Shifted log-logistic distribution

Shifted log-logistic
Probability density function

values of as shown in legend
Cumulative distribution function

values of as shown in legend
Parameters

location (real)
scale (real)

shape (real)
Support



PDF


where
CDF


where
Mean


where
Median
Mode
Variance


where

The shifted log-logistic distribution is a probability distribution also known as the generalized log-logistic or the three-parameter log-logistic distribution.[1][2] It has also been called the generalized logistic distribution,[3] but this conflicts with other uses of the term: see generalized logistic distribution.

Definition

The shifted log-logistic distribution can be obtained from the log-logistic distribution by addition of a shift parameter . Thus if has a log-logistic distribution then has a shifted log-logistic distribution. So has a shifted log-logistic distribution if has a logistic distribution. The shift parameter adds a location parameter to the scale and shape parameters of the (unshifted) log-logistic.

The properties of this distribution are straightforward to derive from those of the log-logistic distribution. However, an alternative parameterisation, similar to that used for the generalized Pareto distribution and the generalized extreme value distribution, gives more interpretable parameters and also aids their estimation.

In this parameterisation, the cumulative distribution function (CDF) of the shifted log-logistic distribution is

for , where is the location parameter, the scale parameter and the shape parameter. Note that some references use to parameterise the shape.[3][4]

The probability density function (PDF) is

again, for

The shape parameter is often restricted to lie in [-1,1], when the probability density function is bounded. When , it has an asymptote at . Reversing the sign of reflects the pdf and the cdf about .

Applications

The three-parameter log-logistic distribution is used in hydrology for modelling flood frequency.[3][4][5]

Alternate parameterization

An alternate parameterization with simpler expressions for the PDF and CDF is as follows. For the shape parameter , scale parameter and location parameter , the PDF is given by [6][7]

The CDF is given by

The mean is and the variance is , where .[7]

References

  1. Venter, Gary G. (Spring 1994), "Introduction to selected papers from the variability in reserves prize program" (PDF), Casualty Actuarial Society Forum, 1: 91–101
  2. Geskus, Ronald B. (2001), "Methods for estimating the AIDS incubation time distribution when date of seroconversion is censored", Statistics in Medicine, 20 (5): 795–812, doi:10.1002/sim.700, PMID 11241577
  3. 1 2 3 Hosking, Jonathan R. M.; Wallis, James R (1997), Regional Frequency Analysis: An Approach Based on L-Moments, Cambridge University Press, ISBN 0-521-43045-3
  4. 1 2 Robson, A.; Reed, D. (1999), Flood Estimation Handbook, 3: "Statistical Procedures for Flood Frequency Estimation", Wallingford, UK: Institute of Hydrology, ISBN 0-948540-89-3
  5. Ahmad, M. I.; Sinclair, C. D.; Werritty, A. (1988), "Log-logistic flood frequency analysis", Journal of Hydrology, 98 (3–4): 205–224, doi:10.1016/0022-1694(88)90015-7
  6. "EasyFit - Log-Logistic Distribution". Retrieved 1 October 2016.
  7. 1 2 "Guide to Using - RISK7_EN.pdf" (PDF). Retrieved 1 October 2016.
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