Statistics based on the finite atomic functions Kravchenko-Rvachev and their use for the description of scattered sea signal

At high resolution in range and angular coordinates, there are significant deviations of distributions of fluctuations reflected by underlying surfaces and “clear” sky signals from standard [1,2]. It is caused by sequential and separate observation of surface regions with different statistical properties of the irregularities which lead to unsteadiness and non-Gaussian scattering signal. For the sea surface are areas in which there are crests of the waves, which have high reflectivity. In this report for the first time discussed the use of statistics to describe the reflected signal sea finite atomic functions Kravchenko-Rvacheva.