Study on Sea Surface Spectrum Model for Electromagnetic Scattering in Ku-Band Based on Two-Scale Model

Chenyu Guo, Hongxia Ye
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Abstract

The wave spectrum model of ocean surface, which describes the statistical characteristics of ocean surface fluctuation, is very important to electromagnetic scattering modeling of ocean surface. By dividing the wave spectrum into large-scale and small-scale parts, the two-scale model (TSM) combines Kirchhoff approximation (KA) with the small perturbation method (SPM) to expand the application range of the model. This paper uses the TSM to study the simulation performance of Durden-Vesecky (DV) spectrum, Apel spectrum and Elfouhaily spectrum in Ku-band. The cutoff wavenumber is one of the most important factors affecting the accuracy of TSM simulation. We simulate the backscattering coefficients by TSM with different cutoff wavenumbers, and compare with the NSCAT-4 geophysical model function (GMF) to find the minimum absolute error. Then these minimum absolute errors are used to calculate the mean absolute error to select the most appropriate wave spectrum model. The simulation results of different spectrums demonstrate that the Apel spectrum is more suitable for backscattering simulation of rough sea surfaces in Ku-band when the incidence angle is 30° ~ 66° and the wind speed is 3 ~ 20 m/s.
基于双尺度模型的ku波段海面电磁散射谱模型研究
海洋表面波谱模型描述了海洋表面波动的统计特征,是海洋表面电磁散射模拟的重要组成部分。双尺度模型(TSM)通过将波浪谱划分为大尺度和小尺度两部分,结合Kirchhoff近似(KA)和小摄动方法(SPM),扩大了模型的适用范围。本文利用TSM对ku波段的Durden-Vesecky (DV)谱、Apel谱和Elfouhaily谱的仿真性能进行了研究。截止波数是影响TSM仿真精度的重要因素之一。采用不同截止波数的TSM方法模拟后向散射系数,并与NSCAT-4地球物理模型函数(GMF)进行比较,找出最小的绝对误差。然后利用这些最小绝对误差来计算平均绝对误差,以选择最合适的波谱模型。不同谱线的模拟结果表明,当入射角为30°~ 66°,风速为3 ~ 20 m/s时,Apel谱线更适合ku波段粗糙海面的后向散射模拟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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