I. Introduction
Synthetic aperture radar (SAR) is a remote sensing technology that uses the motion of the radar transmitter to synthesize an antenna aperture much larger than the actual antenna aperture in order to yield high spatial resolution radar images. It is an active coherent all weather imaging system that operates in the microwave region of the spectrum. This imagery is well suited to the task of remote ground mapping in many applications. In the last few years, high quality images of the Earth produced by SAR systems, carried on a variety of airborne and space borne platforms, have become increasingly available. The primary geophysical quantity determining the SAR data is the complex radar reflectivity of the scene. The SAR data provide measurements of this reflectivity [1]. The local reflectivity at each pixel is represented by a complex number, so the SAR data are known as complex imagery. The noise-like characteristic of these types of images is known as speckle, and it is strongly reflected in the intensity and amplitude parts of the SAR data. The speckle is in fact a scattering phenomenon that occurs because the resolution of the sensor is insufficient to resolve individual scatters within an imaged pixel. In a homogeneous area where the underlying backscattering coefficient is constant, the fluctuation of SAR intensity is only caused by speckle and could be removed using appropriate filters [2]. The real and imaginary parts of the SAR data have resembling Gaussian distribution. Meanwhile, the phase of the complex SAR data has an almost uniform distribution, and the amplitude part of the complex SAR data belongs to the family of gamma distribution [1].