Parameters | — stability parameter Contents— location parameter | ||
---|---|---|---|
Support | , or if and , or if and | ||
not analytically expressible, except for some parameter values | |||
CDF | not analytically expressible, except for certain parameter values | ||
Median | when | ||
Mode | when | ||
Variance | when , otherwise infinite | ||
Skewness | when , otherwise undefined | ||
Ex. kurtosis | when , otherwise undefined | ||
MGF | undefined | ||
CF | , |
A geometric stable distribution or geo-stable distribution is a type of leptokurtic probability distribution. Geometric stable distributions were introduced in Klebanov, L. B., Maniya, G. M., and Melamed, I. A. (1985). A problem of Zolotarev and analogs of infinitely divisible and stable distributions in a scheme for summing a random number of random variables. [1] These distributions are analogues for stable distributions for the case when the number of summands is random, independent of the distribution of summand, and having geometric distribution. The geometric stable distribution may be symmetric or asymmetric. A symmetric geometric stable distribution is also referred to as a Linnik distribution. [2] The Laplace distribution and asymmetric Laplace distribution are special cases of the geometric stable distribution. The Mittag-Leffler distribution is also a special case of a geometric stable distribution. [3]
The geometric stable distribution has applications in finance theory. [4] [5] [6] [7]
For most geometric stable distributions, the probability density function and cumulative distribution function have no closed form. However, a geometric stable distribution can be defined by its characteristic function, which has the form: [8]
where .
The parameter , which must be greater than 0 and less than or equal to 2, is the shape parameter or index of stability, which determines how heavy the tails are. [8] Lower corresponds to heavier tails.
The parameter , which must be greater than or equal to −1 and less than or equal to 1, is the skewness parameter. [8] When is negative the distribution is skewed to the left and when is positive the distribution is skewed to the right. When is zero the distribution is symmetric, and the characteristic function reduces to: [8]
The symmetric geometric stable distribution with is also referred to as a Linnik distribution. [9] A completely skewed geometric stable distribution, that is, with , , with is also referred to as a Mittag-Leffler distribution. [10] Although determines the skewness of the distribution, it should not be confused with the typical skewness coefficient or 3rd standardized moment, which in most circumstances is undefined for a geometric stable distribution.
The parameter is referred to as the scale parameter, and is the location parameter. [8]
When = 2, = 0 and = 0 (i.e., a symmetric geometric stable distribution or Linnik distribution with =2), the distribution becomes the symmetric Laplace distribution with mean of 0, [9] which has a probability density function of:
The Laplace distribution has a variance equal to . However, for the variance of the geometric stable distribution is infinite.
A stable distribution has the property that if are independent, identically distributed random variables taken from such a distribution, the sum has the same distribution as the 's for some and .
Geometric stable distributions have a similar property, but where the number of elements in the sum is a geometrically distributed random variable. If are independent and identically distributed random variables taken from a geometric stable distribution, the limit of the sum approaches the distribution of the 's for some coefficients and as p approaches 0, where is a random variable independent of the 's taken from a geometric distribution with parameter p. [5] In other words:
The distribution is strictly geometric stable only if the sum equals the distribution of the 's for some a. [4]
There is also a relationship between the stable distribution characteristic function and the geometric stable distribution characteristic function. The stable distribution has a characteristic function of the form:
where
The geometric stable characteristic function can be expressed in terms of a stable characteristic function as: [11]
In probability theory and statistics, the exponential distribution is the probability distribution of the time between events in a Poisson point process, i.e., a process in which events occur continuously and independently at a constant average rate. It is a particular case of the gamma distribution. It is the continuous analogue of the geometric distribution, and it has the key property of being memoryless. In addition to being used for the analysis of Poisson point processes it is found in various other contexts.
In probability theory and statistics, the beta distribution is a family of continuous probability distributions defined on the interval [0, 1] parameterized by two positive shape parameters, denoted by alpha (α) and beta (β), that appear as exponents of the random variable and control the shape of the distribution. The generalization to multiple variables is called a Dirichlet distribution.
In probability theory, a compound Poisson distribution is the probability distribution of the sum of a number of independent identically-distributed random variables, where the number of terms to be added is itself a Poisson-distributed variable. In the simplest cases, the result can be either a continuous or a discrete distribution.
In probability theory and statistics, the Laplace distribution is a continuous probability distribution named after Pierre-Simon Laplace. It is also sometimes called the double exponential distribution, because it can be thought of as two exponential distributions spliced together back-to-back, although the term is also sometimes used to refer to the Gumbel distribution. The difference between two independent identically distributed exponential random variables is governed by a Laplace distribution, as is a Brownian motion evaluated at an exponentially distributed random time. Increments of Laplace motion or a variance gamma process evaluated over the time scale also have a Laplace distribution.
In probability theory, a distribution is said to be stable if a linear combination of two independent random variables with this distribution has the same distribution, up to location and scale parameters. A random variable is said to be stable if its distribution is stable. The stable distribution family is also sometimes referred to as the Lévy alpha-stable distribution, after Paul Lévy, the first mathematician to have studied it.
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Financial models with long-tailed distributions and volatility clustering have been introduced to overcome problems with the realism of classical financial models. These classical models of financial time series typically assume homoskedasticity and normality cannot explain stylized phenomena such as skewness, heavy tails, and volatility clustering of the empirical asset returns in finance. In 1963, Benoit Mandelbrot first used the stable distribution to model the empirical distributions which have the skewness and heavy-tail property. Since -stable distributions have infinite -th moments for all , the tempered stable processes have been proposed for overcoming this limitation of the stable distribution.
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The multivariate stable distribution is a multivariate probability distribution that is a multivariate generalisation of the univariate stable distribution. The multivariate stable distribution defines linear relations between stable distribution marginals. In the same way as for the univariate case, the distribution is defined in terms of its characteristic function.
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In probability theory and statistics, the noncentral beta distribution is a continuous probability distribution that is a noncentral generalization of the (central) beta distribution.
In queueing theory, a discipline within the mathematical theory of probability, a fluid queue is a mathematical model used to describe the fluid level in a reservoir subject to randomly determined periods of filling and emptying. The term dam theory was used in earlier literature for these models. The model has been used to approximate discrete models, model the spread of wildfires, in ruin theory and to model high speed data networks. The model applies the leaky bucket algorithm to a stochastic source.
In probability theory and statistics, the asymmetric Laplace distribution (ALD) is a continuous probability distribution which is a generalization of the Laplace distribution. Just as the Laplace distribution consists of two exponential distributions of equal scale back-to-back about x = m, the asymmetric Laplace consists of two exponential distributions of unequal scale back to back about x = m, adjusted to assure continuity and normalization. The difference of two variates exponentially distributed with different means and rate parameters will be distributed according to the ALD. When the two rate parameters are equal, the difference will be distributed according to the Laplace distribution.