50.5751) (80.8805) (37.1890) (53.9109) (79.5531)
0.52:1.0:2.02 0.9545 0.9538 0.9676 0.9715 0.9818 0.9870
(25.5380) (23.5178) (37.1670) (15.2344) (20.9148) (36.4956)
0.85 0.55 0.9548 0.9642 0.9728 0.9833 0.9895 0.9958
(1.2560) (1.2612) (1.3683) (1.2413) (1.3445) (1.8432)
1.05 0.9529 0.9523 0.9627 0.9857 0.9915 0.9875
(3.2430) (3.1186) (3.4726) (3.0017) (3.3297) (4.2211)
2.05 0.9495 0.9447 0.9567 0.9929 0.9963 0.9757
(16.3407) (15.2264) (17.9101) (13.5908) (15.7761) (19.7367)
0.52:1.0:2.02 0.9525 0.9508 0.9614 0.9696 0.9775 0.9807
(7.2308) (7.5393) (8.7262) (6.1994) (7.0193) (9.6191)
505 0.25 0.55 0.9676 0.9864 0.9896 0.9990 0.9996 0.9994
(4.3044) (4.1252) (5.2361) (3.9094) (4.8405) (7.1615)
1.05 0.9610 0.9688 0.9792 0.9988 0.9997 0.9969
(17.6359) (14.5147) (22.9054) (12.3017) (17.7946) (25.7023)
2.05 0.9532 0.9499 0.9673 0.9988 0.9997 0.9882
(428.000) (253.198) (996.537) (122.265) (272.000) (578.397)
0.52:1.0:2.02 0.9548 0.9550 0.9707 0.9735 0.9849 0.9903
(191.069) (122.152) (490.477) (47.626) (101.477) (276.993)
0.55 0.55 0.9602 0.9789 0.9818 0.9899 0.9921 0.9987
(1.2089) (1.2989) (1.3660) (1.2850) (1.3502) (1.9561)
1.05 0.9548 0.9618 0.9677 0.9876 0.9911 0.9941
(3.0083) (2.9852) (3.2034) (2.9072) (3.1133) (4.2457)
2.05 0.9506 0.9496 0.9578 0.9913 0.9944 0.9839
(13.0787) (12.5396) (13.8536) (11.6771) (12.8287) (16.6737)
0.52:1.0:2.02 0.9537 0.9574 0.9644 0.9695 0.9752 0.9881
(6.1486) (6.5705) (7.1952) (5.7079) (6.1752) (8.6478)
0.85 0.55 0.9541 0.9654 0.9700 0.9763 0.9799 0.9958
(0.7579) (0.7881) (0.8142) (0.7825) (0.8083) (1.1163)
1.05 0.9516 0.9536 0.9589 0.9755 0.9790 0.9874
(1.7233) (1.7170) (1.7855) (1.6937) (1.7603) (2.2261)
2.05 0.9508 0.9495 0.9548 0.9838 0.9871 0.9760
(6.2622) (6.1471) (6.4545) (5.9443) (6.2338) (7.4475)
0.52:1.0:2.02 0.9512 0.9522 0.9574 0.9646 0.9691 0.9808
(3.1366) (3.3900) (3.5463) (3.1199) (3.2508) (4.0931)
1005 0.25 0.55 0.9660 0.9867 0.9883 0.9954 0.9966 0.9994
(2.1027) (2.2959) (2.4445) (2.2638) (2.4055) (3.5676)
1.05 0.9566 0.9680 0.9732 0.9935 0.9958 0.9968
(5.5583) (5.4771) (6.0303) (5.2701) (5.7768) (8.2755)
2.05 0.9521 0.9526 0.9617 0.9951 0.9971 0.9883
(27.9967) (26.1432) (30.2853) (23.4497) (26.8163) (37.2629)
0.52:1.0:2.02 0.9550 0.9598 0.9676 0.9697 0.9763 0.9915
(12.6571) (13.2932) (15.2030) (11.0107) (12.3119) (18.6781)
0.55 0.55 0.9594 0.9791 0.9807 0.9848 0.9862 0.9987
(0.7720) (0.8589) (0.8767) (0.8540) (0.8717) (1.2557)
1.05 0.9546 0.9635 0.9664 0.9793 0.9816 0.9947
(1.7331) (1.7739) (1.8229) (1.7555) (1.8035) (2.4495)
2.05 0.9527 0.9540 0.9582 0.9825 0.9852 0.9848
(6.0963) (6.0429) (6.2535) (5.9008) (6.1028) (7.6733)
0.52:1.0:2.02 0.9527 0.9579 0.9613 0.9645 0.9681 0.9884
(3.1078) (3.4067) (3.5167) (3.1961) (3.2916) (4.3313)
1005 0.85 0.55 0.9542 0.9670 0.9691 0.9721 0.9742 0.9966
(0.5010) (0.5295) (0.5374) (0.5269) (0.5348) (0.7392)
1.05 0.9509 0.9544 0.9570 0.9665 0.9688 0.9875
(1.0812) (1.0918) (1.1102) (1.0842) (1.1024) (1.3890)
2.05 0.9506 0.9507 0.9533 0.9730 0.9752 0.9755
(3.4721) (3.4569) (3.5238) (3.4111) (3.4762) (4.0692)
0.52:1.0:2.02 0.9500 0.9524 0.9552 0.9593 0.9619 0.9806
(1.8380) (2.0041) (2.0416) (1.9233) (1.9575) (2.3760)
252:50:1002 0.55 0.55 0.9608 0.9770 0.9830 0.9830 0.9886 0.9985
(1.5163) (1.4923) (1.6614) (1.4314) (1.5704) (2.2909)
1.05 0.9549 0.9595 0.9688 0.9785 0.9852 0.9940
(4.4104) (3.8914) (4.6543) (3.4894) (4.0239) (5.7364)
2.05 0.9511 0.9484 0.9600 0.9813 0.9872 0.9826
(32.7160) (25.3223) (37.4111) (17.8405) (23.1773) (37.9900)
0.52:1.0:2.02 0.9552 0.9603 0.9655 0.9801 0.9835 0.9901
(3.8324) (4.0083) (4.2595) (3.8460) (4.0906) (5.3939)
0.85 0.55 0.9555 0.9656 0.9719 0.9753 0.9817 0.9959
(0.9159) (0.8965) (0.9522) (0.8736) (0.9239) (1.2760)
1.05 0.9506 0.9512 0.9583 0.9707 0.9774 0.9856
(2.2438) (2.0817) (2.2545) (1.9682) (2.1113) (2.7304)
2.05 0.9496 0.9469 0.9551 0.9774 0.9824 0.9744
(10.1646) (8.9783) (10.2014) (7.7693) (8.6055) (11.2231)
0.52:1.0:2.02 0.9515 0.9536 0.9582 0.9704 0.9737 0.9832
(2.2063) (2.3189) (2.3964) (2.2595) (2.3367) (2.8768)

Notes.

255 represents 25:25:25:25:25.

Figure 2. Comparison of the performances of the proposed methods in terms of their coverage probabilities and expected lengths with various probabilities of non-zero values: (A) k = 3 (B) k = 5 (C) k = 10.

Figure 2

Discussion

The simulation results indicate that the Bayesian credible interval using Jeffreys’ rule prior outperformed the other methods in virtually all cases. Although the coverage probabilities in some cases were close to 1.00, suggesting that overestimation may have occurred, the expected lengths were the shortest. Therefore, the Bayesian credible interval using Jeffreys’ rule prior can be used to construct the SCIs for all of the pairwise differences between the CVs of delta-lognormal distributions. Since constructing SCIs concerns the differences between the parameters of interest for all pairwise comparisons, our findings correspond with Yosboonruang, Niwitpong & Niwitpong (2020) who found that the highest posterior density Bayesian using Jeffreys’ rule prior is appropriate for constructing the confidence interval for the difference between two independent CVs of delta-lognormal distributions. However, Abdel-Karim (2015) and Thangjai, Niwitpong & Niwitpong (2019) reported that MOVER is the most suitable for constructing SCIs for the mean or CV of a lognormal distribution, but this is not in agreement with our findings for the data and scenario used in this study since the range of intervals for its SCI was wider than when using the Bayesian methods. In addition, the SCI range between the CVs of the daily rainfall data series from the five different areas of Thailand was too wide, and so this demonstrates that it is different in rainfall dispersion from five areas in Thailand.

Conclusions

Herein, we proposed methods to construct the SCIs for all pairwise differences between the CVs of delta-lognormal distributions, including FGCI, two Bayesian methods constructed under the equal-tailed confidence intervals and credible intervals using the Jeffreys’ rule and uniform priors, and MOVER. The performances of the proposed methods were determined via their coverage probabilities together with their expected lengths under various circumstances. The results indicate that the Bayesian credible interval using the Jeffreys’ rule prior was suitable for constructing the SCIs for all pairwise differences between the CVs of delta-lognormal distributions in terms of the coverage probability together with the expected length. Furthermore, FGCI is appropriate for constructing these SCIs in cases of the variances equal to 0.5 and 1.0 with the proportion of non-zero values equal to 0.5 and 0.8 for the sample sizes of 50 and 100. In addition, the results of using daily rainfall data from five regions in Thailand coincided with those from the simulation study.

Funding Statement

This research was funding by King Mongkut’s University of Technology North Bangkok. Grant number: KMUTNB-BasicR-64-32. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

Supplemental Information

Supplemental Information 1. The daily rainfall data from these areas in August 2020.

Northern, Northeastern, Central, Eastern and Southern

DOI: 10.7717/peerj.11651/supp-1
Supplemental Information 2. R code for computing coverage probabilities and average length widths for all confidence intervals.
DOI: 10.7717/peerj.11651/supp-2

Additional Information and Declarations

Competing Interests

The authors declare there are no competing interests.

Author Contributions

Noppadon Yosboonruang and Suparat Niwitpong conceived and designed the experiments, performed the experiments, analyzed the data, prepared figures and/or tables, authored or reviewed drafts of the paper, and approved the final draft.

Sa-Aat Niwitpong performed the experiments, analyzed the data, prepared figures and/or tables, authored or reviewed drafts of the paper, and approved the final draft.

Data Availability

The following information was supplied regarding data availability:

All the data and R code are available as Supplemental File.

The data from northern, northeastern, and southern regions of Thailand were collected by the Northern, Upper Northeastern, and Southern East Coast Meteorological Centers and published at:

- Northern Meteorological Center: http://www.cmmet.tmd.go.th/,

- Upper Northeastern Meteorological Center: http://www.khonkaen.tmd.go.th/Home.php,

- Southern-East Coast Meteorological Center: http://www.songkhla.tmd.go.th/.

The data from central Thailand was collected by the Thai Meteorological Department at: https://www.tmd.go.th/en/.

The data from eastern Thailand was obtained from the Eastern Region Irrigation Hydrology Center at: http://hydro-6.com/.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

Supplemental Information 1. The daily rainfall data from these areas in August 2020.

Northern, Northeastern, Central, Eastern and Southern

DOI: 10.7717/peerj.11651/supp-1
Supplemental Information 2. R code for computing coverage probabilities and average length widths for all confidence intervals.
DOI: 10.7717/peerj.11651/supp-2

Data Availability Statement

The following information was supplied regarding data availability:

All the data and R code are available as Supplemental File.

The data from northern, northeastern, and southern regions of Thailand were collected by the Northern, Upper Northeastern, and Southern East Coast Meteorological Centers and published at:

- Northern Meteorological Center: http://www.cmmet.tmd.go.th/,

- Upper Northeastern Meteorological Center: http://www.khonkaen.tmd.go.th/Home.php,

- Southern-East Coast Meteorological Center: http://www.songkhla.tmd.go.th/.

The data from central Thailand was collected by the Thai Meteorological Department at: https://www.tmd.go.th/en/.

The data from eastern Thailand was obtained from the Eastern Region Irrigation Hydrology Center at: http://hydro-6.com/.


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