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Doppler Spectra of Microwave Scattering Fields From Nonlinear Oceanic Surface at Moderate- and Low-Grazing Angles

机译:中等和低掠角下非线性海洋表面微波散射场的多普勒谱

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Results of microwave radar Doppler spectra from 1-D nonlinear ocean surface at moderate- and low-grazing angles are calculated by the composite surface scattering model. For the large-scale undulating surface description, the narrow-band Lagrange model is used, which takes into account the vertical and horizontal skewnesses. Moreover, the shadow and the curvature effects of large-scale waves on the Doppler spectra are also considered in our calculations. Comparisons of computed curves with experimentally measured Doppler spectra at different incidence angles and at various wind speeds show that the simulated results can fit the measured data well at moderate incident angles. From the simulations, we also find that the hydrodynamic modulation and the horizontal skewness of the large-scale waves can induce remarkable influence on Doppler shift. In addition, when the shadow and the curvature effects of large-scale waves are considered in the calculations, the Doppler shifts grow more quickly and the spectral widths become narrower at low-grazing angles, and this is consistent with the numerical results given by Toporkov in the nonlinear surface case. The conclusions obtained in this work seem promising for better understanding the properties of time-dependent radar echoes from oceanic surfaces.
机译:通过复合表面散射模型,计算了中度和低掠角下一维非线性海洋表面的微波雷达多普勒光谱结果。对于大规模起伏表面描述,使用了窄带拉格朗日模型,该模型考虑了垂直和水平偏斜。此外,在我们的计算中还考虑了大尺度波对多普勒频谱的阴影和曲率效应。在不同的入射角和不同的风速下,将曲线与实验测得的多普勒光谱进行比较,结果表明,模拟结果可以在中等入射角下很好地拟合测量数据。从模拟中,我们还发现大尺度波的流体动力调制和水平偏斜可以对多普勒频移产生显着影响。另外,在计算中考虑到大尺度波的阴影和曲率效应时,在低掠角时多普勒频移增长更快,光谱宽度变窄,这与托普尔科夫给出的数值结果一致。在非线性表面情况下。在这项工作中获得的结论对于更好地了解海洋表面随时间变化的雷达回波的特性似乎很有希望。

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