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A Computer Simulation of Relative Backscattering Coefficients of Sea Surfaces in Satellite Altimetry

机译:卫星测高中海面相对反向散射系数的计算机模拟

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The purpose of this study is to establish a method for estimating the sea wave period by satellite radar altimetry. The backscatter coefficient, which is closely related to the period, is evaluated by computer simulation. Specifically, the following method is presented. The sea wave is modeled on the basis of the Pierson-Moskowitz spectrum. The average received power is determined by radar altimetry simulation of our proposal. It is shown that the backscatter coefficient of the sea surface can be calculated on a relative basis. Using the data for the relative received power calculated from various sea wave parameters, the relation between the significant wave height and the backscatter coefficient, and also the relation between the significant wavelength and the backscatter coefficient, are derived. Thus, the possibility of observing the sea wave period by using satellite radar altimetry is demonstrated.
机译:这项研究的目的是建立一种通过卫星雷达测高仪估算海浪周期的方法。与周期密切相关的反向散射系数通过计算机仿真进行评估。具体地,提出以下方法。海浪是基于Pierson-Moskowitz光谱建模的。平均接收功率由我们建议的雷达测高模拟确定。结果表明,可以相对地计算出海面的后向散射系数。使用从各种海浪参数计算出的相对接收功率的数据,得出有效波高与反向散射系数之间的关系,以及有效波长与反向散射系数之间的关系。因此,证明了使用卫星雷达测高仪观测海浪周期的可能性。

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