It is expected that the problem of the azimuth cutoff wavelength in single-satellite synthetic aperture radar (SAR) observations can be solved by means of the cooperative observation of networked SAR satellites. Multiview SAR wave synchronization data are required in the process. However, most of the current orbiting satellites are geosynchronous orbit satellites; the simultaneous observation by multiple SARs in the same sea area cannot be achieved, and multiview synchronization data cannot be obtained. Therefore, this paper studies the simulation of the multiview SAR wave synchronization data. Ocean wave spectra were simulated by using the Pierson Moskowitz (PM) spectrum. The Monte Carlo method was used to simulate two-dimensional (2D) ocean surfaces at different wind speeds. The two-scale electromagnetic scattering model was used to calculate the ocean surface backscattering coefficient, and the time-domain echo algorithm was used to generate echo signals. The echo signals were processed by the Range–Doppler (RD) imaging algorithm to obtain ocean SAR data. Based on the obtained single-SAR wave data, networked satellites consisting of three SARs were simulated, and the SAR wave data were synchronized. The results show that when SARs are used to observe the same sea area from different observation directions, the clarity of the wave fringes in the SAR images are different. For different azimuth angles, the degrees of azimuth cutoff are different. These results reflect the influences of different degrees of azimuth cutoff on SAR images. The simulated wave synchronization data can be used as the basic data source for subsequent azimuth cutoff wavelength compensation.

Synthetic aperture radar (SAR) can extract sea surface wind speed information. To extract wind speed information through the geophysical model function (GMF), the corresponding wind direction information must be input. This article introduces some concepts about networked SAR satellites. The networked satellites enable multiple SARs to observe the same sea surface at different incidence angles at the same time. Aiming at the X-band networked SAR data with different incident angles, the cost function is established by using the GMF. By minimizing the cost function, accurate wind speed information can be extracted without inputting wind direction information. When the noise is small, the wind direction information is introduced, and the accuracy of the extracted wind speed will be improved. When the noise is less than 1 dB and the incident angle is greater than 30°, the root-mean-square error (RMSE) of the wind speed extracted by this method is basically less than 2 m/s.

Due to the nonlinear effect of velocity bunching modulation, azimuth cutoff occurs when waves are propagating along the azimuth direction. This is an inherent disadvantage of synthetic aperture radar (SAR) wave observation and makes it impossible to obtain complete wave information. For a single SAR observation, the problem of the azimuth cutoff wavelength of ocean waves can be solved to some extent by the cooperative observations of SAR satellites. It is necessary to use multiple SAR satellites to achieve simultaneous observation of the same ocean area to obtain multiview SAR ocean wave synchronization data. At present, it is impossible to acquire multiview synchronization data based on in-orbit SARs. Therefore, this paper first carried out imaging simulations of multiview SAR ocean wave synchronization data. Second, the MPI method was used to obtain the optimum wave spectrum of synchronous data. The influencing factors of the azimuth cutoff wavelength were analyzed by using the measured SAR data. Based on the analysis results, a new method of multiview wave spectrum data fusion is proposed to realize azimuth cutoff compensation. The azimuth cutoff compensation effect is evaluated by using the inversion results of the azimuth cutoff before and after spectral data fusion, the significant wave height and the mean wave period. The results show that the azimuth cutoff compensation method established in this paper can solve the problem of information loss caused by azimuth cutoff to some extent, improve the ability of SAR wave observation, and lay a foundation for SAR wave operational observation.