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A study of sea surface height retrieval using Doppler measurements from numerically simulated low grazing angle backscatter data

机译:使用多普勒测量从数值模拟的低掠角反向散射数据中检索海面高度的研究

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A numerical study of the retrieval of sea surface height profiles from low grazing angle Doppler radar measurements is described. Backscattered fields computed using the method-of-moments for one-dimensional ocean-like surface profiles are used to examine properties of Doppler spectra versus range. “Discrete” behaviors observed in the Doppler spectra versus range are found to be related to similar behaviors in orbital velocity statistics obtained directly from the corresponding surface profiles. Differences between Doppler spectra are also observed between VV- and HH-polarizations, with VV-polarization showing smaller Doppler spectral widths in some situations. In order to improve understanding of the accuracies to be expected in surface profile retrievals from Doppler information, estimation errors for the Doppler centroid versus range are studied using a simplified signal model. Comparisons of the results of this signal model with the method-of-moments simulations show that shadowing and multi-path propagation effects cause errors in Doppler centroid estimation beyond those caused by speckle effects alone.
机译:描述了从低掠角多普勒雷达测量值反演海面高度剖面的数值研究。使用矩量法对一维海洋状表面轮廓计算的反向散射场用于检查多普勒光谱随距离变化的特性。发现在多普勒谱中观察到的“离散”行为与距离有关,这与直接从相应表面轮廓直接获得的轨道速度统计中的类似行为有关。在VV和HH极化之间也观察到多普勒频谱之间的差异,在某些情况下VV极化显示较小的多普勒频谱宽度。为了更好地理解从多普勒信息中进行表面轮廓检索时所期望的精度,使用简化的信号模型研究了多普勒质心对距离的估计误差。该信号模型的结果与矩量法仿真结果的比较表明,阴影和多径传播效应引起的多普勒质心估计误差超出了仅由散斑效应引起的误差。

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