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首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Study of Microwave Backscattering From Two-Dimensional Nonlinear Surfaces of Finite-Depth Seas
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Study of Microwave Backscattering From Two-Dimensional Nonlinear Surfaces of Finite-Depth Seas

机译:有限深度海二维非线性表面微波反向散射研究

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This paper presents a study of the microwave backscattering from 2-D time-evolving nonlinear surfaces of a sea with finite depth by using the second-order small-slope approximation. According to the shallow-water dispersion relation, the revised nonlinear hydrodynamic choppy wave model in connection with an experiment-verified sea spectrum for finite-depth water is employed to construct the wave profiles in the finite-depth sea. The numerical results show that the discrepancy between the choppy surfaces of the infinite-depth sea and their finite-depth counterparts for monostatic normalized radar cross section is much smaller than that between the linear surfaces and the nonlinear choppy surfaces. Furthermore, the comparison of the Doppler spectra of the backscattered echoes from the linear and nonlinear choppy sea surfaces shows that the nonlinear hydrodynamic features significantly impact the Doppler spectrum. In particular, the Doppler spectrum for nonlinear finite-depth sea presents much higher second-order peaks and increased spectral amplitudes in the frequency range around the Doppler peak frequency, which reiterates the importance of the role that the nonlinear hydrodynamic effect of waves played in the interpretation of backscattering from finite-depth nearshore seas from the qualitative point of view.
机译:本文利用二阶小斜率逼近技术,研究了有限深度海面二维随时间演化的非线性表面的微波反向散射问题。根据浅水扩散关系,采用修正的非线性水动力波动波模型,并结合实验验证的有限深度水域的海谱,构造了有限深度海域的波廓。数值结果表明,单深度归一化雷达横截面的无限深度海浪表面与有限深度对应物之间的差异远小于线性表面和非线性波浪面之间的差异。此外,对来自线性和非线性波涛汹涌的海面的反向散射回波的多普勒频谱的比较表明,非线性流体动力学特征会显着影响多普勒频谱。特别是,非线性有限深度海的多普勒频谱在多普勒峰值频率附近的频率范围内呈现出更高的二阶峰值和增加的频谱幅度,这重申了波浪的非线性水动力效应在海浪中发挥作用的重要性。从质的角度解释近海有限深度海域的反向散射。

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