method u0440u0430u0434u0438u043eu043au043eu043du0442u0440u043eu043bu00a0 comprising receiving bars of the individual antennas in a frequency signal source u0440u0430u0434u0438u043eu0438u0437u043bu0443u0447u0435u043du0438u00a0, coherent transport u043fu0440u0438u043du00a0u0442u044bu0445 each and u043du0442u0435u043du043du043eu0439 signals at the lower frequency, synchronized conversion of the signals into digital signals, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0, synchronously record the digital u0441u0438u0433u043d al at successive time intervals the receptionu0434u043bu00a0 each time interval are of known algorithms and remember the number of rays and 2d u043fu0435u043bu0435u043du0433u0438 each beam u043fu0440u0438u043du00a0u0442u043eu0433u043e signal u043eu043fu0440u0435u0434u0435u043bu00a0u044e are the average number of rays, which identify the signal source as u043eu0434u043du043eu043bu0443u0447u0435u0432u043eu0439 or u043cu043du043eu0433u043eu043bu0443u0447u0435u0432u043eu0439, u0434u043bu00a0 signal source is identified as u043eu0434u043du043eu043bu0443u0447u0435u0432u043eu0439,the transformation of two-dimensional u0437u0430u043fu043eu043cu043du0435u043du043du044bu0445 bearings u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 average vector of the angular velocity, the components of which are compared to a threshold value of the speed in the p u0440u0435u0432u044bu0448u0435u043du0438u0438 which source identify as air and u0438u0441u043fu043eu043bu044cu0437u0443u00a0 u0437u0430u043fu043eu043cu043du0435u043du043du044bu0435 u0443u0433u043bu043eu043cu0435u0441u0442u043du044bu0435 u043fu0435u043bu0435u043du0433u0438 u043eu0434u043du043eu043bu0443u0447u0435u0432u043eu0433u043e signal and the known height of the flight. signalu043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 change in time down the range to the source signal, while not exceeding the threshold, the speed of the source to ground, after which the institute u043eu043bu044cu0437u0443u00a0 u0437u0430u043fu043eu043cu043du0435u043du043du044bu0435 u043fu0435u043bu0435u043du0433u0438 u043eu0434u043du043eu043bu0443u0447u0435u0432u043eu0433u043e signal, receive the average u043fu0435u043bu0435u043du0433u0438, compared to the average of the u0443u0433u043bu043eu043cu0435u0441u0442u043du044bu0439 bearing source u0438u0434u0435u043du0442u0438u0444u0438u0446u0438u0440u043eu0432 u0430u043du043du043eu0433u043e ground, while not exceeding the threshold.u043eu0434u043du043eu043bu0443u0447u0435u0432u043eu0439 signal ground source identify as surface wave, described the average u0430u0437u0438u043cu0443u0442u0430u043bu044cu043du044bu043c u043fu0435u043bu0435u043du0433u043eu043c, exceeds the threshold, the u043eu0434u043du043eu043bu0443u0447u0435u0432 oh, a terrestrial source identify as spatial wave coordinates of points u0438u0437u043bu0443u0447u0435u043du0438u00a0 which u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442,u043cu043eu0434u0435u043bu0438u0440u0443u00a0 with u043fu0440u0438u0432u00a0u0437u043au043eu0439 to frequency and temporal u0438u043du0442u0435u0440u0432u0430u043bu0443 admission u043cu043du043eu0433u043eu0441u043au0430u0447u043au043eu0432u0443u044e trajectory signal through the ionosphere in the model of reverse u0440u0430u0441u043fu0440u043eu0441u0442u0440u0430u043du0435u043du0438u00a0 measured of u043du0430u043fu0440u0430u0432u043bu0435u043du0438u00a0u0445, u0434u043bu00a0 signal source, u043au043bu0430u0441u0441u0438u0444u0438u0446u0438u0440u043eu0432u0430u043du043du043eu0433u043e as u043cu043du043eu0433u043eu043bu0443u0447u0435u0432u043eu0439, u0438u0441u043fu043eu043bu044cu0437u0443u00a0 u0437u0430u043fu043eu043cu043du0435u043du043du044bu0435 u043fu0435u043bu0435u043du0433u0438 are averages of each beam and u043du0430u0445u043eu0434u00a0 u043fu0435u043bu0435u043du0433u0438 t the maximum difference between the u0443u0433u043bu043eu043cu0435u0441u0442u043du044bu043cu0438 by homogenized u043fu0435u043bu0435u043du0433u0430u043cu0438 rayscompare the maximum difference with a threshold, while not exceeding the threshold u043cu043du043eu0433u043eu043bu0443u0447u0435u0432u043eu0439 signal identify as spatial wavelength, the coordinates of point u0438u0437u043bu0443u0447u0435u043du0438u00a0 which u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442, u043cu043eu0434u0435u043bu0438u0440u0443u00a0 u043cu043du043eu0433u043eu0441u043au0430u0447u043au043eu0432u044bu0435 trajectories of rays otherwise u0440u0430u0441u043fu0440u043eu0441u0442u0440u0430u043du0435u043du0438u00a0 signal through the ionosphere in the model and the measured u043du0430u043fu0440u0430u0432u043bu0435u043du0438u00a0u0445 u0432u044bu0431u0438u0440u0430u00a0 the common point of their arrival at the earth's surface, when it exceeds the threshold.u043cu043du043eu0433u043eu043bu0443u0447u0435u0432u043eu0439 signal identify as surface spatial wavelength caused by the air source with u0430u0437u0438u043cu0443u0442u043eu043c corresponding bearing beam with mini u043cu0430u043bu044cu043du044bu043c angle place, range and height of the flight as a point source u043du0430u0445u043eu0434u00a0u0442 u043fu0435u0440u0435u0441u0435u0447u0435u043du0438u00a0 u043eu0434u043du043eu0441u043au0430u0447u043au043eu0432u043eu0439 trajectory of a signal plane, which you u0431u0440u0430u043du043du044bu0439 minimum angle with the surface of the earth.
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