Nakagami distribution
What it describes
Nakagami models signal amplitude under fast fading. m controls fading severity and omega mean power; the family adapts to different propagation environments.
Amplitude is non-negative. m=1 is Rayleigh and m=1/2 is Half Normal under a common convention; larger values concentrate the signal around mean power.
History and names
Minoru Nakagami proposed the model in 1960 while studying rapid radio fading. It spread into wireless-channel and performance analysis.
How it connects to other distributions
It is a Gamma transform applied to squared amplitude. Rayleigh and approximate Rician behaviours are related cases; Weibull is another empirical fading alternative.
Where it appears
- wireless channels and multipath fading
- radar, sonar, and signal-intensity models
Fitting cautions
Enforce m ≥ 1/2 and omega > 0; compare omega with mean power only when package conventions agree.
The amplitude whose power becomes Gamma
Minoru Nakagami proposed the m distribution for rapid fading of radio waves. Its key construction is simple: squared amplitude is Gamma. Thus omega represents mean power while m governs fading severity.
In the classical form, m=1 recovers Rayleigh and m=1/2 is related to Half Normal. Larger values concentrate amplitude and can approximate some Rice channels, although Nakagami does not explicitly model a line-of-sight component. This approximation ability explains much of its computational success. It also warns against reading m as a physical count without evidence from the channel.
Decision guide
A good candidate when: nonnegative signal amplitude is modelled and its power can be described by a Gamma law.
Compare it with: Rayleigh with no line of sight and Rice with an explicit coherent component. Fit and diagnose power as well as amplitude.
References
- SciPy reference: scipy.stats.nakagami — definition and parameterization
- Johnson, N. L., Kotz, S. & Balakrishnan, N. (1995). Continuous Univariate Distributions, 2nd ed., Vol. 2. Wiley.
- Nakagami, M. (1960). The m-distribution: A general formula of intensity distribution of rapid fading. In Statistical Methods in Radio Wave Propagation. Pergamon.