SAR imagery (Radar satellite data) is a special type of space imaging in which microwave radiation with wavelengths ranging from 1 cm to 1 m is used to obtain information by illuminating the Earth's surface and detecting the reflected signals. Radar aerial and space imaging is one of the methods of remote sensing of the Earth's surface, allowing for the acquisition of images of the terrain in the microwave range of the electromagnetic spectrum. Radar images enable the visualization of the Earth's surface and objects regardless of weather conditions, in both day and night time, by emitting and receiving reflected signals from the Earth's surface, followed by the conversion of these signals into images or extraction of phase difference information between the transmitted and reflected signals. The data obtained from radar sensors, similar to optical satellite images, have different spatial resolutions and the ability to capture information in various electromagnetic bands. Radar satellite data consist of two components: the phase component and the amplitude component. The differential interferometric processing of the phase component allows for the measurement of surface displacements, while the processing of the amplitude component enables differentiation of the reflecting surface based on roughness characteristics and volumetric scattering, i.e., object decryption. The technology of differential interferometric processing involves the formation of an interferogram, which, in simplified terms, is the result of multiplying a pair of complex-valued radar images of the same area acquired by identical SAR (Synthetic Aperture Radar) systems from closely located points of the orbit. The phase cycle differences within each pixel in the interferogram represent the relative change in distance between the radar antenna and the reflector (probed surface).