陆海交界区与运动目标复合散射的矩量法研究

    Study on composite scattering of the land sea boundary area and moving target above it by method of moments

    • 摘要: 为了满足陆海交界区域上方雷达目标检测、识别和分类等的需要,对陆海交界区域表面与上方运动目标复合散射特性进行了研究。采用Monte Carlo方法结合皮尔森-莫斯科维茨(pierson-moskowitz,PM)海谱、Texel-Marsen-Arlose(TMA)海谱与指数功率谱分别生成深水海域海面、有限深海域海面和海岸地貌表面,参照国际无线电咨询委员会推荐的介质反射系数图表模拟海水与海岸的介电常数,运用矩量法计算了陆海交界区域表面与其上方运动圆形截面柱的复合散射系数,得出了复合散射系数的角分布曲线,分析了圆形截面柱分别在深水海域海面、有限深海域海面与海岸地貌表面横向平移、纵向平移对复合散射系数的影响,同时还分析了圆形截面柱分别移动至海岸地貌表面、有限深海域海面、深水海域海面对复合散射系数的影响。数值计算结果表明,复合散射系数随散射角振荡的变化,圆形截面柱在海岸地貌表面与深水海域海面上方的纵向平移对复合散射系数影响较为显著,而圆形截面柱在有限深海域海面上方的移动对复合散射系数的影响比较复杂,且当圆形截面柱沿陆海交界区域表面移动时,复合散射系数会受到较大的影响。

       

      Abstract: In order to meet the needs of radar target detection, recognition, and classification above the land sea boundary area, the composite scattering characteristics of the surface and moving targets above the land sea boundary area were studied. The Monte Carlo method was used to combine PM sea spectrum, TMA sea spectrum, and exponential power spectrum to generate deep water sea surface, limited depth sea surface, and coastal geomorphic surface, respectively. The dielectric constant of seawater and coast was simulated using the medium reflection coefficient chart recommended by CCIR(International Radio Consultative Committee). The composite scattering coefficient of the surface of the land sea boundary area and the moving circular cross-section column above it was calculated using the method of moments, and the angular distribution curve of the composite scattering coefficient was obtained, we analyzed the effects of horizontal and vertical translation of circular cross-section columns on the composite scattering coefficient in deep-sea sea surface, coastal geomorphic surface, and limited depth sea surface. We also analyzed the effects of circular cross-section columns moving to coastal geomorphic surface, limited depth sea surface, and deep water sea surface on the composite scattering coefficient. The numerical calculation results show that the composite scattering coefficient oscillates with the scattering angle, and the longitudinal translation of a circular cross-section column above the coastal geomorphic surface and the deep water sea surface has a significant impact on the composite scattering coefficient. However, the movement of a circular cross-section column above the finite depth sea surface has a complex impact on the composite scattering coefficient, and when the circular cross-section column moves along the surface of the land sea boundary area, the composite scattering coefficient will be greatly affected.