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Article

Half Logistic Inverted Nadarajah–Haghighi Distribution under Ranked Set Sampling with Applications

1
Department of Mathematics and Statistics, Faculty of Science, Imam Mohammad Ibn Saud Islamic University (IMSIU), Riyadh 11432, Saudi Arabia
2
Department of Mathematics, College of Science, Jouf University, P.O. Box 848, Sakaka 72351, Saudi Arabia
3
Department of Statistics and Operations Research, College of Science, King Saud University, P.O. Box 2455, Riyadh 11451, Saudi Arabia
4
Mathematics and Computer Science Department, Faculty of Science, Beni-Suef University, Beni-Suef 62521, Egypt
5
Faculty of Business Administration, Delta University for Science and Technology, Gamasa 11152, Egypt
*
Author to whom correspondence should be addressed.
Mathematics 2023, 11(7), 1693; https://doi.org/10.3390/math11071693
Submission received: 5 March 2023 / Revised: 23 March 2023 / Accepted: 28 March 2023 / Published: 1 April 2023

Abstract

:
In this paper, we present the half logistic inverted Nadarajah–Haghigh (HL-INH) distribution, a novel extension of the inverted Nadarajah–Haghigh (INH) distribution. The probability density function (PDF) for the HL-INH distribution might have a unimodal, right skewness, or heavy-tailed shape for numerous parameter values; however, the shape forms of the hazard rate function (HRF) for the HL-INH distribution may be decreasing. Four specific entropy measurements were investigated. Some useful expansions for the HL-INH distribution were investigated. Several statistical and computational features of the HL-INH distribution were calculated. Using simple (SRS) and ranked set sampling (RSS), the parameters for the HL-INH distribution were estimated using the maximum likelihood (ML) technique. A simulation analysis was executed in order to determine the model parameters of the HL-INH distribution using the SRS and RSS methods, and RSS was shown to be more efficient than SRS. We demonstrate that the HL-INH distribution is more adaptable than the INH distribution and other statistical distributions when utilizing three real-world datasets.

1. Introduction

The concept of probability distribution has made significant contributions to the process of dealing with both small and big datasets. Probability distribution models are very important and are widely utilized in various sectors such as physics, healthcare, business management, engineering, and food; it also covers the study of social sciences such as economics and psychology. They are ideally suited for the prediction and forecasting of real-world issue modeling. There are several ways for generalizing distributions, including: beta-G [1]; generalized Kumaraswamy-G [2]; Weibull odd Burr III-G [3]; Gompertz-G [4]; a new power Topp-Leone-G [5]; exponentiated Kumaraswamy-G [6]; type I half logistic Weibull-G [7]; type I half logistic Burr X-G [8]; the transmuted Burr X-G in [9]; odd power Lindley-G [10]; gamma Kumaraswamy-G [11]; new extended cosine-G in [12]; extended-gamma-G [13]; odd Chen-G [14]; Kumaraswamy type I half logistic-G [15]; log-logistic-G [16]; gamma-G [17]; Kumaraswamy Poisson-G [18]; Kumaraswamy Kumaraswamy-G [19]; additive odd-G [20]; beta generalized Marshall–Olkin Kumaraswamy-G [21]; extended alpha power transformed family of distributions [22]; odd Burr X-G [23]; the Weibull-G in [24]; type II half logistic-G [25]; sec-G [26]; generalized odd linear exponential-G [27]; Stacy-G [28]; odd Perks-G [29]; sine Topp-Leone-G [30]; Kumaraswamy generalized Marshall–Olkin-G [31]; arcsine-exponentiated-X family-G [32]; odd exponentiated half logistic-G [33]; Kumaraswamy Marshall–Olkin-G [34]; and sine-exponentiated Weibull-H [35], among others. Recently, ref. [36] proposed the type I half logistic (HL)-G, and it has the next cumulative distribution function (CDF):
F y ; α , ς = 1 1 G y ; α , ς α 1 + 1 G y ; α , ς α , α > 0 , y R ,
where ς is the vector of parameters for the baseline distribution. The corresponding PDF of the HL-G is provided via:
f y ; α , ς = 2 α g y ; α , ς 1 G y ; α , ς α 1 1 + 1 G y ; α , ς α 2 .
Ref. [37] proposed the Nadarajah–Haghighi (NH) distribution as a generalization version of the exponential distribution. Its PDF allows for decreasing and unimodal forms, but its HRF allows for decreasing, constant, and increasing shapes. Moreover, like the Weibull, generalized exponential, and lifespan models, its PDF, survival function (SF), and HRF have two parameters. The authors also demonstrated how to interpret the NH model as a shortened Weibull distribution. The PDF and CDF of the NH model are provided as below:
G ( z ; λ , γ ) = 1 e 1 1 + λ z γ , z > 0 , λ , γ > 0 ,
and
g ( z ; λ , γ ) = λ γ 1 + λ z γ 1 e 1 1 + λ z γ , z > 0 , λ , γ > 0 ,
Ref. [38] proposed a novel inverted model called the INH distribution using the transformation Y = 1 / Z , where Z has an NH distribution. The CDF and PDF of INH distribution are given by:
G ( y ; λ , γ ) = e 1 1 + λ y 1 γ , y > 0 , λ , γ > 0 ,
and
g ( y ; λ , γ ) = λ γ y 2 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ , y > 0 , λ , γ > 0 .
Many authors have studied the generalization of the INH distribution, such as: Marshall–Olkin INH (MOINH) distribution [39]; transmuted INH distribution [40]; extended odd Weibull INH distribution (EOWINH) [41]; power INH (PINH) distribution [42]; discrete INH distribution [43]; and odd Lomax INH (OLINH) distribution [44].
The main purpose of this paper is to present the HL-INH model as a new extension of the INH model with one scale parameter λ and two shape parameters γ and α . The following factors provide adequate motivation and explanation to explore the HL-INH model. We will characterize them as follows:
  • The HL-INH distribution is more flexible than the INH distribution, and this is recommended in the application part;
  • The curves of the PDF for the HL-INH distribution may be right-skewed, uni-modal, and heavy-tailed, but the HRF may be decreasing;
  • Several basic important mathematical characteristics of the HL-INH distribution, such as the probability-weighted moments (PWMs), ordinary moments, generating function, and various kinds of entropy, such as the Rényi entropy (REN), Tsallis entropy (TEN), Arimoto entropy (AEN), and Havrda and Charvat entropy (HCEN);
  • The quantile function in the HL-INH distribution has a closed shape (QUF). The QUF is used to determine Bowley skewness (BOS) and Moors kurtosis (MOK);
  • The methodology of ML estimation was utilized to estimate the three unknown parameters of the HL-INH distribution using both simple and ranked set sampling;
  • For modeling real-world datasets in several disciplines, the HL-INH distribution fits better than the INH distribution and several other well-known statistical distributions, which is suggested in the application part.
The following describes the way that this manuscript is structured. Section 2 describes how to create the HL-INH model by merging the INH model with the HL generated family of distributions. In Section 3, we develop and analyze various essential expansions for calculating the statistical features of the HL-INH. In Section 4, several entropy measurements are calculated. In Section 5, we investigate various important mathematical characteristics of the HL-INH model. Section 6 discusses RSS. Section 7 investigates estimations of the three unknown parameters utilizing the ML approach under SRS and RSS. Section 8 discusses the simulation results. The relevance and adaptability of the HL-INH distribution are demonstrated in Section 9 by employing three real-world datasets. Furthermore, the concluding remarks are made at the end of the manuscript.

2. The HL-INH Distribution

In this section, we construct three new parameters for continuous statistical distribution called the half logistic inverted Nadarajah–Haghighi (HL-INH) distribution by inserting Equations (5) and (6) into (1) and (2); then, the CDF, PDF, and reliability function (RF) are:
F y ; α , λ , γ = 1 1 e 1 1 + λ y 1 γ α 1 + 1 e 1 1 + λ y 1 γ α ,
f y ; α , λ , γ = 2 α λ γ y 2 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ α 1 1 + 1 e 1 1 + λ y 1 γ α 2 ,
and
S y ; α , λ , γ = 2 1 e 1 1 + λ y 1 γ α 1 + 1 e 1 1 + λ y 1 γ α .
The HRF, reversed HRF, and cumulative HRF are supplied as below:
h y ; α , λ , γ = α λ γ y 2 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ 1 + 1 e 1 1 + λ y 1 γ α ,
τ y ; α , λ , γ = 2 α λ γ y 2 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ α 1 1 1 e 1 1 + λ y 1 γ 2 α ,
and
H y ; α , λ , γ = log 2 1 e 1 1 + λ y 1 γ α 1 + 1 e 1 1 + λ y 1 γ α .
Figure 1 shows the curves of PDF and HRF for the HL-INH distribution with various values of parameters.

3. Some Important Linear Representations

Here, three important linear representations of f ( y ; α , λ , γ ) , F ( y ; α , λ , γ ) h , and f ( y ; α , λ , γ ) η for the HL-INH distribution are investigated to make the calculation of the basic mathematical characteristics simple because we can rewrite the PDF and CDF of the HL-INH distribution as a linear representation of the INH distribution.
At the beginning, we investigate the expansion of f ( y ; α , λ , γ ) by using the binomial theorem:
1 + y β = i = 0 1 i β + i 1 i y i .
By substituting (9) in (8), then
f y ; α , λ , γ = 2 α β λ γ y 2 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ i = 0 1 i ( 1 + i ) 1 e 1 1 + λ y 1 γ α ( i + 1 ) 1 .
Again, by utilizing the binomial theorem,
1 y β = j = 0 1 j β j y j .
By inserting (11) in (10), then
f y ; α , λ , γ = i , j = 0 i , j y 2 1 + λ y 1 γ 1 e ( j + 1 ) 1 + λ y 1 γ ,
where, i , j = 2 α β λ γ e j + 1 1 i + j ( 1 + i ) α ( i + 1 ) 1 j .
To investigate the linear representation of F ( y ; α , λ , γ ) h , then
F y ; α , λ , γ h = 1 1 e 1 1 + λ y 1 γ α 1 + 1 e 1 1 + λ y 1 γ α h .
By utilizing the binomial series two times in the previous equation, then we get
F y ; α , λ , γ h = u , ν = 0 h 1 u + ν h + u 1 u h ν 1 e 1 1 + λ y 1 γ α ( u + ν ) ,
Again, by utilizing the binomial theorem, then
F y ; α , λ , γ h = u , ν = 0 h m = 0 u , ν , m e m 1 + λ y 1 γ ,
where i , j , k = 1 u + ν + m h + u 1 u h ν α ( u + ν ) m e m .
To compute the linear combination of f ( y ; α , λ , γ ) η , then
f y ; α , λ , γ η = 2 α λ γ e η y 2 η 1 + λ y 1 η ( γ 1 ) e η 1 + λ y 1 γ 1 e 1 1 + λ y 1 γ η ( α 1 ) 1 + 1 e 1 1 + λ y 1 γ α 2 η .
By employing the binomial theorem in the above equation, then
f y ; α , λ , γ η = 2 α λ γ e η y 2 η 1 + λ y 1 η ( γ 1 ) e η 1 + λ y 1 γ i = 0 1 i 2 η + i 1 i 1 e 1 1 + λ y 1 γ η ( α 1 ) + α i ,
Again, by employing the binomial theorem, we get
f y ; α , λ , γ η = y 2 η 1 + λ y 1 η ( γ 1 ) i , j = 0 π i , j e ( η + j ) 1 + λ y 1 γ ,
where π i , j = 2 α λ γ η 1 i + j 2 η + i 1 i η ( α 1 ) + α i j e η + j .

4. Four Various Measures of Uncertainty

One of the most important measures of uncertainty is entropy. The various types of entropy are useful in determining the risk and reliability analysis.

4.1. Arimoto Entropy

The AEN [45] measure is computed from the equation below:
A η = η 1 η J η y 1 η 1 , η > 0 , η 1 .
where J η y = 0 f y ; α , λ , γ η d y . Now, we need to compute the integral J η y . Then, by using Equation (15), we get
J η y = 0 f y ; α , λ , γ η d y = i , j = 0 π i , j 0 y 2 η 1 + λ y 1 η ( γ 1 ) e ( η + j ) 1 + λ y 1 γ d y ,
Let v = 1 + λ y 1 γ , then
J η y = λ 2 η + 1 γ i , j = 0 π i , j 0 v η η γ + 1 γ 1 1 v 1 γ 2 η 2 e ( η + j ) v d v .
By using the binomial theory to Equation (17), then
J η y = λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j 0 v η η γ + k γ + 1 γ 1 e ( η + j ) v d v .
By utilizing the gamma function, then
J η y = λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j Γ η + k η + 1 γ ( η + j ) η + k η + 1 γ .
By inserting Equation (18) into (16), then the AEN of the HL-INH distribution is
A η = η 1 η λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j Γ η + k η + 1 γ ( η + j ) η + k η + 1 γ 1 η 1 .

4.2. Rényi Entropy

The REN [46] measure is computed from the equation below:
R η = 1 1 η log J η y , η > 0 , η 1 .
By inserting Equation (18) into (19), then the REN of the HL-INH distribution is
R η = 1 1 η log λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j Γ η + k η + 1 γ ( η + j ) η + k η + 1 γ .

4.3. Tsallis Entropy

The TEN [47] measure is computed from the equation below:
T η = 1 η 1 1 J η y , η > 0 , η 1 .
By inserting Equation (18) into (20), then the TEN of the HL-INH distribution is
T η = 1 η 1 1 λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j Γ η + k η + 1 γ ( η + j ) η + k η + 1 γ .

4.4. Havrda and Charvat Entropy

The HCEN [48] measure is computed from the equation below:
H C η = 1 2 1 η 1 J η y 1 η 1 , η > 0 , η 1 .
By inserting Equation (18) into (21), then the HCEN of the HL-INH distribution is
H C η = 1 2 1 η 1 λ 2 η + 1 γ i , j = 0 k = 0 2 η 2 1 k 2 η 2 k π i , j Γ η + k η + 1 γ ( η + j ) η + k η + 1 γ 1 η 1 .
Table 1 and Table 2 represent the analysis of the REN, HCEN, TEN, and AEN for the HL-INH distribution at λ = 1.5.

5. Important Mathematical Features of the HL-INH Distribution

This section investigates some important mathematical features of the HL-INH distribution.

5.1. Probability Weighted Moments

The ( q , h ) th PWMs for the HL-INH distribution, signified as ρ q , h , is computed from the equation below:
ρ q , h = 0 1 y q f ( y ; α , λ , γ ) F y ; α , λ , γ h d y .
By entering Equation (12) and (13) into (22), then
ρ q , h = i , j = 0 u , ν = 0 h m = 0 u , ν , m i , j 0 y q 2 1 + λ y 1 γ 1 e ( j + m + 1 ) 1 + λ y 1 γ d y .
Let v = 1 + λ y 1 γ , then
ρ q , h = λ q 1 γ i , j = 0 u , ν = 0 h m = 0 1 q u , ν , m i , j 0 1 v 1 γ q e ( j + m + 1 ) v d v ,
By using the binomial expansion, then
ρ q , h = λ q 1 γ i , j = 0 u , ν = 0 h m = 0 k = 0 1 q q + k 1 k u , ν , m i , j 0 v k γ e ( j + m + 1 ) v d v ,
Then, the PWMs of the HL-INH distribution is
ρ q , h = λ q 1 γ i , j = 0 u , ν = 0 h m = 0 k = 0 1 q q + k 1 k u , ν , m i , j Γ k γ + 1 ( j + m + 1 ) k γ + 1 .

5.2. Moments

The mth ordinary moment of a random variable Y may be calculated using the following equation:
μ m = 0 y m f ( y ; α , λ , γ ) d y .
By inserting Equation (12) into (23), then
μ m = i , j = 0 i , j 0 y m 2 1 + λ y 1 γ 1 e ( j + 1 ) 1 + λ y 1 γ d y
Let v = 1 + λ y 1 γ , then
μ m = i , j = 0 1 m λ m i , j γ 0 1 v 1 γ m e ( j + 1 ) v d v ,
By using the binomial theory, then
μ m = i , j , k = 0 1 m λ m i , j γ m + k 1 k 0 v k γ e ( j + 1 ) v d v .
By using the gamma function ( Γ ( . , . ) ), the mth moment of the HL-INH distribution is
μ m = i , j , k = 0 1 m λ m i , j Γ k γ + 1 γ j + 1 k γ + 1 m + k 1 k .
Table 3 represents the numerical results of E ( Y ) , E ( Y 2 ) , E ( Y 3 ) , E ( Y 4 ) , the variance ( σ 2 ), the skewness ( γ 1 ), the kurtosis ( γ 2 ), the index of dispersion (ID), and the coefficient of variation ( C V ).

5.3. Quantile Function and Skewness

The QUF is a useful measure that is utilized in order to produce random samples from the HL-INH distribution. Assume that Y HL - INH ( α , λ , γ ) for Y > 0 and α , λ , γ > 0 ; then, the QUF is provided via
y p = λ 1 ln 1 1 p 1 + p 1 α 1 γ 1 1 , 0 < p < 1 .
The first quantile ( y 0.25 ), the second quantile ( y 0.5 ) (median), and the third quantile ( y 0.75 ) for the HL-INH distribution are provided as below:
y 0.25 = λ 1 ln 1 3 5 1 α 1 γ 1 1 , 0 < p < 1 ,
y 0.5 = λ 1 ln 1 1 3 1 α 1 γ 1 1 , 0 < p < 1 ,
and
y 0.75 = λ 1 ln 1 1 7 1 α 1 γ 1 1 , 0 < p < 1 .
The Bowley skewness ( β 3 ) and Moors kurtosis ( β 4 ) are provided via
β 3 = y 0.75 + y 0.25 2 y 0.5 y 0.75 y 0.25 .
and
β 4 = y 0.875 y 0.625 + y 0.375 y 0.125 y 0.75 y 0.25 .

6. Sampling Techniques

The SRS method is the most common method of data collection. In these situations, ranked sampling procedures may be employed to investigate more representative samples from the underlying population and improve the efficacy of the statistical inference. The RSS method was first put forth by [49,50]. Several investigations have demonstrated that, either numerically or theoretically, RSS statistical processes are superior to their SRS analogs. The size of ranking sampling n for the one-cycle c = 1 is as follows:
1 . y ( 1 : n ) ( 1 ) ̲ y ( 2 : n ) ( 1 ) y ( n : n ) ( 1 ) y ( 1 ) = y ( 1 : n ) ( 1 ) 2 . y ( 1 : n ) ( 2 ) y ( 2 : n ) ( 2 ) ̲ y ( n : n ) ( 2 ) y ( 2 ) = y ( 2 : n ) ( 2 ) n . y ( 1 : n ) ( n ) y ( 2 : n ) ( n ) y ( n : n ) ( n ) ̲ y ( n ) = y ( n : n ) ( n )
The resulting sample, which has the size n, is known as a one-cycle RSS; it is represented by the equation Y ̲ = ( y ( 1 ) , y ( 2 ) , , y ( n ) ) . According to [51], using the perfect judgement ranking as a foundation, y ( i ) has the same distribution as the order statistic in a set of size n generated from the ith sample with the PDF method.
The initial ranking of n samples of size n for more than one cycle appears as described in Table 4.
f ( i ) ( y ) = n ! ( i 1 ) ! ( n i ) ! [ F ( y ( i ) j ) ] i 1 [ 1 F ( y ( i ) j ) ] n i f ( y ( i ) j ) .

7. Approach of Maximum Likelihood Estimation

In this part, we derive the SRS and RSS to estimate the parameter estimators of the HL-INH distribution α , γ , and λ .

7.1. ML Estimation under SRS

In this subsection, we must first investigate the ML estimates (MLEs) of α , γ , and λ under SRS. Let Y i , where i = ( 1 , , n ) . The likelihood function (LF) under SRS is:
L ( α , γ , λ ) = i = 1 n f Y ( y i ) = 2 n α n λ n γ n e n i = 1 n 1 + λ y i 1 γ i = 1 n y i 2 1 + λ y i 1 γ 1 1 e 1 1 + λ y i 1 γ α 1 1 + 1 e 1 1 + λ y i 1 γ α 2 .
The observed samples’ ln-LF is
( α , γ , λ ) = n ln ( 2 ) + ln ( α ) + ln ( λ ) + ln ( γ ) + n i = 1 n 1 + λ y i 1 γ 2 i = 1 n ln ( y i ) + ( γ 1 ) i = 1 n ln 1 + λ y i 1 + ( α 1 ) i = 1 n ln 1 e 1 1 + λ y i 1 γ 2 i = 1 n ln 1 + 1 e 1 1 + λ y i 1 γ α .
To derive the likelihood equations, the partial derivatives of Equation (28) with respect to α , γ , and λ are
( α , γ , λ ) α = n α + i = 1 n ln 1 e 1 1 + λ y i 1 γ 2 i = 1 n 1 e 1 1 + λ y i 1 γ α ln 1 e 1 1 + λ y i 1 γ 1 + 1 e 1 1 + λ y i 1 γ α ,
( α , γ , λ ) γ = n γ i = 1 n 1 + λ y i 1 γ ln 1 + λ y i 1 + i = 1 n ln 1 + λ y i 1 + ( α 1 ) i = 1 n e 1 1 + λ y i 1 γ 1 + λ y i 1 γ ln 1 + λ y i 1 1 e 1 1 + λ y i 1 γ 2 i = 1 n 1 e 1 1 + λ y i 1 γ α 1 e 1 1 + λ y i 1 γ 1 + λ y i 1 γ ln 1 + λ y i 1 1 + 1 e 1 1 + λ y i 1 γ α ,
and
( α , γ , λ ) λ = n λ γ i = 1 n y i 1 1 + λ y i 1 γ 1 + ( γ 1 ) i = 1 n y i 1 1 + λ y i 1 + ( α 1 ) γ i = 1 n y i 1 1 + λ y i 1 γ 1 e 1 1 + λ y i 1 γ 1 e 1 1 + λ y i 1 γ 2 α γ i = 1 n y i 1 1 + λ y i 1 γ 1 e 1 1 + λ y i 1 γ 1 e 1 1 + λ y i 1 γ α 1 1 + 1 e 1 1 + λ y i 1 γ α .
To obtain the MLE under the SRS method, it is necessary to simultaneously solve three non-linear Equations (29)–(31) by equating them to zero, respectively. The “optim” function of the “stats” package, which uses the “Nelder–Mead (NM)” strategy of maximization in the MLE computations, can be used in R language to obtain the MLEs α , γ , and λ for any given data set.

7.2. ML Estimation under on RSS

Let the c-cycle of RSS from the HL-INH ( α , γ , λ ) be y ( i ) j , i = 1 , , n j , j = 1 , , c . Equation (26) yields the following function under RSS:
g i : n j ( y ( i ) j ; α , γ , λ ) = C i : n j F ( y ( i ) j ; α , γ , λ ) i 1 1 F ( y ( i ) j ; α , γ , λ ) n j i f ( y ( i ) j ; α , γ , λ ) ,
where C i : n j = n j ! ( i 1 ) ! ( n j i ) ! . By using Equation (26), the LF under RSS is
L ( α , γ , λ ; y ( i ) j ) = j = 1 c i = 1 n j g i ( y ( i ) j ; α , γ , λ ) = j = 1 c i = 1 n j C i : n j 1 1 e 1 1 + λ y ( i ) j 1 γ α 1 + 1 e 1 1 + λ y ( i ) j 1 γ α i 1 2 1 e 1 1 + λ y ( i ) j 1 γ α 1 + 1 e 1 1 + λ y ( i ) j 1 γ α n j 1 × j = 1 c 2 n j α n j λ n j γ n j e n j i = 1 n j 1 + λ y ( i ) j 1 γ i = 1 n j y ( i ) j 2 1 + λ y ( i ) j 1 γ 1 1 e 1 1 + λ y ( i ) j 1 γ α 1 1 + 1 e 1 1 + λ y ( i ) j 1 γ α 2 .
where N = j = 1 c n j . The ln-LF of the HL-INH distribution in this situation is given by
α , γ , λ , y i j = j = 1 c i = 1 n j ln C i : n j + j = 1 c i = 1 n j i 1 ln 1 1 e 1 1 + λ y i j 1 γ α j = 1 c i = 1 n j i 1 ln 1 + 1 e 1 1 + λ y i j 1 γ α + j = 1 c i = 1 n j n j 1 ln 2 1 e 1 1 + λ y i j 1 γ α j = 1 c i = 1 n j n j 1 ln 1 + 1 e 1 1 + λ y i j 1 γ α + N ln 2 + N ln α + N ln λ + N ln γ + N j = 1 c i = 1 n j 1 + λ y i j 1 γ 2 j = 1 c i = 1 n j ln y i j + γ 1 j = 1 c i = 1 n j ln 1 + λ y i j 1 + α 1 j = 1 c i = 1 n j ln 1 e 1 1 + λ y i j 1 γ 2 j = 1 c i = 1 n j ln 1 + 1 e 1 1 + λ y i j 1 γ α .
With respect to unknown parameters, the partial derivatives of ( α , γ , λ ; y i j ) can be written as
α , γ , λ , y i j α = j = 1 c i = 1 n j i 1 ln 1 e 1 1 + λ y i j 1 γ 1 e 1 1 + λ y i j 1 γ α 1 j = 1 c i = 1 n j i 1 ln 1 e 1 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α + j = 1 c i = 1 n j n j 1 ln 1 e 1 1 + λ y i j 1 γ j = 1 c i = 1 n j n j 1 ln 1 e 1 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α + N α + j = 1 c i = 1 n j ln 1 e 1 1 + λ y i j 1 γ 2 j = 1 c i = 1 n j ln 1 e 1 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α .
α , γ , λ , y i j γ = α j = 1 c i = 1 n j i 1 1 + λ y i j 1 γ e 1 1 + λ y i j 1 γ 1 e 1 1 + λ y i j 1 γ α 1 ln 1 + λ y i j 1 1 1 e 1 1 + λ y i j 1 γ α α j = 1 c i = 1 n j i 1 1 + λ y i j 1 γ e 1 1 + λ y i j 1 γ 1 e 1 1 + λ y i j 1 γ α 1 ln 1 + λ y i j 1 1 + 1 e 1 1 + λ y i j 1 γ α + α j = 1 c i = 1 n j n j 1 1 + λ y i j 1 γ ln 1 + λ y i j 1 e 1 + 1 + λ y i j 1 γ 1 + N γ α j = 1 c i = 1 n j n j 1 1 + λ y i j 1 γ e 1 1 + λ y i j 1 γ 1 e 1 1 + λ y i j 1 γ α 1 ln 1 + λ y i j 1 1 + 1 e 1 1 + λ y i j 1 γ α j = 1 c i = 1 n j 1 + λ y i j 1 γ ln 1 + λ y i j 1 + j = 1 c i = 1 n j ln 1 + λ y i j 1 + α 1 j = 1 c i = 1 n j 1 + λ y i j 1 γ e 1 1 + λ y i j 1 γ ln 1 + λ y i j 1 1 e 1 1 + λ y i j 1 γ 2 α j = 1 c i = 1 n j 1 + λ y i j 1 γ e 1 1 + λ y i j 1 γ 1 e 1 1 + λ y i j 1 γ α 1 ln 1 + λ y i j 1 1 + 1 e 1 1 + λ y i j 1 γ α ,
and
α , γ , λ , y i j λ = α γ j = 1 c i = 1 n j i 1 1 + λ y i j 1 γ 1 1 e 1 1 + λ y i j 1 γ α 1 y i j e 1 + 1 + λ y i j 1 γ 1 1 e 1 1 + λ y i j 1 γ α + N λ α γ j = 1 c i = 1 n j i 1 1 + λ y i j 1 γ 1 1 e 1 1 + λ y i j 1 γ α 1 y i j e 1 + 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α + α γ j = 1 c i = 1 n j n j 1 1 + λ y i j 1 γ 1 y i j e 1 + 1 + λ y i j 1 γ 1 γ j = 1 c i = 1 n j y i j 1 1 + λ y i j 1 γ 1 α γ j = 1 c i = 1 n j n j 1 1 + λ y i j 1 γ 1 1 e 1 1 + λ y i j 1 γ α 1 y i j e 1 + 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α + γ 1 j = 1 c i = 1 n j 1 y i j + λ + γ α 1 j = 1 c i = 1 n j 1 + λ y i j 1 γ 1 y i j e 1 + 1 + λ y i j 1 γ 1 2 α γ j = 1 c i = 1 n j 1 + λ y i j 1 γ 1 1 e 1 1 + λ y i j 1 γ α 1 y i j e 1 + 1 + λ y i j 1 γ 1 + 1 e 1 1 + λ y i j 1 γ α .
The MLEs can be derived by numerically solving the nonlinear equations ( α , γ , λ ; y ( i ) j ) α = 0 , ( α , γ , λ ; y ( i ) j ) γ = 0 , and ( α , γ , λ ; y ( i ) j ) λ = 0 .

7.3. Asymptotic Confidence Interval

The Fisher information matrix (FIM) I of parameters α , γ , and λ , which are the negative expectations of the second derivative of ln-LF, is produced by the Hessian matrix using the “optim” function. The variance–covariance is described by the inverse FIM. When n rises, the asymptotic distribution of the MLE ( α ^ , γ ^ , λ ^ ) is as follows:
α ^ γ ^ λ ^ N α γ λ , V ^ 11 V ^ 12 V ^ 13 V ^ 21 V ^ 22 V ^ 23 V ^ 31 V ^ 32 V ^ 33
.
The estimates of α ^ , γ ^ , and λ ^ of the asymptotic variance–covariance matrix V are obtained by inverting the Hessian matrix.

8. Simulation

Using R packages, we perform numerous calculations in accordance with Monte Carlo simulation (MCS) experiments with different combinations of sample sizes n (as n = 6, 8, 12, 17) and cycle sizes c ( c = 1, 3) as part of our complete effort to assess the effectiveness of the inference estimation methods provided. The following parameters ( α , γ , λ ) are used to create a HL-INH sample: (0.7, 0.5, 0.6), (0.7, 0.5, 3), (0.7, 3, 0.6), (2.5, 0.5, 0.6), (2.5 0.5, 3), (2.5, 3, 0.6), and (2.5 3, 3). The bias, accompanying mean squared error (MSEs), and relative efficiency (RE) of the point parameter resultant α , γ , and λ estimators are evaluated as follows:
B i a s ( α ) = 1 L i = 1 L α ^ α , B i a s ( γ ) = 1 L i = 1 L γ ^ γ , B i a s ( λ ) = 1 L i = 1 L λ ^ λ ,
M S E s ( α ) = 1 L i = 1 L α ^ α 2 , M S E s ( γ ) = 1 L i = 1 L γ ^ γ 2 , M S E s ( λ ) = 1 L i = 1 L λ ^ λ 2 ,
and
R E 1 ( α ) ) = M S E s S R S ( α ) ) M S E s R S S s = 1 ( α ) ) , R E 2 ( α ) = M S E s S R S ( α ) M S E s R S S s = 3 ( α ) , R E 3 ( α ) = M S E s R S S s = 1 ( α ) M S E s R S S s = 3 ( α ) ,
R E 1 ( γ ) ) = M S E s S R S ( γ ) ) M S E s R S S s = 1 ( γ ) ) , R E 2 ( γ ) = M S E s S R S ( γ ) M S E s R S S s = 3 ( γ ) , R E 3 ( γ ) = M S E s R S S s = 1 ( γ ) M S E s R S S s = 3 ( γ ) ,
and
R E 1 ( λ ) ) = M S E s S R S ( λ ) ) M S E s R S S s = 1 ( λ ) ) , R E 2 ( λ ) = M S E s S R S ( λ ) M S E s R S S s = 3 ( λ ) , R E 3 ( λ ) = M S E s R S S s = 1 ( λ ) M S E s R S S s = 3 ( λ ) ,
The ACI has been considered to obtain the lower (L-ACI), upper (U-ACI), and coverage probability (CP) for the parameters of the f HL-INH distribution with each sampling techniques as follows:
L A C I ( α ) = α ^ z 0.025 V a r ( α ^ ) , L A C I ( γ ) = γ ^ z 0.025 V a r ( γ ^ ) , L A C I ( λ ) = λ ^ z 0.025 V a r ( λ ^ ) 1 c m U A C I ( α ) = α ^ + z 0.025 V a r ( α ^ ) , U A C I ( γ ) = γ ^ + z 0.025 V a r ( γ ^ ) , U A C I ( λ ) = λ ^ + z 0.025 V a r ( λ ^ ) ,
C P ( α ) = M e a n 1 if L A C I ( α ) α ^ U A C I ( α ) 0 otherwise ,
C P ( γ ) = M e a n 1 if L A C I ( γ ) γ ^ U A C I ( γ ) 0 otherwise ,
and
C P ( λ ) = M e a n 1 if L A C I ( λ ) λ ^ U A C I ( λ ) 0 otherwise
where V a r ( . ) = M S E s ( . ) B i a s ( . ) .
Using an MCS and the “optim” function in the “stats” R package with “L = 10,000” repeats, the performance of the estimations is compared for different sizes n, number of cycles c, and different chosen parameter values. We utilized the “rss” function in the “RSSampling” R package to create an RSS sampling. This function uses ranked set sampling to select samples from a target population.
The results of the simulation investigation for point estimation are presented in Table 5 and Table 6. We draw the following conclusions from these tables:
  • The bias and MSEs for parameters have a downward trend when n value increases.
  • We can see that the results for bias and MSEs under RSS are consistently L-ACI compared with the values under SRS.
  • As n or c increases, all recommended estimates perform better.
  • When the value of λ increases with sample size > 8 , we note that the bias and MSEs for the parameters have a downward trend.
  • When the value of γ increases with sample size > 8 , we note that the bias and MSEs for parameters have a downward trend.
  • RE2 is the largest RE when compared with RE1 and RE3 because it is the ratio between the estimated MSEs of the SRS and RSS with c = 3 .
  • All RE values are greater than 1.
The results of the simulation investigation for point estimation are presented in Table 7 and Table 8. We draw the following conclusions from these tables:
  • The L-ACI and U-ACI for the parameters have convergence when n value increases.
  • The length of ACI (U-ACI-L-ACI) have a downward trend when n value increases.
  • We can see that the results for L-ACI and U-ACI under RSS are consistently lower than the values under SRS.
  • As n or c increases, all recommended estimates perform better.
  • The CP for all estimates are approximately 95%.

9. Application

The analysis of three real-world datasets, one of which is linked to COVID-19 data and another to yearly flood flows, are discussed in this part to confirm that the HL-INH distribution is the best model fitting present in the literature. The models used for comparison are OLINH; PINH; INH; EOWINH; MOINH; extended Weibull (EW), which was discussed by [52]; exponential Lomax (EL), which was discussed by [53]; Weibull-Lomax (WL), which was discussed by [54]; and Gumbel-Lomax (GL), which was discussed by [55].
Furthermore, we calculate the estimates with the standard error (SE) and eight measures of goodness of fit statistics (GFS) for each statistical model, with the eight measures consisting of “Akaike Information (AI) as M1, corrected AI as M2, Bayesian information as M3, Hannan—Quinn information as M4, Cramer-von-Mises as M5, Anderson—Darling as M6, Kolmogorov-Smirnov distance as M7, and p-value as M8”. The model generally regarded as the best is the one with the smaller M1, M2, M3, M4, M5, M6, and M7 statistics and the higher M8 for the GFS. It should be emphasized that all findings were obtained using the MLE technique.
Flood data: The North Saskatchewan River in Edmonton’s annual flood flows in units of 1000 f3/second over a 47-year period make up the first dataset, according to [56]. Figure 2 discussed the flood data description by box plots, strip plots, and violin plots. The violin plot is used to show how the numerical data is distributed. Violin plots provide summary statistics as well as the density of each variable unlike box plots, which can only show summary statistics. This flood data set has a right-skewed shape, which corresponds to the nature of the distribution form (see Figure 1). The MLE for various competitive statistical distributions with various measures of GFS for the flood data are discussed in Table 9. Figure 3 displays the fitted CDF with an empirical CDF in I, the fitted PDF with flood data histograms in II, a QQ plot in III, and a PP plot for HL-INH in IV. Figure 4 shows the profile likelihood of the estimators of parameters for the HL-INH distribution using the flood data. We confirm that the HL-INH distribution is the best model to fit the flood data, and the estimates have uniqueness and a maximum point of log likelihood.
COVID-19 data: The COVID-19 data covers Britain over 82 days, ranging from 1 May to 16 July 2021. The data shown below are derived from daily new deaths, daily cumulative cases, and daily cumulative deaths. These data have been obtained by [57] as follows: “0.0023, 0.0023, 0.0023, 0.0046, 0.0065, 0.0067, 0.0069, 0.0069, 0.0091, 0.0093, 0.0093, 0.0093, 0.0111, 0.0115, 0.0116, 0.0116, 0.0119, 0.0133, 0.0136, 0.0138, 0.0138, 0.0159, 0.0161, 0.0162, 0.0162, 0.0162, 0.0163, 0.0180, 0.0187, 0.0202, 0.0207, 0.0208, 0.0225, 0.0230, 0.0230, 0.0239, 0.0245, 0.0251, 0.0255, 0.0255, 0.0271, 0.0275, 0.0295, 0.0297, 0.0300, 0.0302, 0.0312, 0.0314, 0.0326, 0.0346, 0.0349, 0.0350, 0.0355, 0.0379, 0.0384, 0.0394, 0.0394, 0.0412, 0.0419, 0.0425, 0.0461, 0.0464, 0.0468, 0.0471, 0.0495, 0.0501, 0.0521, 0.0571, 0.0588, 0.0597, 0.0628, 0.0679, 0.0685, 0.0715, 0.0766, 0.0780, 0.0942, 0.0960, 0.0988, 0.1223, 0.1343, 0.1781”. These data have been cited in https://covid19.who.int/ (accessed on 15 February 2023). Figure 5 discusses the data description using box, strip, and violin plots. This COVID-19 dataset has a right-skewed shape, which corresponds to the nature of the distribution form (see Figure 1). The MLE for various models with various statistics of GFS for the COVID-19 data of Britain are discussed in Table 10. Figure 6 displays the fitted CDF with an empirical CDF in I, the fitted PDF with COVID-19 data histograms in II, a QQ plot in III, and a PP plot for the HL-INH distribution in IV. Figure 7 shows the profile likelihood for the parameters of the HL-INH distribution based on British COVID-19 data. We confirm that the HL-INH distribution is the best model for the fitting of the COVID-19 data, and the estimates have uniqueness and a maximum point of log likelihood.
We observed random samples of varied sizes for analysis using the SRS and RSS techniques with different set sizes and cycle counts. The performance of the estimations was then compared after we computed the MLE for the observed SRS and RSS with different cycle c values. As demonstrated in Table 11, we were able to obtain RSS data for the first batch of data when n = 12 and n = 15 with various cycles as c = 1 and c = 3 . Table 12 displays the MLE under SRS and RSS with various c for the flood data. As demonstrated in Table 13, we were able to obtain RSS data for the second batch of data when n = 15 and n = 18 with various cycles as c = 1 and c = 3 . Table 14 displays the MLE under SRS and RSS with various cycles for the COVID-19 data. We note that the SE for RSS is smaller than the SE for SRS. The performance of the estimations was then compared after we computed the MLE for the observed SRS and RSS with different cycle c values. Table 15 discusses the summarized measures for each data sets. As demonstrated in Table 16 and Table 17, we were discussed MLE for each model with different measures for carbon fibre data and we were able to obtain RSS carbon fibre data for the first batch of data when n = 28 with various cycles as c = 1 and c = 4 , respectively. Table 18 displays the MLE under SRS and RSS with various c for the carbon fibre data.
Carbon fibre data: The third dataset has [58] as its source. It includes the single carbon fibre tensile strength (in GPa). This information is provided by: 0.312, 0.314, 0.479, 0.552, 0.700, 0.803, 0.861, 0.865, 0.944, 0.958, 0.966, 0.997, 1.006, 1.021, 1.027, 1.055, 1.063, 1.098, 1.140, 1.179, 1.224, 1.240, 1.253, 1.270, 1.272, 1.274, 1.301, 1.301, 1.359, 1.382, 1.382, 1.426, 1.434, 1.435, 1.478, 1.490, 1.511, 1.514, 1.535, 1.554, 1.566, 1.570, 1.586, 1.629, 1.633, 1.642, 1.648, 1.684, 1.697, 1.726, 1.770, 1.773, 1.800, 1.809, 1.818, 1.821, 1.848, 1.880, 1.954, 2.012, 2.067, 2.084, 2.090, 2.096, 2.128, 2.233, 2.433, 2.585, 2.585.
Table 15 discusses the summarized measures for each dataset, including the minimum (Min), maximum (Max), first quantile (Q1), median, mean, third quantile (Q3), variance ( σ 2 ), skewness (SK), and kurtosis (KT).
The MLE for the various models with various statistics of GFS for the carbon fibre data are discussed in Table 16 and Figure 8. Figure 9 displays the fitted CDF using an empirical CDF in I and the fitted PDF using carbon fibre data histograms in II, a QQ plot in III, and a PP plot for HL-INH in IV. Figure 10 shows the profile likelihood for the parameters of the HL-INH distribution based on the carbon fibre data. We confirm that the HL-INH distribution is the best model for the fitting of the carbon fibre data, and the estimates have uniqueness and a maximum point of log likelihood.

10. Conclusions

In this paper, we suggested and studied the HL-INH distribution, a new extension of the INH distribution. The shape forms of the PDF for the HL-INH distribution for numerous parameter values are asymmetric. Some useful expansions for the HL-INH distribution were computed. Four alternative entropy measurements were discussed. Several statistical and computational aspects of the HL-INH distribution were computed. Using the SRS and RSS methods, the parameters for the HL-INH distribution were estimated using the ML technique. A simulation analysis was carried out to demonstrate that RSS outperforms SRS. The HL-INH distribution is more flexible than the INH distribution and other distributions such as the OLINH, PINH, INH, EOWINH, MOINH, EW, EL, GL, and WL distributions. The HL-INH distribution provides the greatest fit for the three datasets. The limitation of this paper is that we only studied the statistical inference of the parameters for the HL-INH model using the ML method of estimation under ranked set sampling. For future works, authors can study the statistical inference of the parameters for the new suggested model using different classical and Bayesian estimation approaches; furthermore, they can study the reliability analysis of the new suggested model utilizing different censored schemes.

Author Contributions

Conceptualization, I.E.; Methodology, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E.; Software, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E.; Formal analysis, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E.; Data curation, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E.; Writing—original draft, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E.; Supervision, N.A., M.S., A.S.A.-M., M.E., E.M.A. and I.E. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by Imam Muhammad ibn Saud Islamic University grant number (221412039).

Data Availability Statement

Data sets are available in the application section.

Acknowledgments

The authors extend their appreciation to the Deanship of Scientific Research, Imam Mohammad Ibn Saud Islamic University (IMSIU), Saudi Arabia, for funding this research work through Grant No. (221412039).

Conflicts of Interest

The authors declare no conflict of interest.

Correction Statement

Due to an error in article production, incorrect references were previously listed in the main text. This information has been updated and this change does not affect the scientific content of the article.

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Figure 1. Curves of PDF and HRF for the HL-INH distribution.
Figure 1. Curves of PDF and HRF for the HL-INH distribution.
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Figure 2. Data description for the flood data using box, strip, and violin plots.
Figure 2. Data description for the flood data using box, strip, and violin plots.
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Figure 3. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for the flood data.
Figure 3. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for the flood data.
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Figure 4. Profile likelihood α , γ , and λ for the flood data.
Figure 4. Profile likelihood α , γ , and λ for the flood data.
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Figure 5. Data description for the COVID-19 data using box, strip, and violin plots.
Figure 5. Data description for the COVID-19 data using box, strip, and violin plots.
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Figure 6. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for plots for the COVID-19 data.
Figure 6. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for plots for the COVID-19 data.
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Figure 7. Profile likelihood α , γ , and λ for the COVID-19 data.
Figure 7. Profile likelihood α , γ , and λ for the COVID-19 data.
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Figure 8. Data description for the carbon fibre data using box, strip, and violin plots.
Figure 8. Data description for the carbon fibre data using box, strip, and violin plots.
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Figure 9. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for the carbon fibre data.
Figure 9. Fitting of (I) ecdf, (II) epdf, (III) QQ and (IV) PP plots for the carbon fibre data.
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Figure 10. Profile likelihood α , γ , and λ for the carbon fibre data.
Figure 10. Profile likelihood α , γ , and λ for the carbon fibre data.
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Table 1. Analysis of the REN, HCEN, TEN, and AEN for the HL-INH distribution at λ = 1.5 and η = 0.5 and 0.8.
Table 1. Analysis of the REN, HCEN, TEN, and AEN for the HL-INH distribution at λ = 1.5 and η = 0.5 and 0.8.
α γ η = 0.5 η = 0.8
RENHCENTENAENRENHCENTENAEN
40.50.2702.0850.7300.8640.0840.3350.1980.199
10.6408.1222.1783.3640.4772.1231.2271.263
1.50.83013.9103.2015.7620.6703.1681.8091.884
20.96019.6064.0408.1210.8023.9442.2332.346
2.51.05925.2614.77210.4630.9024.5762.5732.721
31.14030.8945.42912.7970.9825.1132.8613.041
3.51.20836.5156.03115.1251.0505.5853.1103.322
41.26642.1286.59117.4501.1096.0083.3323.573
50.50.1160.7410.2870.307−0.040−0.155−0.092−0.092
10.5015.2461.5632.1730.3661.5760.9170.938
1.50.6959.5412.4513.9520.5632.5721.4781.530
20.82613.7543.1765.6970.6953.3071.8851.967
2.50.92617.9303.8067.4270.7953.9032.2112.322
31.00622.0884.3729.1490.8764.4112.4852.624
3.51.07426.2344.89010.8670.9444.8562.7232.888
41.13330.3735.37012.5811.0035.2542.9353.125
60.50.0040.0210.0090.009−0.135−0.502−0.301−0.299
10.4023.6811.1781.5250.2831.1910.6970.708
1.50.5987.1571.9822.9650.4822.1521.2441.280
20.73010.5582.6364.3730.6152.8591.6381.700
2.50.83013.9263.2035.7680.7163.4311.9532.041
30.91117.2763.7127.1560.7973.9172.2182.33
3.50.98020.6164.1778.5400.8664.3432.4492.583
41.03823.9504.6099.9200.9244.7242.6532.810
Table 2. Analysis of the REN, HCEN, TEN, and AEN for the HL-INH distribution at λ = 1.5 and η = 1.2 and 1.5.
Table 2. Analysis of the REN, HCEN, TEN, and AEN for the HL-INH distribution at λ = 1.5 and η = 1.2 and 1.5.
α γ η = 1.2 η = 1.5
RENHCENTENAENRENHCENTENAEN
40.5−0.021−0.062−0.048−0.048−0.065−0.176−0.156−0.154
10.3851.0620.8130.8250.3470.7970.6580.701
1.50.5811.5451.1741.2000.5431.1640.9301.023
20.7131.8501.4001.4370.6761.3821.0811.214
2.50.8132.0711.5621.6090.7761.5321.1811.346
30.8942.2441.6881.7430.8571.6461.2541.446
3.50.9622.3861.7901.8530.9251.7361.3111.525
41.0212.5041.8761.9450.9841.8101.3561.590
50.5−0.133−0.403−0.315−0.313−0.172−0.483−0.439−0.424
10.2860.8030.6170.6240.2520.6000.5030.527
1.50.4851.3111.0001.0180.4510.9990.8100.878
20.6181.6301.2381.2660.5841.2330.9791.084
2.50.7181.8611.4081.4450.6851.3951.0911.226
30.7992.0411.5401.5850.7661.5171.1721.333
3.50.8672.1871.6471.6990.8341.6141.2341.418
40.9262.3111.7361.7950.8931.6941.2841.488
60.5−0.218−0.676−0.529−0.525−0.255−0.738−0.682−0.649
10.2110.6010.4630.4670.1790.4380.3730.385
1.50.4121.1290.8630.8770.3800.8640.7090.760
20.5451.4581.1101.1330.5141.1130.8930.978
2.50.6461.6971.2871.3180.6151.2851.0151.129
30.7281.8821.4231.4620.6971.4141.1031.242
3.50.7962.0331.5341.5790.7651.5161.1711.332
40.8552.1601.6271.6780.8241.6001.2251.406
Table 3. Numerical results of E ( Y ) , E ( Y 2 ) , E ( Y 3 ) , E ( Y 4 ) , σ 2 , γ 1 , γ 2 , C V , and ID for the HL-INH distribution at λ = 1.5.
Table 3. Numerical results of E ( Y ) , E ( Y 2 ) , E ( Y 3 ) , E ( Y 4 ) , σ 2 , γ 1 , γ 2 , C V , and ID for the HL-INH distribution at λ = 1.5.
α γ E ( Y ) E ( Y 2 ) E ( Y 3 ) E ( Y 4 ) σ 2 γ 1 γ 2 CVID
40.50.4280.3790.86785.6930.1966.2082204.0001.0350.458
11.2902.59910.4431493.0000.9345.1861670.0000.7490.724
1.52.2177.09541.4508305.0002.1794.9921700.0000.6660.983
23.16213.923107.13223,710.0003.9254.9231485.0000.6271.241
2.54.11423.097220.78360,880.0006.1714.8921542.0000.6041.500
35.07034.623395.713119,219.2958.9164.8741441.1200.5891.758
3.56.02848.502645.233228,588.14512.1604.8641485.5100.5782.017
46.98864.735982.655374,735.52315.9034.8571419.8540.5712.276
50.50.3340.2010.2300.6600.0893.90156.8220.8920.266
11.0811.6283.72816.9440.4593.13738.6020.6270.425
1.51.8964.68316.409104.5001.0892.99235.6660.5500.574
22.7309.42744.663367.8011.9732.94134.6690.5150.723
2.53.57215.87394.932960.7513.1102.91834.2130.4940.871
34.41924.026173.6752086.7454.5012.90533.9670.4801.019
3.55.26733.890287.3533998.6766.1442.89733.8190.4711.166
46.11845.465442.4286998.9438.0402.89233.7230.4631.314
60.50.2790.1290.0990.1410.0513.05928.1960.8070.182
10.9531.1882.0215.1860.2802.38718.8500.5560.294
1.51.6983.5589.58436.3890.6742.25917.3780.4840.397
22.4647.29827.045136.7251.2282.21416.8800.4500.498
2.53.23812.42458.719371.4391.9402.19316.6530.4300.599
34.01618.941108.935828.1072.8112.18216.5300.4170.700
3.54.79726.852182.0241616.6533.8412.17516.4570.4090.801
45.57936.157282.3212869.3455.0292.17016.4090.4020.901
Table 4. RSS design with more than one cycle.
Table 4. RSS design with more than one cycle.
Cycle 1Cycle 2 Cycle c
y ( 1 : n ) 1 ( 1 ) ̲ y ( 2 : n ) 1 ( 1 ) y ( n : n ) 1 ( 1 ) y ( 1 : n ) 2 ( 1 ) ̲ y ( 2 : n ) 2 ( 1 ) y ( n : n ) 2 ( 1 ) y ( 1 : n ) c ( 1 ) ̲ y ( 2 : n ) c ( 1 ) y ( n : n ) c ( 1 )
y ( 2 : n ) 2 ( 2 ) y ( 2 : n ) 1 ( 2 ) ̲ y ( n : n ) 1 ( 2 ) y ( 2 : n ) 2 ( 2 ) y ( 2 : n ) 1 ( 2 ) ̲ y ( n : n ) 2 ( 2 ) y ( 2 : n ) c ( 2 ) y ( 2 : n ) c ( 2 ) ̲ y ( n : n ) c ( 2 )
y ( 2 : n ) 1 ( n ) y ( 2 : n ) 1 ( n ) y ( n : n ) 1 ( n ) ̲ y ( 2 : n ) 2 ( n ) y ( 2 : n ) 2 ( n ) y ( n : n ) 2 ( n ) ̲ y ( 2 : n ) c ( n ) y ( 2 : n ) c ( n ) y ( n : n ) c ( n ) ̲
Table 5. MLE under the SRS and RSS of parameters α = 0.75 .
Table 5. MLE under the SRS and RSS of parameters α = 0.75 .
α = 0.7 SRSRSSRSS c = 3
γ , λ n BiasMSEsBiasMSEsBiasMSEsRE1RE2RE3
0.5, 0.66 α 0.34430.51910.14210.14980.04470.03123.4716.644.80
γ 0.76641.16240.41900.41670.21870.16422.797.082.54
λ 0.25781.28970.10820.58620.01860.23682.205.452.48
8 α 0.24960.29900.09670.08600.01110.02193.4813.643.92
γ 0.58560.77190.34340.33440.18790.11722.316.582.85
λ 0.22210.98140.02560.3406−0.00700.23372.884.201.46
12 α 0.14370.15160.02140.02030.01120.01297.4711.711.57
γ 0.42650.51610.20310.12690.08400.04104.0712.603.10
λ 0.18030.7201−0.06160.12540.02910.12155.745.931.03
17 α 0.09200.10890.01020.01330.00560.00388.1828.813.52
γ 0.41460.48750.16450.09980.04580.01734.8928.105.75
λ 0.17220.7018−0.03140.1236−0.01490.03845.6818.283.22
0.5, 36 α 0.30480.58060.11820.09000.04200.01826.4531.994.96
γ 0.84841.81930.25020.29800.11360.07036.1025.864.24
λ −0.54882.9406−0.21421.1465−0.18040.66452.564.431.73
8 α 0.18030.18430.08670.06040.02390.00943.0519.606.43
γ 0.70251.27270.21570.19790.03380.01266.43100.7815.67
λ −0.64032.7989−0.35561.0682−0.04820.17182.6216.306.22
12 α 0.10090.08910.02940.01370.01130.00436.5220.593.16
γ 0.43080.75040.10610.05910.01980.007812.7096.487.60
λ −0.40681.9500−0.27620.5721−0.05070.11763.4116.594.87
17 α 0.04920.04020.02240.00950.01060.00194.2421.625.10
γ 0.33080.47160.05930.02400.01130.003719.69128.376.52
λ −0.40431.9017−0.07260.4903−0.01610.02323.8881.8421.10
3, 0.66 α 0.40530.93900.14440.11970.05880.02277.8441.315.27
γ 0.48221.25080.16140.31040.08210.28424.034.401.09
λ 0.46961.15720.17160.23980.10460.13074.838.861.83
8 α 0.24900.24690.11150.07290.02780.01133.3921.796.43
γ 0.36910.91750.19120.27350.03880.08733.3510.513.13
λ 0.32450.69200.09570.10020.03750.04176.9116.592.40
12 α 0.15370.12820.04790.01730.01680.00527.4024.513.31
γ 0.17900.85330.09420.2374−0.01590.07303.5911.693.25
λ 0.30460.68960.06700.07330.04480.03779.4118.281.94
17 α 0.08940.05940.02710.00780.01240.00227.5826.573.51
γ 0.19560.68490.06370.09730.01220.04837.0414.172.01
λ 0.22180.59100.02420.01550.01350.007538.2078.972.07
3, 36 α 0.37240.90020.13150.10000.05250.01919.0047.135.24
γ 1.19943.03710.55781.07980.29480.54272.815.601.99
λ 0.51402.24460.17071.08380.13530.80422.072.791.35
8 α 0.22660.20630.10590.06690.02530.01033.0919.996.48
γ 0.94392.38140.37880.84800.19620.28662.818.312.96
λ 0.29491.68750.11590.5516−0.01770.34183.064.941.61
12 α 0.12980.10200.04440.01600.01360.00456.3622.543.54
γ 0.64871.66060.26130.47540.08920.13433.4912.363.54
λ 0.19061.40160.06090.51000.00180.17462.758.032.92
17 α 0.07510.04470.02610.00730.01190.00206.0921.863.59
γ 0.59691.56320.11620.14510.03510.084210.7818.561.72
λ 0.12891.04840.01640.08940.01410.071211.7214.721.26
Table 6. MLE under the SRS and RSS of parameters α = 2.5 .
Table 6. MLE under the SRS and RSS of parameters α = 2.5 .
α = 2.5 SRSRSSRSS c = 3
γ , λ n BiasMSEsBiasMSEsBiasMSEsRE1RE2RE3
0.5, 0.66 α 0.26040.85750.02230.12640.01890.11586.78557.40561.0914
γ 0.43250.42840.18560.12220.07880.03223.506613.30143.7933
λ −0.12030.2945−0.09730.0999−0.02950.06732.94724.37541.4846
8 α 0.17470.80020.02120.1148−0.01300.01856.972243.25616.2041
γ 0.33210.27500.18410.12040.03880.01262.283521.76909.5332
λ −0.10620.2510−0.03900.0915−0.03930.02612.74239.61463.5060
12 α 0.12470.5156−0.03610.1138−0.02270.01674.528730.88146.8191
γ 0.21460.22580.09010.03290.02900.00896.856325.23933.6812
λ −0.05560.1729−0.07730.0615−0.02670.02572.80936.72522.3939
17 α −0.04420.19000.02730.03330.00180.00735.711625.94084.5417
γ 0.17830.11250.03320.00980.01420.002611.487343.51743.7883
λ −0.10140.0970−0.02080.0338−0.01980.00882.871611.04553.8464
0.5, 36 α 0.69441.95150.26780.65470.15660.19782.98089.86723.3103
γ 0.24690.32020.05820.02810.02650.005411.379358.84205.1710
λ −0.53501.1013−0.17650.2926−0.07100.11513.76389.56792.5421
8 α 0.61251.47210.24080.46070.03550.09503.195415.49414.8489
γ 0.13850.09040.03150.01000.01090.00329.046427.95503.0902
λ −0.34910.7967−0.07510.2688−0.06720.06132.964412.99084.3822
12 α 0.40170.91240.13750.21510.05210.09124.242610.00752.3588
γ 0.09660.07010.02250.00470.01030.002214.960331.69542.1186
λ −0.16010.7151−0.08000.2146−0.02080.06123.332111.68353.5064
17 α 0.18390.52610.03790.04180.02950.035112.596214.97781.1891
γ 0.08080.04890.00480.00110.00670.000943.218855.28681.2792
λ −0.27460.5518−0.01980.0059−0.01420.005693.967998.40081.0472
3, 0.66 α 1.02523.54610.45451.15310.24260.45633.07537.77062.5268
γ 0.30680.59230.14840.15870.07430.06253.73249.47702.5391
λ 0.14180.29580.02240.02200.01500.007913.435037.64762.8022
8 α 0.81792.38240.23730.44840.09770.19725.313212.08122.2738
γ 0.21690.36020.03220.12220.01980.05542.94886.49732.2034
λ 0.09380.19050.02040.02110.01060.00739.036226.11802.8904
12 α 0.58301.57790.18650.33270.02630.05664.742927.90305.8831
γ 0.13750.13970.12850.12040.00670.00281.160250.069443.1558
λ 0.08600.1281−0.00050.0118−0.00030.001110.8728113.413410.4309
17 α 0.38140.85030.10940.15410.06160.04555.517018.69873.3893
γ 0.14480.11420.04270.0500−0.04600.00272.284442.929118.7925
λ 0.07170.11500.00440.00530.02360.001021.6820119.63835.5179
3, 36 α 1.62859.59290.69782.61520.27300.47113.668120.36305.5514
γ 1.16813.14330.33650.57410.28320.56305.47545.58341.0197
λ −0.02412.01580.01130.50140.01620.46294.02044.35491.0832
8 α 1.10454.42070.48811.47930.11310.23502.988418.80806.2936
γ 0.85902.16160.40070.50790.09730.11014.255819.64144.6152
λ 0.01331.8999−0.06490.4786−0.03320.13253.969414.33463.6113
12 α 0.66652.48060.19880.33920.07020.11487.312721.60712.9547
γ 0.55761.36830.16160.16610.03710.09108.236215.03561.8256
λ 0.01791.2303−0.04890.16380.02370.11587.512510.62551.4144
17 α 0.39541.09980.11700.16980.05210.04306.476525.58333.9502
γ 0.36460.76320.32810.15830.01540.01694.822245.14289.3615
λ 0.03010.9246−0.02210.94950.00910.01500.973861.460263.1151
Table 7. Confidence intervals with CP for the parameters of the HL-INH distribution: α = 0.7 .
Table 7. Confidence intervals with CP for the parameters of the HL-INH distribution: α = 0.7 .
α = 0.7 SRSRSSRSS c = 3
γ , λ n L-ACIU-ACICPL-ACIU-ACICPL-ACIU-ACICP
0.5, 0.66 α 0.09822.286994.67%0.13541.548894.33%0.40921.080296.67%
γ 0.12222.755297.67%0.20451.883098.00%0.04901.388594.33%
λ 0.23143.029294.67%0.27802.196394.33%0.27351.510696.67%
8 α 0.10561.904793.67%0.25321.340195.00%0.42121.001096.00%
γ 0.13202.371597.33%0.14071.756995.67%0.12611.249896.33%
λ 0.30732.717693.67%0.31521.770495.00%0.35591.541996.00%
12 α 0.13321.554296.00%0.44500.997994.33%0.48890.933596.67%
γ 0.14212.061495.67%0.12861.277694.00%0.22250.945696.67%
λ 0.31852.408396.00%0.35151.222994.33%0.35281.538096.67%
17 α 0.16991.414294.67%0.48450.935995.67%0.58540.825894.33%
γ 0.15882.017596.00%0.13521.193995.67%0.30340.788295.67%
λ 0.32122.752494.67%0.36151.289695.67%0.20150.968794.33%
0.5, 36 α 0.13662.375996.00%0.27691.359594.67%0.49070.993396.00%
γ 0.17103.407194.67%0.20251.702893.33%0.14301.084296.33%
λ 0.27385.640896.00%0.72614.845594.67%1.25894.380396.00%
8 α 0.11551.645194.33%0.33521.238294.33%0.53940.908395.33%
γ 0.28532.935695.00%0.30481.479595.00%0.32340.744296.67%
λ 0.29675.394294.33%0.73924.549794.33%2.14373.760095.33%
12 α 0.24941.352496.00%0.50730.951596.00%0.58410.838594.67%
γ 0.30542.406293.00%0.17661.035695.67%0.35110.688597.67%
λ 0.30295.215996.00%1.34144.106296.00%2.28353.615194.67%
17 α 0.36771.130795.33%0.53650.908495.33%0.62850.792694.33%
γ 0.35082.012493.00%0.27870.840097.33%0.39440.628298.33%
λ 0.31085.268495.33%1.06704.787995.33%2.68633.281594.33%
3, 0.66 α 0.16232.833496.67%0.22691.461894.67%0.48621.031495.67%
γ 1.50105.463492.33%2.11454.208493.00%2.04794.116391.67%
λ 0.18312.969796.67%0.19291.672094.67%0.12531.384095.67%
8 α 0.10481.793294.67%0.32861.294394.67%0.52610.929596.00%
γ 1.63375.104594.33%2.09384.288692.00%2.46363.614094.33%
λ 0.19582.428494.67%0.10321.288194.67%0.24331.031796.00%
12 α 0.21891.488695.67%0.50730.988695.00%0.57870.854995.33%
γ 1.72955.063492.33%2.15584.032692.33%2.16813.800191.00%
λ 0.20782.675995.67%0.15201.181995.00%0.27381.015995.33%
17 α 0.34411.234795.33%0.56160.892795.33%0.62270.802095.00%
γ 1.86174.774390.00%2.46413.663494.00%2.58133.443294.00%
λ 0.30622.266995.33%0.38460.863795.33%0.44570.781295.00%
3, 36 α −0.64092.785697.00%0.26681.396294.67%0.50141.003597.00%
γ 1.71726.681695.33%1.83655.279094.67%1.96934.620294.33%
λ 0.75126.276997.00%1.15455.186994.67%1.39484.875797.00%
8 α 0.15371.699594.67%0.34261.269195.33%0.53210.918596.33%
γ 1.54706.340896.00%1.73095.026794.00%2.21824.174192.67%
λ 0.81115.778794.67%1.67564.556295.33%1.83514.129596.33%
12 α 0.25671.402896.33%0.51140.977395.33%0.58420.842995.00%
γ 1.46265.834794.00%2.00864.514093.00%2.39133.787193.33%
λ 0.89675.484696.33%1.54554.576395.33%2.18133.822295.00%
17 α 0.38701.163196.00%0.56590.886395.00%0.62620.797594.33%
γ 1.44015.753793.33%2.40413.828396.33%2.46963.600792.00%
λ 0.75085.507196.00%2.43023.602695.00%2.35783.724594.33%
Table 8. Confidence intervals with CP for the parameters of the HL-INH distribution: α = 2.5 .
Table 8. Confidence intervals with CP for the parameters of the HL-INH distribution: α = 2.5 .
α = 2.5 SRSRSSRSS c = 3
γ , λ n L-ACIU-ACICPL-ACIU-ACICPL-ACIU-ACICP
0.5, 0.66 α 1.01584.505096.67%1.82583.218893.33%1.82893.349393.67%
γ 0.09321.897195.67%0.10411.267194.33%0.26230.895495.33%
λ 0.05591.518696.67%0.08771.093293.33%0.06451.076593.67%
8 α 0.73964.609899.67%1.28303.954896.67%2.22122.752896.00%
γ 0.03531.629096.33%0.15751.943799.33%0.33180.745996.33%
λ 0.10891.880299.67%0.20201.323996.67%0.25300.868496.00%
12 α 1.23644.013092.33%1.80533.122694.33%1.97132.983494.33%
γ 0.12511.546997.33%0.28080.899497.00%0.35230.705895.33%
λ 0.12651.353492.33%0.05990.985594.33%0.25440.892294.33%
17 α 1.60453.307191.67%2.17332.881397.00%2.33392.669896.67%
γ 0.12071.235994.33%0.35030.716296.67%0.41840.610095.33%
λ 0.13081.076891.67%0.22060.937797.00%0.40030.760096.67%
0.5, 36 α 0.81465.574295.33%1.26884.266893.67%1.83943.473894.33%
γ 0.12531.746692.67%0.24940.867196.00%0.39140.661795.67%
λ 0.69254.237595.33%1.81963.827393.67%2.27773.580394.33%
8 α 1.05635.168794.67%1.49493.986794.67%1.93443.136695.33%
γ 0.11441.162695.67%0.34510.717897.00%0.40130.620597.33%
λ 1.03814.263794.67%1.91783.931994.67%2.46483.400795.33%
12 α 1.20024.603194.67%1.76803.507095.00%1.88793.216495.33%
γ 0.11261.080696.33%0.39550.649496.00%0.42030.600496.00%
λ 0.75754.922494.67%2.02423.815995.00%1.85144.107195.33%
17 α 1.30634.061497.33%2.14372.932293.67%2.16612.892995.00%
γ 0.17660.985195.67%0.43940.570296.00%0.44980.563694.00%
λ 1.37034.080497.33%2.83493.125593.67%2.42583.490395.00%
3, 0.66 α 0.42416.626496.67%1.04454.864594.33%1.50473.980496.33%
γ 1.92104.692692.33%2.42253.874293.67%2.60563.542993.33%
λ 0.28901.772796.67%0.33440.910494.33%0.44350.786596.33%
8 α 0.74815.887895.33%1.50793.966697.00%1.74723.448196.67%
γ 2.11824.315694.00%2.34893.715595.00%2.55913.480494.33%
λ 0.29141.530795.33%0.30011.282597.00%0.42130.799996.67%
12 α 0.89855.267595.67%1.61503.758196.00%2.06232.990394.67%
γ 1.93014.344994.00%2.43313.824096.00%2.90393.109694.33%
λ 0.00391.368195.67%0.38640.812696.00%0.53370.665794.67%
17 α 1.23334.529695.67%1.86923.349695.33%2.16082.962495.67%
γ 1.90134.388293.33%2.61183.473795.67%2.45753.450594.67%
λ 0.02111.322395.67%0.46170.747195.33%0.47770.769695.67%
3, 36 α 0.04399.300995.33%0.33366.062094.67%1.53674.009394.67%
γ 1.54976.786697.00%2.00384.669394.00%1.91904.647397.00%
λ 0.18895.762995.33%1.62134.401394.67%1.45964.572894.67%
8 α 0.09207.116993.00%0.80105.175295.33%1.68753.538696.00%
γ 1.51646.201697.67%1.84204.959596.00%2.47463.719996.67%
λ 0.30735.719293.00%1.19904.671395.33%2.25503.678596.00%
12 α 0.36485.968196.33%1.62403.773696.67%1.91943.221095.33%
γ 1.53885.576497.00%2.42703.896296.00%2.44933.624895.00%
λ 0.84055.195396.33%2.16243.739896.67%2.19403.853495.33%
17 α 0.98854.802495.67%1.84133.392895.67%2.15812.946195.67%
γ 1.80604.923296.33%1.66344.992898.67%2.76193.268994.00%
λ 1.14324.917095.67%1.06534.890595.67%2.76893.249295.67%
Table 9. MLE for each model with different measures: flood data.
Table 9. MLE for each model with different measures: flood data.
EstimatesSEM1M2M3M4M5M6M7M8
HL-INH α 2.93130.4873436.4053436.9987442.0669438.57470.02280.16080.05980.9954
γ 376.47446103.8330
λ 0.08681.4100
OLINH α 2.87051.8291437.9109438.8411445.3957440.73940.02370.17260.06430.9888
β 1.27681.2160
λ 0.59660.5223
θ 59.552251.3453
PINH α 2.14181.1729436.4633437.0096442.0269438.63460.02430.16690.06700.9823
β 562.8134638.9703
γ 2.06110.2153
INH γ 868.54193765.7212453.6735453.9402457.4159455.08780.02830.30060.24380.0067
λ 0.03220.1398
EOWINH α 1.80630.8672439.4286440.3589446.9134442.25720.02730.19220.06100.9941
β 0.81040.8693
γ 19.07637.2102
λ 1.20524.5071
MOINH α 5.36848.3880439.9131440.4585445.5267442.03450.05550.36170.07000.9727
β 8.765716.5036
γ 0.17510.1106
EW α 0.22270.0072466.2669466.8123471.8805468.38830.40232.42140.18270.0813
β 0.00500.0013
θ 0.05620.0279
EL α 47.010792.6907437.1066437.6520442.7202439.22790.02630.18740.06140.9935
β 3.45591.6865
θ 17.598828.6909
GL α 1.10371.7143438.2232439.1534445.7080441.05170.02390.16580.06990.9731
β 8.591149.4043
θ 0.43550.4307
λ 41.2152498.9307
WL α 25.362793.1384452.5347453.4650460.0195455.36330.18971.22340.12640.4270
β 3.74051.4798
θ 0.16510.1322
λ 7.612810.6009
Table 10. MLE for each model with different measures: COVID-19 data.
Table 10. MLE for each model with different measures: COVID-19 data.
EstimatesSEM1M2M3M4M5M6M7M8
HL-INH α 15.378529.9414−387.0614−386.7537−379.8412−384.16260.01350.12870.03980.9995
γ 0.29840.1454
λ 2.09658.1945
OLINH α 20.012835.5663−383.8202−383.3007−374.1933−379.95520.02860.24650.05730.9509
β 11.329917.0058
λ 0.11020.0949
θ 0.48620.0876
PINH α 0.15110.0954−385.8691−385.5614−378.6489−382.97030.02310.21340.04510.9963
β 0.00010.0008
γ 3.44851.0951
INH γ 0.78080.1283−363.0467−362.8948−358.2333−361.11420.23821.62340.13640.0944
λ 0.02420.0074
EOWINH α 1.67141.1690−385.0412−384.5217−375.4143−381.17610.01370.12990.04170.9988
β 0.32990.4791
γ 0.33320.2501
λ 0.12350.1712
MOINH α 0.28890.0238−373.1607−372.8530−365.9406−370.26190.17031.11570.07250.7813
β 14.36359.7515
γ 0.00510.0022
EW α 1.25180.1027−383.0809−382.7732−375.8607−380.18210.05520.39090.05720.9510
β 108.82495.0239
θ 191.799662.5018
EL α 1.97350.4825−386.9522−386.6445−379.7320−384.05340.01430.13010.04320.9980
β 8.02628.3354
θ 0.16500.2126
GL α 20.264626.5200−384.8166−384.2971−375.1897−380.95150.01800.16310.04180.9988
β 0.19180.3158
θ 2.08040.6499
λ 2.43900.9729
WL α 6.634919.1434−384.8288−384.3093−375.2019−380.96380.01440.12970.04170.9988
β 1.85510.4084
θ 0.25590.2911
λ 0.01560.0113
Table 11. SRS and RSS for the flood data.
Table 11. SRS and RSS for the flood data.
n 123456789101112131415
17SRS 21.8224.88831.531.532.640.442.2544.0250.3361.7475.884.1
RSS c = 1c = 121.8227.534.432.639.239.257.2265.59765.4484.175.866
RSS c = 3c = 127.544.0232.675.8
c = 2 40.444.0232.684.1
c = 3 24.88832.661.7444.02
15SRS 21.8224.88827.531.531.532.640.442.2544.0244.0244.7350.3361.7475.884.1
RSS c = 1c = 123.728.130.3830.3828.138.140.458.844.7344.944.0284.175.8121.9784.1
RSS c = 3c = 131.532.650.3344.958.8
c = 2 21.8231.542.2575.844.73
c = 3 27.531.542.2544.7375.8
Table 12. MLE for SRS and RSS of the flood data.
Table 12. MLE for SRS and RSS of the flood data.
SRSRSS c = 1RSS c = 3
n EstimatesSEEstimatesSEEstimatesSE
12 α 3.90301.86203.24240.39374.31220.2669
γ 376.4743208.1903376.4824203.5782376.4811174.4104
λ 0.09371.29850.09850.17420.09910.1691
15 α 4.41952.02932.99630.23295.33640.0921
γ 376.4737121.7994376.476391.5062376.454545.1077
λ 0.09710.81300.09050.05300.10610.0255
Table 13. SRS and RSS for the COVID-19 data.
Table 13. SRS and RSS for the COVID-19 data.
n1218
SRSRSS c = 1RSS c = 3SRSRSS c = 1RSS c = 3
i c = 1c = 1c = 2c = 3 c = 1c = 1c = 2c = 3
10.00910.00230.0162 0.00690.00460.0091
20.01150.01620.0116 0.00910.01160.0162
30.01150.00930.0162 0.00910.01110.0207
40.01620.01160.0588 0.01150.01190.0349
50.01620.02080.0521 0.01150.01590.0394
60.02070.0255 0.0116 0.01620.02080.1343
70.02750.0225 0.0346 0.01620.0255 0.0069
80.02950.0295 0.0115 0.02070.0275 0.0162
90.03460.0208 0.0295 0.02750.023 0.0207
100.03490.0275 0.0988 0.02750.023 0.0239
110.03940.0314 0.00910.02950.0255 0.0521
120.05210.0412 0.01620.03460.0379 0.096
130.05880.0685 0.05210.03490.0275 0.0115
140.06790.0394 0.03490.03940.0468 0.0091
150.09880.1343 0.03940.05210.0501 0.0162
16 0.05880.0394 0.0163
17 0.06790.1343 0.0679
18 0.09880.0942 0.1343
Table 14. MLE for the SRS and RSS of the COVID-19 data.
Table 14. MLE for the SRS and RSS of the COVID-19 data.
SRSRSS c = 1RSS c = 3
n EstimatesSEEstimatesSEEstimatesSE
15 α 3.966360.849410.785731.53712.48271.1644
γ 0.73961.60070.37470.04201.01010.0394
λ 0.06530.08380.59890.07310.02510.0009
18 α 3.270112.03563.18131.27171.88000.1719
γ 0.74060.55930.81600.03861.56850.0279
λ 0.04880.01530.04270.00120.01090.00005
Table 15. Data summarized.
Table 15. Data summarized.
DataMinQ1MedianMeanQ3Max σ 2 γ 1 γ 2
I19.88530.33540.40051.49561.335185.5601048.2592.0697.951
II0.0020.0140.0270.0360.0460.1780.0012.0218.176
III0.3121.0981.4781.4511.7732.5850.245−0.0282.941
Table 16. MLE for each model with different measures: carbon fibre data.
Table 16. MLE for each model with different measures: carbon fibre data.
EstimatesSEM1M2M3M4M5M6M7M8
HLINH α 199.000427.8633106.8813107.2505113.5836109.54030.05460.42840.06140.9574
γ 0.44050.0814
λ 87.71809.2797
OLINH α 270.42225.1566113.8216114.4466122.7580117.36700.10680.76760.10200.4697
β 2.29280.1464
λ 40.29907.3892
θ 0.53060.0288
PINH α 0.18670.0325113.8216114.4466122.7580117.36700.10680.76760.10200.4697
β 82.176061.6231
γ 5.99970.9364
INH γ 3.60782.0237185.1993185.3811189.6675186.97200.85925.17730.31760.0000
λ 0.24020.1612
MOINH α 0.60190.0488135.2326135.6019141.9350137.89170.40462.58560.13030.1917
β 30.35949.3200
γ 0.00370.0012
EL α 9.18322.2274120.7969121.1661127.4992123.45590.22161.49640.11340.3374
β 41.543234.0397
θ 20.914918.1903
GL α 88.468885.2253119.7791120.4041128.7155123.32450.19031.28780.10020.4926
β 14.501111.9328
θ 2.68881.0941
λ 13.54033.1472
Table 17. SRS and RSS for the carbon fibre data.
Table 17. SRS and RSS for the carbon fibre data.
iSRSRSSRSS
c = 1c = 1c = 2c = 3c = 4
10.8610.3120.865
20.8610.5520.944
30.8610.8651.14
40.9440.8651.24
50.9440.8611.684
60.9441.241.697
71.0211.0211.818
81.0211.098 0.803
91.0271.27 0.552
101.2531.274 1.301
111.2721.434 1.24
121.2741.382 2.128
131.3011.382 1.88
141.3821.382 2.233
151.4261.511 0.7
161.491.535 1.224
171.5661.426 1.274
181.571.77 1.478
191.571.514 1.648
201.5861.809 1.818
211.5861.697 2.067
221.7261.77 0.803
231.772.012 0.7
241.81.88 1.24
251.8482.084 1.514
262.0122.096 1.848
272.4331.88 1.697
282.5852.585 2.09
Table 18. MLE for the SRS and RSS of the carbon fibre data.
Table 18. MLE for the SRS and RSS of the carbon fibre data.
SRSRSS c = 1RSS c = 3
n EstimatesSEEstimatesSEEstimatesSE
28 α 204.192328.1256250.096925.1562265.076815.1517
γ 0.50840.10550.45540.03040.44220.0217
λ 50.05749.102684.36805.151794.87562.2562
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Alotaibi, N.; Al-Moisheer, A.S.; Elbatal, I.; Shrahili, M.; Elgarhy, M.; Almetwally, E.M. Half Logistic Inverted Nadarajah–Haghighi Distribution under Ranked Set Sampling with Applications. Mathematics 2023, 11, 1693. https://doi.org/10.3390/math11071693

AMA Style

Alotaibi N, Al-Moisheer AS, Elbatal I, Shrahili M, Elgarhy M, Almetwally EM. Half Logistic Inverted Nadarajah–Haghighi Distribution under Ranked Set Sampling with Applications. Mathematics. 2023; 11(7):1693. https://doi.org/10.3390/math11071693

Chicago/Turabian Style

Alotaibi, Naif, A. S. Al-Moisheer, Ibrahim Elbatal, Mansour Shrahili, Mohammed Elgarhy, and Ehab M. Almetwally. 2023. "Half Logistic Inverted Nadarajah–Haghighi Distribution under Ranked Set Sampling with Applications" Mathematics 11, no. 7: 1693. https://doi.org/10.3390/math11071693

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