the receiver due to coherent scattering from a random sea surface. We represent the sea
surface as a Sum of Sinusoids (SoS) and model it using Pierson-Moscovitz (PM) sea wave
spectrum. We evaluate the random behavior of potential scatterers along the sea surface,
sea surface wave height, and their possible impact on the distribution of AoA at the receiver.
Initially, analysis is carried out for a single realization of the sea surface, ie, a sinusoidal …