K-distribution
The K-distribution is a continuous probability distribution that models the statistics of radar returns from textured surfaces, such as sea clutter, by combining a gamma-distributed texture component representing local reflectivity variations with an exponential speckle component arising from coherent imaging.[1] Introduced in 1976 by E. Jakeman and P. N. Pusey to explain non-Rayleigh scattering in microwave sea echo, it captures the spiky, heavy-tailed nature of such signals, which deviate from Gaussian assumptions in traditional radar models.[1][2] The probability density function (PDF) for the intensity z in a single-look K-distributed clutter is given by the compound formP(z) = \int_0^\infty P(z|x) P_c(x) \, dx,
where P(z|x) = \frac{1}{x} \exp\left(-\frac{z}{x}\right) is the conditional exponential PDF for speckle given local power x, and P_c(x) = \frac{b^\nu}{\Gamma(\nu)} x^{\nu-1} \exp(-b x) is the gamma PDF for x, with shape parameter \nu > 0 controlling texture roughness (lower \nu yields spikier distributions) and scale parameter b = \nu / p_c related to mean clutter power p_c = \mathbb{E}.[2] This integral lacks a simple closed form but evaluates to
P(z) = \frac{2 b^{\nu/2} z^{(\nu-1)/2}}{\Gamma(\nu) } K_{\nu-1}(2 \sqrt{b z}),
involving the modified Bessel function of the second kind K_{\nu-1}(\cdot).[3] Key properties include infinite higher-order moments for \nu \leq k (where k is the moment order), a shape parameter \nu that quantifies deviation from Rayleigh (as \nu \to \infty, it approaches exponential), and versatility in extensions like the multivariate or polarimetric K-distribution for correlated channels in synthetic aperture radar (SAR) imagery.[4] Applications span radar performance analysis, including constant false alarm rate (CFAR) detection in sea clutter, where numerical integration (e.g., Gauss-Laguerre quadrature) computes detection probabilities, and simulation of nonhomogeneous environments for target discrimination.[2][5] The model has been validated extensively against X-band and other radar measurements, influencing maritime surveillance, ocean remote sensing, and even adaptations in optical coherence tomography for heavy-tailed intensity data.[6][7]