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Comparison of geometric optics and diffraction effects in radar scattering from steep and breaking waves

机译:陡波和碎波雷达散射中几何光学和衍射效应的比较

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To address the issue of radar scattering from steep and breaking ocean waves, we developed an efficient and fast 2-D numerical full-wave approach to model both wave evolution and radar scattering from these waves. It enabled us to reproduce the main features of the temporal and polarization behavior of the radar signal such as sea spikes. In addition, to better understand the contribution of multiple scattering that might emerge from radar scattering on steep and breaking waves, we have modeled scattering using a ray-tracing approach that not only provides the ray picture but also supplies both the ray amplitude and the ray phase. This approach eliminates diffraction effects from consideration, leaving only geometric optics effects that include multiple reflections. As a result, angular dependencies of the scattering cross section based on the ray approach were calculated and compared with corresponding values from the full-wave approach. Generally, better agreement between these two approaches is obtained for forward scattering directions than for backscattering directions. Ray simulation for a backscattering direction does not reproduce the HH/VV ratio with the spikes observed in the fullwave solution. This indicates that diffraction effects are critical for explaining important features of backscattering from breaking waves. The role of multiple reflections from the breaking wave profile in creating spikes with an anomalous HH/VV ratio proved to be negligible.
机译:为了解决陡峭和破裂的海浪产生的雷达散射问题,我们开发了一种高效且快速的二维数值全波方法,可以对波的演化和这些波的雷达散射进行建模。它使我们能够重现雷达信号的时间和极化行为的主要特征,例如海峰。此外,为了更好地理解雷达散射在陡峭和破碎波上可能产生的多重散射的影响,我们使用射线跟踪方法对散射进行了建模,该方法不仅提供射线图像,还提供射线幅度和射线阶段。这种方法消除了考虑的衍射效应,只留下了包括多重反射的几何光学效应。结果,计算了基于射线方法的散射截面的角度相关性,并将其与全波方法的相应值进行了比较。通常,对于前向散射方向要比对后向散射方向获得这两种方法之间更好的一致性。反向散射方向的射线模拟不能重现HH / VV比率,并且在全波解决方案中会观察到尖峰。这表明衍射效应对于解释碎波引起的反向散射的重要特征至关重要。破碎波剖面的多次反射在产生具有异常HH / VV比的尖峰中的作用被证明是微不足道的。

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