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Numerical research on clear imaging of azimuth-traveling ocean waves in SAR images

机译:SAR图像中行进海浪清晰成像的数值研究

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摘要

This paper presents the imaging mechanisms of ocean waves traveling in the azimuth direction by applying a numerical simulation of synthetic aperture radar (SAR) image for moving ocean surfaces. The numerical simulation was originally designed in the time domain to take into account motion-induced modulations. It is known that azimuthal waves are affected by azimuth shifts due to orbital motions of ocean waves, i.e., velocity bunching. The effect of bunching generally results in nonlinear imaging; however, a clear wavelike pattern of a homogeneous wave field propagating to the azimuth direction occurs in SAR imagery under a certain condition. More specifically, if azimuth shifts due to the orbital motions are concentrated on wave crests or troughs, bunching causes a single peak in SAR image planes. Theoretically, it is derived noticeably when the maximum orbital motion of an azimuth-traveling ocean wave is nearly equal to one quarter of its wavelength. To demonstrate this, SAR signals were simulated numerically for ocean waves with and without employing the condition of the clear imaging. The results showed that a wavelike pattern relating to the azimuthal waves can be imaged apparently under the specific condition. In addition, the simulations were performed in the case of the other wave and wind conditions. From the results, it was revealed that the specific condition leads to clear wavelike imaging of azimuthal waves in SAR images if noise is relatively small.
机译:本文通过对合成孔径雷达(SAR)图像进行海面运动的数值模拟,介绍了沿方位角方向传播的海浪的成像机理。数值模拟最初是在时域中设计的,以考虑运动引起的调制。众所周知,由于海浪的轨道运动即速度成束,方位角波受到方位角偏移的影响。聚束的效果通常会导致非线性成像。但是,在一定条件下,SAR图像会出现向方位角方向传播的均匀波场的清晰波状图案。更具体地说,如果由于轨道运动而引起的方位角偏移集中在波峰或波谷上,则聚束会在SAR图像平面中引起单个峰值。从理论上讲,当方位角海浪的最大轨道运动几乎等于其波长的四分之一时,就可以明显地得出。为了证明这一点,在有或没有采用清晰成像条件的情况下,对海浪的SAR信号进行了数值模拟。结果表明,在特定条件下,可以清晰地成像出与方位波有关的波状图案。另外,在其他波浪和风的情况下进行了仿真。从结果可以看出,如果噪声相对较小,则特定条件会导致SAR图像中方位角波的清晰波状成像。

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