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首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >A Numerical Study of the Retrieval of Sea Surface Height Profiles From Low Grazing Angle Radar Data
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A Numerical Study of the Retrieval of Sea Surface Height Profiles From Low Grazing Angle Radar Data

机译:低掠角雷达数据反演海面高度剖面的数值研究

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A numerical study of the retrieval of sea surface height profiles from low grazing angle radar observations is described. The study is based on a numerical method for electromagnetic scattering from 1-D rough sea profiles, combined with the “improved linear representation” of Creamer for simulating weakly nonlinear sea surface hydrodynamics. Numerical computations are performed for frequencies from 2975 to 3025 MHz so that simulated radar pulse returns are achieved. The geometry utilized models a radar with an antenna height of 14 m, observing the sea surface at ranges from 520 to 1720 m. The low grazing angles of this configuration produce significant shadowing of the sea surface, and standard analytical theories of sea scattering are not directly applicable. Three approaches for retrieving sea height profile information are compared. The first method uses a statistical relationship between the surface height and the computed radar cross sections versus range (an incoherent measurement). A second method uses the phase difference between scattering measurements in two vertically separated antennas (“vertical interferometry) in the retrieval. The final technique retrieves height profiles from variations in the apparent Doppler frequency (coherent measurements) versus range and requires that time-stepped simulations be performed. The relative advantages and disadvantages of each of the three approaches are examined and discussed.
机译:描述了从低掠角雷达观测中获取海面高度剖面的数值研究。该研究基于一种数值方法,用于从一维波涛汹涌的海面电磁散射,并结合Creamer的“改进的线性表示”来模拟弱非线性海面流体动力学。对2975至3025 MHz的频率进行了数值计算,以便获得模拟的雷达脉冲返回。所使用的几何模型对天线高度为14 m的雷达进行建模,观察海面的范围为520至1720 m。这种配置的低掠角会在海面产生明显的阴影,并且标准的海散射分析理论不能直接应用。比较了三种检索海平面高度信息的方法。第一种方法使用表面高度和计算出的雷达横截面与范围之间的统计关系(非相干测量)。第二种方法是在检索中使用两个垂直分开的天线中的散射测量值之间的相位差(“垂直干涉测量法”)。最终技术从视在多普勒频率(相干测量)相对于范围的变化中检索高度轮廓,并要求执行时步仿真。考察并讨论了这三种方法中每种方法的相对优缺点。

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