Wang R, Guo L-X
School of Science, Xidian University, Xi'an, Shaanxi Province, China.
J Opt Soc Am A Opt Image Sci Vis. 2009 Mar;26(3):517-29. doi: 10.1364/josaa.26.000517.
The problem of electromagnetic (EM) scattering between the time-varying lossy dielectric ocean and a moving target is always solved by using some numerical algorithm. However, the elements of the impedance matrix and the surface electric and magnetic currents of the lossy dielectric ocean must be determined and evaluated again at different moments due to the varying of the ocean with time, and the numerical algorithm will produce an enormous amount of calculation. To overcome this shortcoming, the reciprocity theorem is used to solve the coupling field between a time-varying lossy dielectric ocean and a moving conducting plate above it. Due to the advantage of the reciprocity theorem, the difficulty in computing the secondary scattered fields is reduced. The polarization currents of the ocean and the first scattered field from the conducting plate are both evaluated by using the physical optics (PO) method. The backscattered field from the ocean is evaluated by using the Kirchhoff approximation (KA) method. The characteristics of the coupling backscattered field and the Doppler spectrum are analyzed in detail for different incident conditions.
时变有耗介质海洋与运动目标之间的电磁(EM)散射问题一直通过某种数值算法来解决。然而,由于海洋随时间变化,有损介质海洋的阻抗矩阵元素以及表面电磁流必须在不同时刻重新确定和评估,这会使数值算法产生大量计算。为克服这一缺点,利用互易定理求解时变有耗介质海洋与其上方运动导电板之间的耦合场。由于互易定理的优势,降低了计算二次散射场的难度。海洋的极化电流和导电板的一次散射场均采用物理光学(PO)方法进行评估。海洋的后向散射场采用基尔霍夫近似(KA)方法进行评估。针对不同入射条件,详细分析了耦合后向散射场的特性和多普勒频谱。