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Research on SAR imaging mechanism for ocean wave propagating in azimuth direction by using numerical simulation

机译:利用数值模拟研究海浪在方位方向传播的SAR成像机理

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The SAR image simulation has been developed in the time domain to investigate a SAR imaging mechanism for moving ocean surfaces. In the previous paper [2], the simulation had carried out for ocean waves to confirm image displacements caused by moving surfaces. The results of the previous paper showed that the wave pattern of the azimuth wave is not displayed in the simulated SAR image. We had concluded that it is caused by velocity bunching. However, in this paper, the SAR imaging mechanism of ocean waves is reconsidered that it is affected not only by motion induced modulation but also by scattering intensity. To examine the SAR imaging mechanism, azimuth signals from moving and stationary waves are simulated. The results show that the velocity bunching might not occur in accordance with the conventional theories. It is suggested that when backscattering intensities from ocean surfaces that have radial velocities are weak, their modulations are also minor components in SAR signals. A possible explanation about diminishing wave patterns of azimuth waves in SAR images is discussed in terms of local incident angles that are angles between SAR and ocean surface.
机译:在时域中已经开发了SAR图像模拟,以研究用于移动海洋表面的SAR成像机制。在先前的论文[2]中,已经对海浪进行了模拟,以确认由移动表面引起的图像位移。先前的结果表明,在模拟的SAR图像中未显示方位角波的波形。我们已经得出结论,它是由速度聚集引起的。然而,在本文中,重新考虑了海浪的SAR成像机制,它不仅受运动引起的调制的影响,还受到散射强度的影响。为了检查SAR成像机制,模拟了来自移动波和固定波的方位角信号。结果表明,按照传统理论,速度成束可能不会发生。建议当具有径向速度的海面的反向散射强度较弱时,它们的调制也是SAR信号中的次要分量。根据局部入射角(SAR和海洋表面之间的角度),讨论了关于减小SAR图像中方位角波型的可能解释。

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