In probability theory and statistics, the Rayleigh distribution is a continuous probability distribution. It usually arises when a two-dimensional vector (e.g. windvelocity) has its two orthogonal components normally and independently distributed. The absolute value (e.g. wind speed) will then have a Rayleigh distribution. The distribution may also arise in the case of random complex numbers whose real and imaginary components are normally and independently distributed. The absolute value of these numbers will then be Rayleigh-distributed.
where is the Gamma function. The moments may be used to calculate:
Mean:
Variance:
Skewness:
Kurtosis:
Parameter estimation
Given N independent and identically distributed Rayleigh random variables with parameter , the maximum likelihood estimate of is
Related distributions
is a Rayleigh distribution if where and are two independent normal distributions. (This gives motivation to the use of the symbol "sigma" in the above parameterization of the Rayleigh density.)