“…As can be seen, at any slow time π‘ Μ= π‘ Μ1, π‘ Μ2, β¦ π‘ Μπ, the signals backscattered by sea surface π π (π‘), n=0, ...15, nβ 8, defined by eq. ( 12), are processed according to a beamforming algorithm (see [30] for more details) based on a double Fast Fourier Transform (FFT), the first one along the time (range-FFT) and the second one along the channels (angle-FFT). In this way, after conversion from slant range r to ground range π on the MSL, a focused intensity image πΌ(π, π, π‘ ) of the sea surface is achieved.…”