Efficiency of radar operating over the sea surface is radically determined by the characteristics of signals scattered by this surface. Averaged characteristics of backscattering for centimetre (CM) and millimetre (MM) wave bands were investigated for a long period of time and a large amount of experimental data has been obtaine (I. But up to now the experimental results of investigations of statistical characteristics of signals scattered by nonstationary rough sea and caused by wave breaking are limited. Introduction
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