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A line-of-sight propagation model for calculating atmospheric, sea, terrain multipath, and clutter at microwave frequencies

机译:一种视距传播模型,用于计算微波频率下的大气,海洋,地形多径和杂波

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The two-dimensional parabolic wave equation (PE) is solved asymptotically in order to derive a propagation/scattering model for propagation in a stratified atmosphere, together with scattering and diffraction from the sea/terrain surface, within line of sight. The asymptotic solution to the PE begins by expanding the unknown field in a Luneberg-Kline expansion. The first-order solution to the Luneberg-Kline expansion yields the eikonal equation for the ray trajectory, and the second-order solution yields the transport equation for the energy density of the rays along the trajectory. The solution to the eikonal and transport equations is used to derive an asymptotic result for the plane wave spectrum solution for the PE, referred to as the wave-theoretic model. The asymptotic solution for the field shows the relationship between a properly directed tube of rays in the atmosphere satisfying the eikonal and conservation of energy equations and the same tube of rays striking an edge and being diffracted, as in the geometrical theory of diffraction (GTD). The solution for the eikonal yields the ray trajectory in the stratified atmosphere and therefore the grazing angle on the sea/terrain profile necessary for calculating multipath and clutter. Also, a new derivation for the backscatter from a deterministic sea/terrain profile is given which agrees with Collin's [1992] new full wave theory and at grazing reduces to the perturbation result with the correct polarization dependence. Incorporating the various electromagnetic propagation/scattering mechanisms in one model yields a prediction tool that can be applied to a large class of propagation/scattering problems such as the analysis of radar performance in a littoral scenario, or the performance of a line-of-sight communication link operating over irregular terrain.
机译:渐近求解二维抛物线波动方程(PE),以便得出在视线内分层大气中传播的传播/散射模型,以及海/地形表面的散射和衍射。 PE的渐近解始于通过Luneberg-Kline展开扩展未知场。 Luneberg-Kline展开的一阶解产生了射线轨迹的推导方程,二阶解产生了沿轨迹的射线能量密度的输运方程。对本征方程和输运方程的解用于得出PE的平面波谱解的渐近结果,称为波理论模型。该场的渐近解表明,在满足能量方程式守恒和能量方程的大气中正确定向的射线管与撞击边缘并被衍射的相同射线管之间的关系,就像在衍射几何理论(GTD)中一样。人体的解产生层状大气中的射线轨迹,因此得出海/地形剖面上的掠射角,这是计算多径和杂波所必需的。另外,给出了确定性海陆地形的反向散射的新推导,该推导与Collin [1992]的新全波理论相吻合,并且在掠射时以正确的偏振相关性降低了扰动结果。将各种电磁传播/散射机制整合到一个模型中,可以得出一种预测工具,该预测工具可以应用于大范围的传播/散射问题,例如在沿海场景中分析雷达性能或视线性能通讯链接在不规则地形上运行。

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