We study the frequency spectra of the radar signals scattered from the wind waves on the sea surface in the full-scale experiment. Two types of the radar Doppler shifts of the spectrum maximum, namely, the averaged shift of the instantaneous spectrum of the scattered signal and the shift of the maximum of the signal time-averaged spectrum as functions of the incidence angle and the wind velocity and direction are analyzed for different sounding-wave polarizations. Significant difference between the average shift of the instantaneous spectrum and the shift of the average-spectrum maximum is demonstrated. This difference is attributed to the radar-signal modulation effect in the field of long surface waves. The obtained results are very important for correct retrieval of the velocities of the surface currents using the data of the satellite-borne measurements of the radar Doppler shifts.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 57, No. 4, pp. 267–280, April 2014.
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Ermakov, S.A., Kapustin, I.A., Kudryavtsev, V.N. et al. On the Doppler Frequency Shifts of Radar Signals Backscattered from the Sea Surface. Radiophys Quantum El 57, 239–250 (2014). https://doi.org/10.1007/s11141-014-9507-8
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DOI: https://doi.org/10.1007/s11141-014-9507-8