Lognormal3.RdDensity, distribution function, quantile function, and random generation
for the three-parameter lognormal distribution with parameters meanlog,
sdlog, and threshold.
dlnorm3(x, meanlog = 0, sdlog = 1, threshold = 0)
plnorm3(q, meanlog = 0, sdlog = 1, threshold = 0)
qlnorm3(p, meanlog = 0, sdlog = 1, threshold = 0)
rlnorm3(n, meanlog = 0, sdlog = 1, threshold = 0)vector of quantiles.
vector of quantiles.
vector of probabilities between 0 and 1.
sample size. If length(n) is larger than 1, then length(n)
random values are returned.
vector of means of the distribution of the random variable on the log scale.
The default is meanlog=0.
vector of (positive) standard deviations of the random variable on the log scale.
The default is sdlog=1.
vector of thresholds of the random variable on the log scale. The default
is threshold=0.
The three-parameter lognormal distribution is simply the usual two-parameter lognormal distribution with a location shift.
Let \(X\) be a random variable with a three-parameter lognormal distribution
with parameters meanlog=\(\mu\), sdlog=\(\sigma\), and
threshold=\(\gamma\). Then the random variable \(Y = X - \gamma\)
has a lognormal distribution with parameters
meanlog=\(\mu\) and sdlog=\(\sigma\). Thus,
dlnorm3 calls dlnorm using the arguments
x = x - threshold, meanlog = meanlog,
sdlog = sdlog
plnorm3 calls plnorm using the arguments
q = q - threshold, meanlog = meanlog, sdlog = sdlog
qlnorm3 calls qlnorm using the arguments
q = q, meanlog = meanlog, sdlog = sdlog and then adds
the argument threshold to the result.
rlnorm3 calls rlnorm using the arguments
n = n, meanlog = meanlog, sdlog = sdlog and then adds
the argument threshold to the result.
The threshold parameter \(\gamma\) affects only the location of the three-parameter lognormal distribution; it has no effect on the variance or the shape of the distribution.
Denote the mean, variance, and coefficient of variation of \(Y = X - \gamma\) by: $$E(Y) = \theta$$ $$Var(Y) = \eta^2$$ $$CV(Y) = \tau = \eta/\theta$$ Then the mean, variance, and coefficient of variation of \(X\) are given by: $$E(X) = \theta + \eta$$ $$Var(X) = \eta^2$$ $$CV(X) = \frac{\eta}{\theta + \gamma} = \frac{\tau \theta}{\theta + \gamma}$$ The relationships between the parameters \(\mu\), \(\sigma\), \(\theta\), \(\eta\), and \(\tau\) are as follows: $$\theta = \beta \sqrt{\omega}$$ $$\eta = \beta \sqrt{\omega (\omega - 1)}$$ $$\tau = \sqrt{\omega - 1}$$ $$\mu = log(\frac{\theta}{\sqrt{\tau^2 + 1}})$$ $$\sigma = \sqrt{log(\tau^2 + 1)}$$ where $$\beta = e^\mu, \omega = exp(\sigma^2)$$
Since quantiles of a distribution are preserved under monotonic transformations, the median of \(X\) is: $$Median(X) = \gamma + \beta$$
dlnorm3 gives the density, plnorm3 gives the distribution function,
qlnorm3 gives the quantile function, and rlnorm3 generates random
deviates.
Aitchison, J., and J.A.C. Brown (1957). The Lognormal Distribution (with special references to its uses in economics). Cambridge University Press, London, 176pp.
Crow, E.L., and K. Shimizu. (1988). Lognormal Distributions: Theory and Applications. Marcel Dekker, New York, 387pp.
Forbes, C., M. Evans, N. Hastings, and B. Peacock. (2011). Statistical Distributions. Fourth Edition. John Wiley and Sons, Hoboken, NJ.
Johnson, N. L., S. Kotz, and N. Balakrishnan. (1994). Continuous Univariate Distributions, Volume 1. Second Edition. John Wiley and Sons, New York.
Ott, W.R. (1990). A Physical Explanation of the Lognormality of Pollutant Concentrations. Journal of the Air and Waste Management Association 40, 1378–1383.
Ott, W.R. (1995). Environmental Statistics and Data Analysis. Lewis Publishers, Boca Raton, FL, Chapter 9.
Royston, J.P. (1992b). Estimation, Reference Ranges and Goodness of Fit for the Three-Parameter Log-Normal Distribution. Statistics in Medicine 11, 897–912.
Wicksell, S.D. (1917). On Logarithmic Correlation with an Application to the Distribution of Ages at First Marriage. Medd. Lunds. Astr. Obs. 84, 1–21.
The two-parameter lognormal distribution is the distribution of a random variable whose logarithm is normally distributed. The two major characteristics of the two-parameter lognormal distribution are that it is bounded below at 0, and it is skewed to the right. The three-parameter lognormal distribution is a generalization of the two-parameter lognormal distribution in which the distribution is shifted so that the threshold parameter is some arbitrary number, not necessarily 0.
The three-parameter lognormal distribution was introduced by Wicksell (1917) in a study of the distribution of ages at first marriage. Both the two- and three-parameter lognormal distributions have been used in a variety of fields, including economics and business, industry, biology, ecology, atmospheric science, and geology (Crow and Shimizu, 1988). Royston (1992) has discussed the application of the three-parameter lognormal distribution in the field of medicine.
The two-parameter lognormal distribution is often used to characterize chemical concentrations in the environment. Ott (1990) has shown mathematically how a series of successive random dilutions gives rise to a distribution that can be approximated by a two-parameter lognormal distribution.
The three-pararameter lognormal distribution starts to resemble a normal distribution as the parameter \(\sigma\) (the standard deviation of \(log(X-\gamma)\) tends to 0.
# Density of the three-parameter lognormal distribution with
# parameters meanlog=1, sdlog=2, and threshold=10, evaluated at 10.5:
dlnorm3(10.5, 1, 2, 10)
#> [1] 0.278794
#[1] 0.278794
#----------
# The cdf of the three-parameter lognormal distribution with
# parameters meanlog=2, sdlog=3, and threshold=5, evaluated at 9:
plnorm3(9, 2, 3, 5)
#> [1] 0.4189546
#[1] 0.4189546
#----------
# The median of the three-parameter lognormal distribution with
# parameters meanlog=2, sdlog=3, and threshold=20:
qlnorm3(0.5, 2, 3, 20)
#> [1] 27.38906
#[1] 27.38906
#----------
# Random sample of 3 observations from the three-parameter lognormal
# distribution with parameters meanlog=2, sdlog=1, and threshold=-5.
# (Note: the call to set.seed simply allows you to reproduce this example.)
set.seed(20)
rlnorm3(3, 2, 1, -5)
#> [1] 18.6339749 -0.8873173 39.0561521
#[1] 18.6339749 -0.8873173 39.0561521